Changeset 309 for branches


Ignore:
Timestamp:
03/28/13 18:00:55 (11 years ago)
Author:
pinsard
Message:

fix typo (missing and, chemical symbols, etc.) thanks to biber

Location:
branches/bibliolocean
Files:
4 edited

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  • branches/bibliolocean/data/biblioref.bib

    r308 r309  
    7070timestamp = {20130220}, 
    7171title = {{Role of air-sea interactions on the coastal rainfall in the Gulf of Guinea during boreal spring}}, 
    72 author = {{M}arion {L}educ-{L}eballeur {G}aëlle {{d}e {C}oëtlogon} and {L}aurence {E}ymard},  
     72author = {{M}arion {L}educ-{L}eballeur and {G}aëlle {{d}e {C}oëtlogon} and {L}aurence {E}ymard},  
    7373abstract = {{The role of air-sea interactions in the boreal spring precipitation of the West African monsoon is explored through the wind variability in the Gulf of Guinea. Satellite measurements and reanalyses data are used to describe the atmosphere and the sea surface in the Gulf of Guinea from 2000 to 2009. Previous results showed a statistical link between the strengthening of southerlies between the Equator and the Guinean coast, and precipitation along the coast. In this study, linear regressions are first performed in May-June (2000-2009) to investigate the mechanisms at stake : an equatorial SST cooling strengthens the wind north of the equator, via the SST front located along 1\degreN. This wind acceleration intensifies the low atmospheric local circulation, which components are surface southerlies, coastal convergence, low atmosphere southward return flow, and subsidence over the Gulf of Guinea. When this circulation is stronger than normal, it brings more humidity toward the coast, which triggers deeper atmospheric convection and increases the coastal rainfall . In addition, an abrupt change in the surface wind pattern is observed between April and July. Composites are used to analyse temporal and spatial variations of the SST, surface wind speed and humidity, in surface as well as in altitude. A clear transition is observed during the spring season, when the wind strengthens between the equator and 5\degreN, which generally occurs at the end of May. Eventually, this study emphasizes very clearly the importance of the intraseasonal variability in the seasonal evolution and setting of the guinean coastal rainfall.}}, 
    7474language = {Anglais}, 
    … …  
    182182timestamp = {20130204}, 
    183183hal_id = {hal-00784292}, 
    184 author={A. Lenton and B. Tilbrook and R. Law and D. Bakker and S. C. Doney and N. Gruber and M. Hoppema and M. Ishii and N. S. Lovenduski and R. J. Matear and B. I. McNeil and {N}icolas {M}etzl and S. E. Mikaloff Fletcher and P. Monteiro and C. Rödenbeck and C. Sweeney and and T. Takahashi}, 
     184author={A. Lenton and B. Tilbrook and R. Law and D. Bakker and S. C. Doney and N. Gruber and M. Hoppema and M. Ishii and N. S. Lovenduski and R. J. Matear and B. I. McNeil and {N}icolas {M}etzl and S. E. {Mikaloff Fletcher} and P. Monteiro and C. Rödenbeck and C. Sweeney and T. Takahashi}, 
    185185title={Sea-air {CO$_{2}$} fluxes in the Southern Ocean for the period 1990-2009}, 
    186186ads={2013BGD....10..285L}, 
    … …  
    282282 
    283283 
    284 abstract = {{We present early mid-Holocene records of Sr/Ca, $\delta$18O and $\delta$18Osw from marine archives collected in Vanuatu: two Porites sp. corals (6.7-6.5 ka BP) and a Tridacna maxima giant clam (6.2-6.0 ka BP). Sr/Ca, $\delta$18O, and $\delta$18Osw were used as proxies for sea surface temperature (SST) and sea surface salinity (SSS). The fossil geochemical records were compared to modern Porites sp. and T. maxima records. Reconstructed mean SSTs from the two fossil Porites sp. and from the modern coral are similar, implying that the Western Pacific Warm Pool (WPWP)' southern edge had reached its modern location by 6.7-6.5 ka BP. The post-glacial SST rise in the Southwest Pacific was thus completed by the early mid-Holocene. The two early mid-Holocene corals and the giant clam recorded saltier conditions than modern related to 1) a decoupling between the precipitation regime and the SPCZ due to a northerly position of this climatic feature and 2) an increase of the moisture transport to the extra-tropics, driven by a strengthened or extended Hadley cell. The longest $\delta$18O coral profile displays an El Ni{\\~n}o Southern Oscillation (ENSO) signal reduced by 20-30\% compared to the period 1928-1992, in concordance with the reduced ENSO variability observed in the Pacific area during the first half of the Holocene. However, the decoupling between the SPCZ and the precipitation regime may have also contributed to the weak ENSO signal recorded in the early mid-Holocene coral $\delta$18O profile.}}, 
     284abstract = {{We present early mid-Holocene records of Sr/Ca, $\delta^{18}$O and $\delta^{18}$Osw from marine archives collected in Vanuatu: two Porites sp. corals (6.7-6.5 ka BP) and a Tridacna maxima giant clam (6.2-6.0 ka BP). Sr/Ca, $\delta^{18}$O, and $\delta^{18}$Osw were used as proxies for sea surface temperature (SST) and sea surface salinity (SSS). The fossil geochemical records were compared to modern Porites sp. and T. maxima records. Reconstructed mean SSTs from the two fossil Porites sp. and from the modern coral are similar, implying that the Western Pacific Warm Pool (WPWP)' southern edge had reached its modern location by 6.7-6.5 ka BP. The post-glacial SST rise in the Southwest Pacific was thus completed by the early mid-Holocene. The two early mid-Holocene corals and the giant clam recorded saltier conditions than modern related to 1) a decoupling between the precipitation regime and the SPCZ due to a northerly position of this climatic feature and 2) an increase of the moisture transport to the extra-tropics, driven by a strengthened or extended Hadley cell. The longest $\delta^{18}$O coral profile displays an El Ni{\\~n}o Southern Oscillation (ENSO) signal reduced by 20-30\% compared to the period 1928-1992, in concordance with the reduced ENSO variability observed in the Pacific area during the first half of the Holocene. However, the decoupling between the SPCZ and the precipitation regime may have also contributed to the weak ENSO signal recorded in the early mid-Holocene coral $\delta^{18}$O profile.}}, 
    285285keywords = {Biogeosciences: Paleoclimatology and paleoceanography (3344;4900);Atmospheric Processes: Paleoclimatology (0473;4900);}, 
    286286language = {Anglais}, 
    … …  
    346346title = {{Authigenic carbonates from active methane seeps offshore southwest Africa}}, 
    347347author = {{C}atherine {P}ierre and Marie-Madeleine Blanc-Valleron and Jérôme Demange and Omar Boudouma and Jean-Paul Foucher and Thomas Pape and Tobias Himmler and Noemi Fekete and Volkhard Spiess}, 
    348 abstract = {{The southwest African continental margin is well known for occurrences of active methane-rich fluid seeps associated with seafloor pockmarks at water depths ranging broadly from the shelf to the deep basins, as well as with high gas flares in the water column, gas hydrate accumulations, diagenetic carbonate crusts and highly diverse benthic faunal communities. During the M76/3a expedition of R/V METEOR in 2008, gravity cores recovered abundant authigenic carbonate concretions from three known pockmark sites--Hydrate Hole, Worm Hole, the Regab pockmark--and two sites newly discovered during that cruise, the so-called Deep Hole and Baboon Cluster. The carbonate concretions were commonly associated with seep-benthic macrofauna and occurred within sediments bearing shallow gas hydrates. This study presents selected results from a comprehensive analysis of the mineralogy and isotope geochemistry of diagenetic carbonates sampled at these five pockmark sites. The oxygen isotope stratigraphy obtained from three cores of 2-5 m length indicates a maximum age of about 60,000-80,000 years for these sediments. The authigenic carbonates comprise mostly magnesian calcite and aragonite, associated occasionally with dolomite. Their very low carbon isotopic compositions (-61.0 < $\delta$13C # V-PDB < -40.1) suggest anaerobic oxidation of methane (AOM) as the main process controlling carbonate precipitation. The oxygen isotopic signatures (+2.4 < $\delta$18O # V-PDB < +6.2) lie within the range in equilibrium under present-day/interglacial to glacial conditions of bottom seawater; alternatively, the most positive $\delta$18O values might reflect the contribution of 18O-rich water from gas hydrate decomposition. The frequent occurrence of diagenetic gypsum crystals suggests that reduced sulphur (hydrogen sulphide, pyrite) from sub-seafloor sediments has been oxidized by oxygenated bottom water. The acidity released during this process can potentially induce the dissolution of carbonate, thereby providing enough Ca2+ ions for pore solutions to reach gypsum saturation; this is thought to be promoted by the bio-irrigation and burrowing activity of benthic fauna. The $\delta$18O-$\delta$13C patterns identified in the authigenic carbonates are interpreted to reflect variations in the rate of AOM during the last glacial-interglacial cycle, in turn controlled by variably strong methane fluxes through the pockmarks. These results complement the conclusions of Kasten et al. in this special issue, based on authigenic barite trends at the Hydrate Hole and Worm Hole pockmarks which were interpreted to reflect spatiotemporal variations in AOM related to subsurface gas hydrate formation-decomposition.}}, 
     348abstract = {{The southwest African continental margin is well known for occurrences of active methane-rich fluid seeps associated with seafloor pockmarks at water depths ranging broadly from the shelf to the deep basins, as well as with high gas flares in the water column, gas hydrate accumulations, diagenetic carbonate crusts and highly diverse benthic faunal communities. During the M76/3a expedition of R/V METEOR in 2008, gravity cores recovered abundant authigenic carbonate concretions from three known pockmark sites--Hydrate Hole, Worm Hole, the Regab pockmark--and two sites newly discovered during that cruise, the so-called Deep Hole and Baboon Cluster. The carbonate concretions were commonly associated with seep-benthic macrofauna and occurred within sediments bearing shallow gas hydrates. This study presents selected results from a comprehensive analysis of the mineralogy and isotope geochemistry of diagenetic carbonates sampled at these five pockmark sites. The oxygen isotope stratigraphy obtained from three cores of 2-5 m length indicates a maximum age of about 60,000-80,000 years for these sediments. The authigenic carbonates comprise mostly magnesian calcite and aragonite, associated occasionally with dolomite. Their very low carbon isotopic compositions (-61.0 < $\delta^{13}$C \textperthousand V-PDB < -40.1) suggest anaerobic oxidation of methane (AOM) as the main process controlling carbonate precipitation. The oxygen isotopic signatures (+2.4 < $\delta^{18}$O \textperthousand V-PDB < +6.2) lie within the range in equilibrium under present-day/interglacial to glacial conditions of bottom seawater; alternatively, the most positive $\delta^{18}$O values might reflect the contribution of 18O-rich water from gas hydrate decomposition. The frequent occurrence of diagenetic gypsum crystals suggests that reduced sulphur (hydrogen sulphide, pyrite) from sub-seafloor sediments has been oxidized by oxygenated bottom water. The acidity released during this process can potentially induce the dissolution of carbonate, thereby providing enough Ca2+ ions for pore solutions to reach gypsum saturation; this is thought to be promoted by the bio-irrigation and burrowing activity of benthic fauna. The $\delta^{18}$O-$\delta^{13}$C patterns identified in the authigenic carbonates are interpreted to reflect variations in the rate of AOM during the last glacial-interglacial cycle, in turn controlled by variably strong methane fluxes through the pockmarks. These results complement the conclusions of Kasten et al. in this special issue, based on authigenic barite trends at the Hydrate Hole and Worm Hole pockmarks which were interpreted to reflect spatiotemporal variations in AOM related to subsurface gas hydrate formation-decomposition.}}, 
    349349language = {Anglais}, 
    350350affiliation = {Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Institut des Sciences de la Terre de Paris - iSTeP , D{\'e}partement G{\'e}osciences Marines}, 
    … …  
    526526timestamp = {20121123}, 
    527527} 
     528 
    528529@unpublished{GarbeRutgerssonEtAl:OAIGP:2012inreview, 
    529530loceanaffectation = {cnrs}, 
    … …  
    531532loceanteam = {surf}, 
    532533timestamp = {20121123}, 
    533 author={C. Garbe and A. Rutgersson and {J}acqueline {B}outin and B. Delillen and C.W. Fairall and N. Grubera and J. Hare and D. Ho and M. Johnson and G. de Leeuw and P.D. Nightingale et al.}, 
     534author={C. Garbe and A. Rutgersson and {J}acqueline {B}outin and B. Delillen and C.W. Fairall and N. Grubera and J. Hare and D. Ho and M. Johnson and G. de Leeuw and P.D. Nightingale and al.}, 
    534535title={Transfer across the air-sea interface}, 
    535536year={2012}, 
    … …  
    672673timestamp={20121115}, 
    673674title = {{Reconstruction of pAST climates from sedimentary biomarkers. {A}ncient molecules for past climate reconstructions: a large field of application for spectroscopic methods.}}, 
    674 author = {{J}érémy {J}acob and {J}ean-{R}obert {D}isnar and {Y}ongsong {H}uang and {M}ohammed {B}oussafir and  {A}bdelfettah {S}ifeddine and {A}na {L}uiza {S}padano {A}lbuquerque and {B}runo {T}urcq}, 
     675author = {{J}érémy {J}acob and {J}ean-{R}obert {D}isnar and {Y}ongsong {H}uang and {M}ohammed {B}oussafir and {A}bdelfettah {S}ifeddine and {A}na {L}uiza {S}padano {A}lbuquerque and {B}runo {T}urcq}, 
    675676abstract = {{Although we have now a better picture of past climates, there are still numerous questions that remain unsolved. {T}hese uncertainties primarily arise from the possible human impact on climate dynamics, the need to assess feedbacks from the biosphere and to better understand and anticipate natural variability of climate (forcing mechanisms, time lags...). {I}n order to record past climatic and environmental changes, numerous tools have been applied to multiple records. {T}he direct interpretation of these data in terms of climatic parameters is sometimes questionable and strengthens the necessity for more accurate paleodata from sedimentary archives. {S}edimentary organic matter is a renewing target for paleoclimate information because it derives from living organisms that are sensible to environmental changes and its complexity promises a virtually infinite source of information. {I}n order to access this information at a molecular or isotopic level, the organic geochemist must now use a large panel of spectroscopic tools (GC-MS, HPLC-MS and GC-IRMS). I will here present some recent advances in the field of molecular and compound-specific isotopes applications to paleoclimate reconstructions. {S}o as to estimate the impact of climatic changes on the ecosystems, paleoflora can be deciphered from the occurrence, in the sediments, of taxon-specific molecules. {S}imilarly, the physico-chemical conditions that prevailed at time of deposition of the sediment are accessible by the study of diagenetic by-products, derived from the alteration of biomolecules. {O}ther molecules are produced by organisms as a response to the variations of environmental/climatic parameters. {T}heir identification and quantitation in sediments can be used as a proxy of these parameters. {F}inally, the recent development of compound-specific isotope techniques allows measuring the isotopic composition ($\Delta$D, $\Delta$13C, 15N...) of single molecules, therefore affording a better constrain on the significance of isotopic signatures.}}, 
    676677language = {{A}nglais}, 
    … …  
    762763timestamp={20121115}, 
    763764url = {http://hal-insu.archives-ouvertes.fr/hal-00068937}, 
    764 title = {{L}a sédimentation organique lacustre en zone tropicale sud au cours des 36 O00 dernières années (Lac {T}ritrivakely, {M}adagascar)}, 
     765title = {{L}a sédimentation organique lacustre en zone tropicale sud au cours des 36 000 dernières années (Lac {T}ritrivakely, {M}adagascar)}, 
    765766author = {{A}bdelfettah {S}ifeddine and {F}atima {L}aggoun-{D}éfarge and {E}lisabeth {L}allier-{V}ergès and {J}ean-{R}obert {D}isnar and {D}avid {W}illiamson and {F}rançoise {G}asse and {E}lisabeth {G}ibert}, 
    766767abstract = {{L'étude pétrographique (palynofaciès) et géochimique (pyrolyse {R}ock {E}val) de la matière organique sédimentaire d'une carotte prélevée dans un lac de cratère de {M}adagascar révèle une sédimentation organique de type tourbeux avant 36 ka, entre ca 28 et 15 ka et entre 6 et O ka, mise en place au cours de périodes d'asséchement. {E}ntre ca 36 et 28 ka, elle se caractérise par une sédimentation lacustre (phytoplancton dominant) et des migrations de végétation du bassin versant vers le lac luimême. {D}es apports de matière organique allochtone témoignent de I'établissement d'un couvert végétal sur le bassin versant et du lessivage de sols, lors des périodes humides. {L}es variations d'\&cosystèmes et de peuplement sont à mettre en relation avec I'évolution du régime hydroclimatique depuis 36 ka, en termes de périodes sèches et humides. {P}etrographic (palynofacies) and geochemical (Rock {E}va1 pyrolysis) studies of sedimentary organic matter of a core from a crater lake in {M}adagascar show a peaty sedimentation before 36 ky and between ca 28 and 15 ky, and between 6 and O ky. {B}etween 36 and 28 ky, the organic sedimentation is characterized by an alternance between phytoplanktonic sedimentation and migrations of vegetation from the basin slope to the lake itself. {C}ontributions of oxidized allochthonous organic matter prove also the presence of vegetation on the surrounding basin and soil leaching. {T}he variation of the ecosystems and their development reveal the hydroclimatic changes during the last 36 kyrs, in terms of arid and humid periods.}}, 
    … …  
    797798loceanbibid = {01900}, 
    798799timestamp={20121115}, 
    799 title = {{Etude de la sedimentation lacustre d'un site de foret d'altitude des {A}ndes centrales (Bolivie); implications paleoclimatiques}}, 
     800title = {{É}tude de la sédimentation lacustre d'un site de forêt d'altitude des {A}ndes centrales (Bolivie); implications paléoclimatiques}, 
    800801author = {{A}bdelfettah {S}ifeddine and {J}acques {B}ertaux and {P}hilippe {M}ourguiart and {L}ouis {M}artin and {J}ean-{R}obert {D}isnar and {F}atima {L}aggoun-{D}éfarge and {J}aime {A}rgollo}, 
    801802abstract = {{A sedimentological study of a 755 cm length core sampled in the middle of a marshy depression surrounded by a cloud forest in the central {A}ndes reveals that this site has recorded important environmental variations during the last 50000 years. {F}or the most part (625 cm) the core is composed of detrital rich sediments deposited during the {U}pper {P}leistocene. {T}he highest amount of detrital influx underlines the {L}ast {G}lacial {M}aximum which ranges from ca 29,000 14 C yr B.P. to ca 16,000 14 C yr B.P. (ca 18,500 cal yr B.P.), between two relatively humid phases. {T}he sedimentation of the present {I}nterglacial, starting at ca 12,500 14 C yr B.P. (14,500 cal yr B.P.), is mainly organic, as a consequence of the great development of soils and the forest vegetal cover all over the catchment area. {T}he maximum extension of this vegetal cover ranging from 12,500 to ca 10,500 14 C yr B.P. (14,500 and 12,400 cal yr B.P.) is followed from 10,500 to 8,000 14 C yr B.P. (12,400 and 8,800 cal yr B.P.) by a drier period as revealed by the occurrence of micro-charcoals in the sediment. {B}etween ca 8,000 and 4,000 14 C yr B.P. (8,800 and 4,500 cal yr B.P.), the sharp increase of micro-charcoals content, likely related to palaeofires, underlines an intensification of this dry trend.}}, 
    … …  
    833834title = {{Major environmental changes recorded by lacustrine sedimentary organic matter since the {L}ast {G}lacial {M}aximum near the {E}quator (Lagoa do {C}açó, NE {B}razil).}}, 
    834835author = {{J}érémy {J}acob and {J}ean-{R}obert {D}isnar and {M}ohammed {B}oussafir and {A}bdelfettah {S}ifeddine and {B}runo {T}urcq and {A}na {L}uiza {S}padano {A}lbuquerque}, 
    835 abstract = {{Sediment samples collected along a 6-m core, drilled in the deepest part of the {L}agoa do {C}açó (NE {B}razil), have been investigated in order to determine source(s) and degradation conditions of the organic matter (OM) with special emphasis on paleoenvironmental implications. {B}ulk organic geochemistry (Rock-{E}val pyrolysis, C/N determination, $\delta$13C and $\delta$15N measurement) and petrography combined with sedimentological evidence and radiocarbon dates allowed to identify four major intervals documenting major environmental changes that occurred during the last 20,000 years. {T}he first interval, dating back to the end of the {L}ast {G}lacial {M}aximum (LGM), contains well-preserved OM derived from higher plants. {T}his material was most probably produced in an ephemeral palustrine system and rapidly buried by sands. {T}his level is thought to have been deposited under relatively arid climate conditions associated with strong but episodic rainfalls. {B}etween 19,240 and 17,250 {C}al years BP, the climate appears to have been more humid and seasonality more pronounced as suggested by the presence of a permanent lake. {A}fter a drastic environmental change dating back to 17,250 {C}al years BP, the sediment became truly lacustrine with restricted mineral input and highly degraded higher plant-derived organic matter. {A}fter that, a stepwise improvement in the preservation of OM occurred, as revealed by several pronounced shifts in the {R}ock-{E}val {T}pS2 signal. {T}hese changes could document abrupt climatically driven changes during the {L}ate {G}lacial. {F}inally, around 5610 {C}al years BP, environmental conditions, approaching those prevailing today were established. {M}inor climatic changes during the {H}olocene were probably buffered by a high water table which might explain the lack of paleoenvironmental fluctuations.}}, 
     836abstract = {{Sediment samples collected along a 6-m core, drilled in the deepest part of the {L}agoa do {C}açó (NE {B}razil), have been investigated in order to determine source(s) and degradation conditions of the organic matter (OM) with special emphasis on paleoenvironmental implications. {B}ulk organic geochemistry (Rock-{E}val pyrolysis, C/N determination, $\delta^{13}$C and $\delta^{15}$N measurement) and petrography combined with sedimentological evidence and radiocarbon dates allowed to identify four major intervals documenting major environmental changes that occurred during the last 20,000 years. {T}he first interval, dating back to the end of the {L}ast {G}lacial {M}aximum (LGM), contains well-preserved OM derived from higher plants. {T}his material was most probably produced in an ephemeral palustrine system and rapidly buried by sands. {T}his level is thought to have been deposited under relatively arid climate conditions associated with strong but episodic rainfalls. {B}etween 19,240 and 17,250 {C}al years BP, the climate appears to have been more humid and seasonality more pronounced as suggested by the presence of a permanent lake. {A}fter a drastic environmental change dating back to 17,250 {C}al years BP, the sediment became truly lacustrine with restricted mineral input and highly degraded higher plant-derived organic matter. {A}fter that, a stepwise improvement in the preservation of OM occurred, as revealed by several pronounced shifts in the {R}ock-{E}val {T}pS2 signal. {T}hese changes could document abrupt climatically driven changes during the {L}ate {G}lacial. {F}inally, around 5610 {C}al years BP, environmental conditions, approaching those prevailing today were established. {M}inor climatic changes during the {H}olocene were probably buffered by a high water table which might explain the lack of paleoenvironmental fluctuations.}}, 
    836837keywords = {{B}razil; {L}acustrine organic matter; {P}aleoenvironments; {P}aleoclimate; {R}ock-{E}val; {O}rganic petrography}, 
    837838language = {{A}nglais}, 
    … …  
    10111012year = {2004}, 
    10121013} 
     1014 
    10131015@inproceedings{TreguierBarnierEtAl:RCCISC:2006, 
    10141016hal_id = {hal-00252101}, 
    … …  
    11301132title = {{Distributions of oxygen and carbon stable isotopes and CFC-12 in the water masses of the {S}outhern {O}cean at 30°E from {S}outh {A}frica to {A}ntarctica: results of the CIVA1 cruise}}, 
    11311133author = {{A}nne-{S}ophie {A}rchambeau and {C}atherine {P}ierre and {A}lain {P}oisson and {B}ernard {S}chauer}, 
    1132 abstract = {{This study presents oceanic distributions of stable isotopes ($\delta$18O of water and $\delta$13C of $\Sigma${CO$_{2}$}) and CFC-12 from samples collected during the CIVA1 cruise (February/March 1993), across the {S}outhern {O}cean, along a meridian section at 30°E, from {S}outh {A}frica (44°S) to {A}ntarctica (70°S). {T}he isotopic measurements show important variations between the subantarctic surface waters with low $\delta$18O--high $\delta$13C values and the antarctic surface waters with very low $\delta$18O--low $\delta$13C values. {T}he surface distributions of $\delta$13C values follow the major frontal oceanic structures; the vertical distribution shows the progressive upwelling from the subantarctic zone to the antarctic divergence of 13C-depleted {CO$_{2}$} derived from remineralization of organic matter. {A}long the {A}ntarctic continental shelf, between 2500 and 4000 m, a core of water with $\delta$18O values close to --0.1 is associated with a relative maximum in CFC-12 concentration, although this core is not detected by its temperature and salinity parameters. {T}his water mass, which corresponds to recently formed deep water, may originate from the eastward extension of the {W}eddell gyre or from bottom waters coming from the {E}ast and formed near {P}rydz {B}ay.}}, 
     1134abstract = {{This study presents oceanic distributions of stable isotopes ($\delta^{18}$O of water and $\delta^{13}$C of $\Sigma${CO$_{2}$}) and CFC-12 from samples collected during the CIVA1 cruise (February/March 1993), across the {S}outhern {O}cean, along a meridian section at 30°E, from {S}outh {A}frica (44°S) to {A}ntarctica (70°S). {T}he isotopic measurements show important variations between the subantarctic surface waters with low $\delta^{18}$O--high $\delta^{13}$C values and the antarctic surface waters with very low $\delta^{18}$O--low $\delta^{13}$C values. {T}he surface distributions of $\delta^{13}$C values follow the major frontal oceanic structures; the vertical distribution shows the progressive upwelling from the subantarctic zone to the antarctic divergence of 13C-depleted {CO$_{2}$} derived from remineralization of organic matter. {A}long the {A}ntarctic continental shelf, between 2500 and 4000 m, a core of water with $\delta^{18}$O values close to --0.1 is associated with a relative maximum in CFC-12 concentration, although this core is not detected by its temperature and salinity parameters. {T}his water mass, which corresponds to recently formed deep water, may originate from the eastward extension of the {W}eddell gyre or from bottom waters coming from the {E}ast and formed near {P}rydz {B}ay.}}, 
    11331135keywords = {{S}table isotopes; 18O; 13C; CFC-12; {A}ustral {O}cean}, 
    11341136language = {{A}nglais}, 
    … …  
    11431145year = {1998}, 
    11441146pdf = {http://hal.ird.fr/ird-00145342/PDF/asa\_JMS.pdf}, 
     1147ads={1998JMS....17...25A}, 
    11451148} 
    11461149 
    … …  
    11831186timestamp={20121014}, 
    11841187title = {{Organic-rich sediments in ventilated deep-sea environments: {R}elationship to climate, sea level, and trophic changes}}, 
    1185 author = {{P}hilippe {B}ertrand and T. F. {P}edersen and R. {S}chneider and G. {S}himmield and  {E}lisabeth {L}allier-{V}ergès and {J}ean-{R}obert {D}isnar and D. {M}assias and J. {V}illanueva and {N}icolas {T}ribovillard and {A}lain-{Y}ves {H}uc and X. {G}iraud and {C}atherine {P}ierre and M.T. {V}énec-{P}eyré}, 
     1188author = {{P}hilippe {B}ertrand and T. F. {P}edersen and R. {S}chneider and G. {S}himmield and {E}lisabeth {L}allier-{V}ergès and {J}ean-{R}obert {D}isnar and D. {M}assias and J. {V}illanueva and {N}icolas {T}ribovillard and {A}lain-{Y}ves {H}uc and X. {G}iraud and {C}atherine {P}ierre and M.T. {V}énec-{P}eyré}, 
    11861189abstract = {{Sediments on the {N}amibian {M}argin in the SE {A}tlantic between water depths of $\sim$1000 and $\sim$3600 m are highly enriched in hydrocarbon-prone organic matter. {S}uch sedimentation has occurred for more than 2 million years and is geographically distributed over hundreds of kilometers along the margin, so that the sediments of this region contain a huge concentrated stock of organic carbon. {I}t is shown here that most of the variability in organic content is due to relative dilution by buried carbonates. {T}his reflects both export productivity and diagenetic dissolution, not differences in either water column or bottom water anoxia and related enhanced preservation of organic matter. {T}hese observations offer a new mechanism for the formation of potential source rocks in a well-ventilated open ocean, in this case the {S}outh {A}tlantic. {T}he organic richness is discussed in terms of a suite of probable controls including local wind-driven productivity (upwelling), trophic conditions, transfer efficiency, diagenetic processes, and climate-related sea level and deep circulation. {T}he probability of past occurrences of such organic-rich facies in equivalent oceanographic settings at the edge of large oceanic basins should be carefully considered in deep offshore exploration.}}, 
    11871190language = {{A}nglais}, 
    … …  
    12431246affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {L}aboratorio de {A}rbovirus , {U}nité de recherches en virologie , {I}nstitut {E}vandro {C}hagas-FNS}, 
    12441247pages = {128-136}, 
    1245 journal = {{B}ulletin de la {S}ociété de pathologie exotique (1990)}, 
     1248journal = {{B}ulletin de la {S}ociété de pathologie exotique}, 
    12461249volume = {89}, 
    12471250audience = {internationale}, 
    … …  
    12501253} 
    12511254 
    1252 @article{tagliabue:hal-00330335, 
     1255@article{TagliabueBoppEtAl:B:2008, 
    12531256hal_id = {hal-00330335}, 
    12541257loceanbibid = {01872}, 
    … …  
    12751278timestamp={20121014}, 
    12761279title = {{Why climate sensitivity may not be so unpredictable ?}}, 
    1277 author = {{A}lexis {H}annart and {J}ean-{L}ouis {D}ufresne and {P}hilipe {N}aveau}, 
     1280author = {{A}lexis {H}annart and {J}ean-{L}ouis {D}ufresne and {P}hilippe {N}aveau}, 
    12781281abstract = {{Different explanations have been proposed as to why the range of climate sensitivity predicted by GCMs have not lessened substantially in the last decades, and subsequently if it can be reduced. {O}ne such study (\textit{Why is climate sensitivity so unpredictable?}, \cite{RB07}) adressed these questions using rather simple theoretical considerations and reached the conclusion that reducing uncertainties on climate feedbacks and underlying climate processes will not yield a large reduction in the envelope of climate sensitivity. {I}n this letter, we revisit the premises of this conclusion. {W}e show that it results from a mathematical artefact caused by peculiar definitions of uncertainty used by these authors. {A}pplying standard concepts and definitions of descriptive statistics to the exact same framework of analysis as {R}oe and {B}aker, we show that within this simple framework, reducing inter-model spread on feedbacks does in fact induce a reduction of uncertainty on climate sensitivity, almost proportionally. {T}herefore, following {R}oe and {B}aker assumptions, climate sensitivity is actually not so unpredictable. \%We then briefly focus on ongoing advances in cloud physics that may narrow the spread on feedbacks, thus reducing the uncertainty on climate sensitivity.}}, 
    12791282language = {{A}nglais}, 
    … …  
    13291332publisher = {{B}ackhuys {P}ublishers, {L}eiden}, 
    13301333pages = {215-223}, 
    1331 editor = {A.H.L. {H}uiskes and  W.W.C.  {G}ieskes and J. {R}ozema and R.M.L. {S}chornoa and S.M. van der {V}ies and W.J {W}olf}, 
     1334editor = {A.H.L. {H}uiskes and  W.W.C. {G}ieskes and J. {R}ozema and R.M.L. {S}chornoa and S.M. van der {V}ies and W.J {W}olf}, 
    13321335series = {ISBN 90 5782 0879 X}, 
    13331336year = {2003}, 
    … …  
    15171520timestamp={20121014}, 
    15181521title = {{Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organisms}}, 
    1519 author = {{J}ames C. {O}rr and {V}ictoria J. {F}abry and {O}livier {A}umont and  {L}aurent {B}opp and {S}cott C. {D}oney and {R}ichard A. {F}eely and {A}nand {G}nanadesikan and {N}icolas {G}ruber and {A}kio {I}shida and {F}ortunat {J}oos and {R}obert M. {K}ey and {K}eith {L}indsay and {E}rnst {M}aier-{R}eimer and {R}ichard J. {M}atear and {P}atrick {M}onfray and {A}nne {M}ouchet and {R}aymond G. {N}ajjar and {G}ian-{K}asper {P}lattner and {K}eith B. {R}odgers and {C}hristopher L. {S}abine and {J}orge L. {S}armiento and {R}einer {S}chlitzer and {R}ichard D. {S}later and {I}an J. {T}otterdell and {M}arie-{F}rance {W}eirig and {Y}asuhiro {Y}amanaka and {A}ndrew {Y}ool}, 
     1522author = {{J}ames C. {O}rr and {V}ictoria J. {F}abry and {O}livier {A}umont and {L}aurent {B}opp and {S}cott C. {D}oney and {R}ichard A. {F}eely and {A}nand {G}nanadesikan and {N}icolas {G}ruber and {A}kio {I}shida and {F}ortunat {J}oos and {R}obert M. {K}ey and {K}eith {L}indsay and {E}rnst {M}aier-{R}eimer and {R}ichard J. {M}atear and {P}atrick {M}onfray and {A}nne {M}ouchet and {R}aymond G. {N}ajjar and {G}ian-{K}asper {P}lattner and {K}eith B. {R}odgers and {C}hristopher L. {S}abine and {J}orge L. {S}armiento and {R}einer {S}chlitzer and {R}ichard D. {S}later and {I}an J. {T}otterdell and {M}arie-{F}rance {W}eirig and {Y}asuhiro {Y}amanaka and {A}ndrew {Y}ool}, 
    15201523language = {{A}nglais}, 
    15211524affiliation = {{L}aboratoire des sciences du climat et de l'environnement - LSCE , {D}epartment of {B}iological {S}ciences , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {W}oods {H}ole {O}ceanographic {I}nstitution , {P}acific {M}arine {E}nvironmental {L}aboratory , {G}eophysical {F}luid {D}ynamics {L}aboratory , {I}nstitute of {G}eophysics and {P}lanetary {P}hysics [Los {A}ngeles] - IGPP , {F}rontier {R}esearch {C}enter for {G}lobal {C}hange , {C}limate and {E}nvironmental {P}hysics, {P}hysics {I}nstitute , {A}tmospheric and {O}ceanic {S}ciences (AOS) {P}rogram , {N}ational {C}enter for {A}tmospheric {R}esearch - NCAR , {M}ax {P}lanck {I}nstitut für {M}eteorologie , {M}arine {R}esearch and {A}ntarctic {C}limate and {E}cosystems CRC , {A}strophysics and {G}eophysics {I}nstitute , {D}epartment of {M}eteorology, {P}ennsylvania {S}tate {U}niversity , {D}epartment of {B}entho-pelagic processes , {N}ational {O}ceanography {C}entre {S}outhampton}, 
    … …  
    23582361} 
    23592362 
    2360 @article{servain:hal-00161925, 
     2363@article{ServainSmithEtAl:BAMS:2004, 
    23612364hal_id = {hal-00161925}, 
    23622365loceanbibid = {01808}, 
    … …  
    24312434timestamp={20121012}, 
    24322435title = {{Life at cold seeps : a synthesis of biogeochemical and ecological data from {K}azan mud volcano, eastern {M}editerranean {S}ea}}, 
    2433 author = {{J}osef P. {W}erne and {R}alf R. {H}aese and {T}iphaine {Z}itter and {G}iovanni {A}loisi and {I}onna {B}ouloubassi and {S}ander {H}eijs and {A}line {F}iala-{M}édioni and {R}ichard D. {P}ancost and {J}aap S. {S}inninghe {D}amsté and {G}ert {D}e {L}ange and {L}arry J. {F}orney and {J}an C. {G}ottschal and {J}ean-{P}aul {F}oucher and {J}ean {M}ascle and {J}ohn {W}oodside}, 
     2436author = {{J}osef P. {W}erne and {R}alf R. {H}aese and {T}iphaine {Z}itter and {G}iovanni {A}loisi and {I}oanna {B}ouloubassi and {S}ander {H}eijs and {A}line {F}iala-{M}édioni and {R}ichard D. {P}ancost and {J}aap S. {S}inninghe {D}amsté and {G}ert {D}e {L}ange and {L}arry J. {F}orney and {J}an C. {G}ottschal and {J}ean-{P}aul {F}oucher and {J}ean {M}ascle and {J}ohn {W}oodside}, 
    24342437language = {{A}nglais}, 
    24352438affiliation = {{D}epartment of {M}arine {B}iogeochemistry and {T}oxicology - NIOZ , {D}epartment of {G}eochemistry {F}aculty of {E}arth {S}ciences , {D}epartment of {S}edimentology and {M}arine {G}eology {F}aculty of {E}arth and {L}ife {S}ciences , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratoire de {C}himie et {B}iogéochimie {M}arines , {D}epartment of {M}icrobiology , {L}aboratoire d'océanographie biologique de {B}anyuls - LOBB , {D}épartement {G}éosciences {M}arines , {G}éoazur - GEOAZUR , {C}entre for {M}arine {E}arth {S}cience}, 
    … …  
    24612464timestamp={20121012}, 
    24622465title = {{CH4-consuming microorganisms and the formation of carbonate crusts at cold-seeps}}, 
    2463 author = {{G}iovanni {A}loisi and {I}oanna {B}ouloubassi and {S}ander {H}eijs and {R}ichard {P}ancost and {C}atherine {P}ierre and {D}amsté {J}aap S. {S}inninghe and {J}an C. {G}ottschaland {L}arry J. {F}orney and J.-{M}. {R}ouchy}, 
     2466author = {{G}iovanni {A}loisi and {I}oanna {B}ouloubassi and {S}ander {H}eijs and {R}ichard {P}ancost and {C}atherine {P}ierre and {D}amsté {J}aap S. {S}inninghe and {J}an C. {G}ottschaland and {L}arry J. {F}orney and J.-{M}. {R}ouchy}, 
    24642467language = {{A}nglais}, 
    24652468affiliation = {{L}aboratoire d'océanographie dynamique et de climatologie - LODYC , {L}aboratoire de biogéochimie et chimie marines - LBCM}, 
    … …  
    24782481title = {{Hydrology and circulation in the {S}trait of {H}ormuz and the {G}ulf of {O}man-{R}esults from the GOGP99 {E}xperiment: 2. {G}ulf of {O}man.}}, 
    24792482author = {{S}téphane {P}ous and X. {C}arton and P. {L}azure}, 
    2480 abstract = {{Hydrological, ADCP, and drifting buoy data obtained during the GOGP99 {E}xperiment in {O}ctober and early {N}ovember 1999 are analyzed to describe the {P}ersian {G}ulf {W}ater (PGW) core and the regional circulation in the {G}ulf of {O}man. {T}he warm and salty PGW core flows out of the {S}trait of {H}ormuz heading southeastward unto (25°20#N, 57°E), approximately. {F}rom there, it cascades down the continental slope, veers southwestward, and joins the {O}mani coast near (24°50#N, 56°50#E) to form a slope current. {T}his PGW current has then thermohaline maxima on isopycnal $\sigma$0 = 26.5, near 220 m depth. {I}ts thermohaline characteristics decrease along its progression to {R}a's al {H}add (and then offshore into the {A}rabian {S}ea) but maintain a sharp contrast with surrounding waters. {O}utflow variability at the {S}trait of {H}ormuz can be related to downstream fluctuations of the thermohaline maxima in the PGW core at gulf scale and over a 2- to 3-week period. {M}oreover, several mechanisms (baroclinic instability, flow intermittency, cape effects) are examined to explain the widening of this PGW core upstream and downstream of {R}a's al {H}amra. {I}n the eastern part of the {G}ulf of {O}man, the regional circulation is a cyclonic gyre. {T}he circulation in the western part of the {G}ulf is more complex, with the outflow of PGW and southeastward currents in the upper 250 m near the {O}mani coast, and a recirculation of upwelled waters near {R}a's {J}agin (on the {I}ranian coast). {T}he large cyclonic gyre occupies at least the upper 300 m of the water column and undergoes little variation over a month. {T}he PGW outflow in the northern {A}rabian {S}ea is southward and located 50--100 km from the coast. {I}t borders a shallower northward current located offshore.}}, 
     2483abstract = {{Hydrological, ADCP, and drifting buoy data obtained during the GOGP99 {E}xperiment in {O}ctober and early {N}ovember 1999 are analyzed to describe the {P}ersian {G}ulf {W}ater (PGW) core and the regional circulation in the {G}ulf of {O}man. {T}he warm and salty PGW core flows out of the {S}trait of {H}ormuz heading southeastward unto (25°20'N, 57°E), approximately. {F}rom there, it cascades down the continental slope, veers southwestward, and joins the {O}mani coast near (24°50'N, 56°50'E) to form a slope current. {T}his PGW current has then thermohaline maxima on isopycnal $\sigma$0 = 26.5, near 220 m depth. {I}ts thermohaline characteristics decrease along its progression to {R}a's al {H}add (and then offshore into the {A}rabian {S}ea) but maintain a sharp contrast with surrounding waters. {O}utflow variability at the {S}trait of {H}ormuz can be related to downstream fluctuations of the thermohaline maxima in the PGW core at gulf scale and over a 2- to 3-week period. {M}oreover, several mechanisms (baroclinic instability, flow intermittency, cape effects) are examined to explain the widening of this PGW core upstream and downstream of {R}a's al {H}amra. {I}n the eastern part of the {G}ulf of {O}man, the regional circulation is a cyclonic gyre. {T}he circulation in the western part of the {G}ulf is more complex, with the outflow of PGW and southeastward currents in the upper 250 m near the {O}mani coast, and a recirculation of upwelled waters near {R}a's {J}agin (on the {I}ranian coast). {T}he large cyclonic gyre occupies at least the upper 300 m of the water column and undergoes little variation over a month. {T}he PGW outflow in the northern {A}rabian {S}ea is southward and located 50--100 km from the coast. {I}t borders a shallower northward current located offshore.}}, 
    24812484keywords = {{G}ulf of {O}man; regional circulation; {P}ersian {G}ulf {W}ater outflow.}, 
    24822485language = {{A}nglais}, 
    … …  
    25462549loceanaffectation={cnrs}, 
    25472550title = {{Mean circulations and variability between 1958 and 2004 as simulated by the DAKKAR eddy permitting 1\/4° global ocean/sea ice model driven by CORE or ERA40 atmospheric forcing}}, 
    2548 author = {{B}ernard {B}arnier and  {T}hierry {P}enduff and {J}ean-{M}arc {M}olines and {A}nne-{M}arie {T}réguier and {A}rne {B}iastoch and {G}urvan {M}adec and {C}laus {B}öning}, 
     2551author = {{B}ernard {B}arnier and {T}hierry {P}enduff and {J}ean-{M}arc {M}olines and {A}nne-{M}arie {T}réguier and {A}rne {B}iastoch and {G}urvan {M}adec and {C}laus {B}öning}, 
    25492552language = {{A}nglais}, 
    25502553affiliation = {{L}aboratoire des écoulements géophysiques et industriels - LEGI , {I}fM-GEOMAR , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC}, 
    … …  
    25742577year = {2004}, 
    25752578} 
    2576 tbin/bash:}errada},: command not found 
     2579 
    25772580@article{Park:GRL:2004, 
    25782581hal_id = {hal-00164938}, 
    25792582loceanbibid = {01795}, 
    25802583timestamp = {20121108}, 
    2581 title = {{Determination of the surface geostrophic velocity field from satellite altimetry}}, 
     2584title = {{D}etermination of the surface geostrophic velocity field from satellite altimetry}, 
    25822585author = {{Y}oung-{H}yang {P}ark}, 
    2583 abstract = {{Determination of the surface geostrophic velocity field from satellite altimetryPresently available marine geoid models are not accurate enough to extract the mean surface circulation directly from satellite altimetry. A novel method for estimating the mean velocity field of major ocean current systems is derived from the free surface boundary condition. {W}ith a given quasi-geostrophic balance for the horizontal surface flow, a scaling analysis of this boundary condition indicates that although the vertical velocity w is mostly balanced by the local change of the free surface, $\partial$$\eta$#/$\partial$t, useful information on the mean current (u overline, v overline) is contained in a small ageostrophic departure ($\partial$$\eta$#/$\partial$t -- w). {O}ur method consists in the development of a simple algebraic equation with two unknowns (u overline, v overline) and an adjustable parameter inline equation associated with $\partial$$\eta$#/$\partial$t, assuming that the latter is proportional to ($\partial$$\eta$#/$\partial$t -- w). {M}ost interestingly, $\partial$$\eta$#/$\partial$t and all other coefficients of the equation can be determined from altimetry. {T}he altimeter data used is combined TOPEX/Poseidon-ERS gridded data, and the solution is obtained by least squares, minimizing the contribution from the time-variable part of the parameter inline equation and prescribing the zonal direction of the mean current. {T}he method, which is found to be particularly useful for quasi-zonal high-energy current systems, has been validated against direct observations in the {G}ulf {S}tream and {S}outhern {O}cean. {C}omparisons with direct observations and {M}onte {C}arlo experiments suggest an overall solution error of about 10 cm s--1. {O}nce calibrated against regional velocity statistics, this method will be able to determine from altimetry the mean or instantaneous surface velocity field down to the frontal scale, with a realism that has been inaccessible because of the geoid constraint.}}, 
     2586abstract = {Determination of the surface geostrophic velocity field from satellite altimetryPresently available marine geoid models are not accurate enough to extract the mean surface circulation directly from satellite altimetry. A novel method for estimating the mean velocity field of major ocean current systems is derived from the free surface boundary condition. {W}ith a given quasi-geostrophic balance for the horizontal surface flow, a scaling analysis of this boundary condition indicates that although the vertical velocity w is mostly balanced by the local change of the free surface, $\partial$$\eta^\prime$$\partial$t, useful information on the mean current (u overline, v overline) is contained in a small ageostrophic departure ($\partial$$\eta^\prime$$\partial$t -- w). {O}ur method consists in the development of a simple algebraic equation with two unknowns (u overline, v overline) and an adjustable parameter inline equation associated with $\partial$$\eta^\prime$$\partial$t, assuming that the latter is proportional to ($\partial$$\eta^\prime$$\partial$t -- w). {M}ost interestingly, $\partial$$\eta^\prime$$\partial$t and all other coefficients of the equation can be determined from altimetry. {T}he altimeter data used is combined TOPEX/Poseidon-ERS gridded data, and the solution is obtained by least squares, minimizing the contribution from the time-variable part of the parameter inline equation and prescribing the zonal direction of the mean current. {T}he method, which is found to be particularly useful for quasi-zonal high-energy current systems, has been validated against direct observations in the {G}ulf {S}tream and {S}outhern {O}cean. {C}omparisons with direct observations and {M}onte {C}arlo experiments suggest an overall solution error of about 10 cm s--1. {O}nce calibrated against regional velocity statistics, this method will be able to determine from altimetry the mean or instantaneous surface velocity field down to the frontal scale, with a realism that has been inaccessible because of the geoid constraint.}, 
    25842587language = {{A}nglais}, 
    25852588affiliation = {{L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN}, 
    … …  
    26332636loceanaffectation={cnrs}, 
    26342637title = {{Centennial to millennial-scale variability of the {I}ndian monsoon during the early {H}olocene from a sediment, pollen and isotope record from the desert of {Y}emen}}, 
    2635 author = {{A}nne-{M}arie {L}ézine and J.-{J}. {T}iercelin and C. {R}obert and {J}ean-{F}rançois {S}aliège and S. {C}leuziou and M.-{L}. {I}nizan and F. {B}raemer}, 
    2636 abstract = {{Lacustrine deposits of al-{H}awa (15°52#N, 46°53#E, 710 m above sea level) document the climatic and environmental history of the inland desert of {Y}emen during the early to mid-{H}olocene. A freshwater lake expanded in one of the most arid areas of the world in response to increased {I}ndian monsoon fluxes from 12,000 to 7500 cal B.P. {T}hree dry intervals punctuated the lacustrine phase recording episodes of weaker summer monsoon activity over {A}rabia. {D}ry intervals were coeval with cold periods recorded in the {N}orth {A}tlantic, confirming the links between the {I}ndian monsoon and the {N}orth {A}tlantic systems during the {H}olocene. {W}e demonstrate that the regional vegetation remained of semi-arid character throughout the lacustrine period.}}, 
     2638author = {{A}nne-{M}arie {L}ézine and {J}.-{J}. {T}iercelin and C. {R}obert and {J}ean-{F}rançois {S}aliège and S. {C}leuziou and M.-{L}. {I}nizan and F. {B}raemer}, 
     2639abstract = {{Lacustrine deposits of al-{H}awa (15°52'N, 46°53'E, 710 m above sea level) document the climatic and environmental history of the inland desert of {Y}emen during the early to mid-{H}olocene. A freshwater lake expanded in one of the most arid areas of the world in response to increased {I}ndian monsoon fluxes from 12,000 to 7500 cal B.P. {T}hree dry intervals punctuated the lacustrine phase recording episodes of weaker summer monsoon activity over {A}rabia. {D}ry intervals were coeval with cold periods recorded in the {N}orth {A}tlantic, confirming the links between the {I}ndian monsoon and the {N}orth {A}tlantic systems during the {H}olocene. {W}e demonstrate that the regional vegetation remained of semi-arid character throughout the lacustrine period.}}, 
    26372640keywords = {{P}ollen; {O}xygen isotopes; {C}lay mineralogy; {P}aleolake; {Y}emen; {H}olocene}, 
    26382641language = {{A}nglais}, 
    … …  
    28562859title = {{Rapid paleoenvironmental variations in NE {B}razil during the {L}ateglacial. {I}nsights from {T}pS2, S3CO2 and S3CO {R}ock {E}val parameters}}, 
    28572860  author = {{J}érémy {J}acob and {J}ean-{R}obert {D}isnar and {M}ohammed {B}oussafir {D}idier {K}éravis and {A}bdelfettah {S}ifeddine and {A}na {L}uiza {S}padano {A}lbuquerque and {B}runo {T}urcq}, 
    2858 abstract = {{The {R}ock-{E}val pyrolysis technique was first developed as a rapid mean for evaluating the petroleum potential of source rocks, via the measurement of bulk organic parameters such as {T}otal {O}rganic {C}arbon (TOC), {H}ydrogen {I}ndex (HI), {O}xygen {I}ndex (OI) and the maximum pyrolysis temperature {T}max (Espitalié et al., 1985; {L}afargue et al., 1998). {T}his method was then used to rapidly estimate organic matter quality and quantity in sedimentary series for paleoenvironmental studies (Talbot and {L}ivingston, 1989). {R}ecently, it has been proposed that there could be more information gained from the {R}ock-{E}val parameters (Disnar et al., 2003). {W}hen considering also the recent analytical developments available from the {T}urbo6 version of the apparatus, there is a large field of investigation that remains unexplored in paleoenvironmental studies. {H}ere we present results from the sedimentary infill of {L}agoa do {C}açó (Northern {B}razil) that records paleoenvironmental changes since the {L}ast {G}lacial {M}aximum (Jacob et al., 2004). {T}he present study focuses on the {L}ateglacial interval (ca. 17,000 to 11,000 cal yrs BP), a time period where different {R}ock-{E}val parameters such as {T}pS2 (Tmax equivalent), HI and OI produce controversial information. {I}n order to better understand the meaning of these parameters, we propose an original mean of obtaining more pertinent information. S3CO2/S3CO ratio and {T}pS2 surprisingly display similar trends over the considered period, in two different cores. {F}urthermore, the evolution of these parameters is comparable with that of #18O in the ice core record of {S}ajama (Bolivia) during the {L}ateglacial (Figure 1). {A}lthough the significance of these parameters and the origin of these variations remain to be cleared, our results confirm a pattern of rapid climate variability over the {S}outh {A}merican {T}ropics during the last deglaciation, as seen in the {N}orthern {H}emisphere.}}, 
     2861abstract = {{The {R}ock-{E}val pyrolysis technique was first developed as a rapid mean for evaluating the petroleum potential of source rocks, via the measurement of bulk organic parameters such as {T}otal {O}rganic {C}arbon (TOC), {H}ydrogen {I}ndex (HI), {O}xygen {I}ndex (OI) and the maximum pyrolysis temperature {T}max (Espitalié et al., 1985; {L}afargue et al., 1998). {T}his method was then used to rapidly estimate organic matter quality and quantity in sedimentary series for paleoenvironmental studies (Talbot and {L}ivingston, 1989). {R}ecently, it has been proposed that there could be more information gained from the {R}ock-{E}val parameters (Disnar et al., 2003). {W}hen considering also the recent analytical developments available from the {T}urbo6 version of the apparatus, there is a large field of investigation that remains unexplored in paleoenvironmental studies. {H}ere we present results from the sedimentary infill of {L}agoa do {C}açó (Northern {B}razil) that records paleoenvironmental changes since the {L}ast {G}lacial {M}aximum (Jacob et al., 2004). {T}he present study focuses on the {L}ateglacial interval (ca. 17,000 to 11,000 cal yrs BP), a time period where different {R}ock-{E}val parameters such as {T}pS2 (Tmax equivalent), HI and OI produce controversial information. {I}n order to better understand the meaning of these parameters, we propose an original mean of obtaining more pertinent information. S3CO2/S3CO ratio and {T}pS2 surprisingly display similar trends over the considered period, in two different cores. {F}urthermore, the evolution of these parameters is comparable with that of $\delta^{18}{O}$ in the ice core record of {S}ajama (Bolivia) during the {L}ateglacial (Figure 1). {A}lthough the significance of these parameters and the origin of these variations remain to be cleared, our results confirm a pattern of rapid climate variability over the {S}outh {A}merican {T}ropics during the last deglaciation, as seen in the {N}orthern {H}emisphere.}}, 
    28592862language = {{A}nglais}, 
    28602863affiliation = {{I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {D}epartamento de {G}eoquimica - DEPARTAMENTO DE GEOQUIMICA , {P}aléo-environnements tropicaux et variabilité climatique - PALEOTROPIQUE}, 
    … …  
    28652868audience = {internationale}, 
    28662869year = {2005}, 
     2870pdf={http://hal-insu.archives-ouvertes.fr/docs/00/44/29/40/PDF/7_-_Resume_IMOG_2005_-_Rock_Eval.pdf}, 
    28672871} 
    28682872 
    … …  
    31473151loceanbibid = {01762}, 
    31483152timestamp = {20121107}, 
    3149 Author = {{M}eaghan K. {G}orman and {T}errence M. {Q}uinn and {F}rederick W. {T}aylor and {J}udson W. {P}artin  and {G}uy {C}abioch and {J}ames A. {J}r {A}ustin and {B}ernard {P}elletier and {V}alerie {B}allu and {C}hristophe {M}aes and {S}teffen {S}austrup}, 
     3153Author = {{M}eaghan K. {G}orman and {T}errence M. {Q}uinn and {F}rederick W. {T}aylor and {J}udson W. {P}artin  and {G}uy {C}abioch and {J}ames A. {J}r {A}ustin and {B}ernard {P}elletier and {V}alérie {B}allu and {C}hristophe {M}aes and {S}teffen {S}austrup}, 
    31503154Title = {{A} coral-based reconstruction of sea surface salinity at {S}abine {B}ank, {V}anuatu from 1842 to 2007 CE}, 
    31513155Journal = {PALEOCEANOGRAPHY}, 
    … …  
    33083312  comment = {thèse au CLS, {D}epartement d'océanographie spatiale}, 
    33093313} 
     3314 
    33103315@conference{Thiria:AMS:2012, 
    33113316author={{S}ylvie {T}hiria}, 
    … …  
    35163521hal_id={hal-00752822}, 
    35173522} 
     3523 
    35183524@article{HermandMeyerEtAL:JASA:2006, 
    35193525author = {{J}ean-{P}ierre {H}ermand and {M}atthias {M}eyer and {M}ark {A}sch and {M}ohamed {B}errada}, 
    … …  
    35863592hal_id={hal-00757240}, 
    35873593} 
     3594 
    35883595@article{ZocatelliTurcEtAl:PPP:2012, 
    35893596hal_id = {insu-00730933}, 
    … …  
    36593666} 
    36603667 
    3661 } 
    36623668@article{CaterinoTishechkinEtAl:Z:2012a, 
    36633669author = {{M}ichael {C}aterino and {A}lexey {T}ishechkin and {N}icolas {D}égallier}, 
    … …  
    37683774note={documentaire {A}rte}, 
    37693775} 
     3776 
    37703777@misc{Testor:T:2009, 
    37713778author = {{P}ierre {T}estor}, 
    … …  
    39433950timestamp = {20120706}, 
    39443951} 
     3952 
    39453953@conference{Levy:HD:2009, 
    39463954author = {{M}arina {L}évy}, 
    … …  
    39713979timestamp = {20120706}, 
    39723980} 
     3981 
    39733982@conference{Levy:CAOS:2009, 
    39743983author = {{M}arina {L}évy}, 
    … …  
    39984007timestamp = {20120706}, 
    39994008} 
     4009 
    40004010@conference{Levy:SWOT:2008, 
    40014011author = {{M}arina {L}évy}, 
    … …  
    41304140timestamp = {20120706}, 
    41314141} 
     4142 
    41324143@conference{Testor::2008b, 
    41334144author={{P}ierre {T}estor}, 
    … …  
    41434154timestamp = {20120706}, 
    41444155} 
     4156 
    41454157@conference{Testor::2010, 
    41464158author={{P}ierre {T}estor}, 
    … …  
    41854197timestamp = {20120706}, 
    41864198} 
     4199 
    41874200@conference{Testor:FOF:2010, 
    41884201author={{P}ierre {T}estor}, 
    … …  
    41984211timestamp = {20120706}, 
    41994212} 
     4213 
    42004214@conference{Testor::2011, 
    42014215author={{P}ierre {T}estor}, 
    … …  
    42114225timestamp = {20120706}, 
    42124226} 
     4227 
    42134228@conference{Testor:MARES:2011, 
    42144229author={{P}ierre {T}estor}, 
    … …  
    42254240timestamp = {20120706}, 
    42264241} 
     4242 
    42274243@conference{Testor:CDMSS:2011, 
    42284244author={{P}ierre {T}estor}, 
    … …  
    42534269timestamp = {20120706}, 
    42544270} 
     4271 
    42554272@conference{Mortier:N:2010, 
    42564273author={{L}aurent {M}ortier}, 
    … …  
    42674284timestamp = {20120706}, 
    42684285} 
     4286 
    42694287@conference{Mortier:FCO:2011, 
    42704288author={{L}aurent {M}ortier}, 
    … …  
    43594377timestamp={20120706}, 
    43604378} 
     4379 
    43614380@Conference{Arnault:A:2010, 
    43624381author = {{S}abine {A}rnault}, 
    … …  
    43974416timestamp={20120706}, 
    43984417} 
     4418 
    43994419@Conference{ArnaultTanguyEtAl:TAM:2009, 
    44004420author = {{S}abine {A}rnault and {Y}ves {T}anguy and {Ph}ilippe {L}attes}, 
    … …  
    44874507  timestamp={20120706}, 
    44884508} 
     4509 
    44894510@CONFERENCE{HenocqBoutinEtAl:IGARSS:2007, 
    44904511author = {{C}laire {H}énocq and {J}acqueline {B}outin and {F}. {P}etitcolin and {S}abine {A}rnault}, 
    … …  
    55255546 
    55265547@article{LavaysseVracEtAl:NHESS:2012, 
    5527   author = {{C}. {L}avaysse and {M}. {V}rac and {Ph}ilipe {D}robinski and {M}atthieu {L}engaigne and {T}. {V}ischel}, 
     5548  author = {{C}. {L}avaysse and {M}. {V}rac and {Ph}ilippe {D}robinski and {M}atthieu {L}engaigne and {T}. {V}ischel}, 
    55285549  title = {{S}tatistical downscaling of {F}rench {M}editerranean climate : assessment for present and projection in an anthropogenic scenario}, 
    55295550  year = {2012}, 
    … …  
    58085829 
    58095830@UNPUBLISHED{MerlivatBoutin::2012inprep, 
    5810   author = {{L}iliane {M}erlivat and {J}acqueline {B}outin and {D}. {A}ntoine}, 
     5831  author = {{L}iliane {M}erlivat and {J}acqueline {B}outin and {D}avid {A}ntoine}, 
    58115832  title = {{R}emote estimates of marine primary productivity in the {S}outhern {O}cean from {C}arioca drifters and satellite based observations}, 
    58125833  year = {2012}, 
    … …  
    65156536 
    65166537@ARTICLE{AlvarezTanhuaEtAl:JGR:2011, 
    6517   author = {{M}. {A}lvarez and {M}. and {T}. {T}anhua and {H}. {B}rix and {C}laire {{L}o {M}onaco} and {N}icolas {M}etzl and {E}. {M}cDonagh and {H}. {B}ryden}, 
     6538  author = {{M}. {A}lvarez and {T}. {T}anhua and {H}. {B}rix and {C}laire {{L}o {M}onaco} and {N}icolas {M}etzl and {E}. {M}cDonagh and {H}. {B}ryden}, 
    65186539  title = {{D}ecadal biogeochemical changes in the {S}ubtropical {I}ndian {O}cean associated with {S}ubantarctic {M}ode {W}ater}, 
    65196540  journal = {{J}ournal of {G}eophysical {R}esearch}, 
    … …  
    71347155 
    71357156@ARTICLE{BouzidKhannousEtAl:IJG:2012, 
    7136   author = {{S}aida {B}ouzid and {S}oumaya {K}hannous and {I}oanna {B}ouloubassi and {A}lain {S}aliot and {H}assan {E}r {R}aioui}, 
     7157  author = {{S}aïda {B}ouzid and {S}oumaya {K}hannous and {I}oanna {B}ouloubassi and {A}lain {S}aliot and {H}assan {E}r {R}aioui}, 
    71377158  title = {{A}ssessment of the {M}oroccan {M}editerranean {C}oasts {C}ontamination by {H}ydrocarbons (Non {A}romatic {H}ydrocarbons, {A}romatic {H}ydrocarbons and {A}lkylbenzenes)}, 
    71387159  journal = {{I}nternational {J}ournal of {G}eosciences}, 
    … …  
    75807601        {P}acific {O}cean. {K}ey differences in their thermohaline vertical 
    75817602        structure were revealed. {T}he core of cyclonic eddies (CEs) is centered 
    7582         at &#8764;150 m depth within the 25.2-26.0 kg m&#8722;3 potential 
     7603        at ~150 m depth within the 25.2-26.0 kg m$^{-3}$ potential 
    75837604        density layer corresponding to the thermocline. {I}n contrast, the 
    75847605        core of the anticyclonic eddies (AEs) is located below the thermocline 
    7585         at &#8764;400 m depth impacting the 26.0-26.8 kg m&#8722;3 density 
     7606        at ~400 m depth impacting the 26.0-26.8 kg m$^{-3}$ density 
    75867607        layer. {T}his difference was attributed to the mechanisms involved 
    75877608        in the eddy formation. {W}hile intrathermocline CEs would be formed 
    … …  
    75957616        only the fraction of the water column associated with the fluid trapped 
    75967617        within the eddies, each CE and AE has a typical volume anomaly flux 
    7597         of &#8764;0.1 {S}v and yields to a heat and salt transport anomaly 
    7598         of ±1-3 × 1011 W and ±3-8 × 103 kg s&#8722;1, respectively.}, 
     7618        of ~0.1 {Sv} and yields to a heat and salt transport anomaly 
     7619        of ±1-3 × 1011 W and ±3-8 × 103 kg s$^{-1}$, respectively.}, 
    75997620  aeresteam = {phybiocar}, 
    76007621  aerestype = {ACL}, 
    … …  
    1057510596 
    1057610597@CONFERENCE{MerlivatBoutinetAl:WCRP:2011, 
    10577   author = {{L}iliane {M}erlivat and {J}acqueline {B}outin and {D}. {A}ntoine}, 
     10598  author = {{L}iliane {M}erlivat and {J}acqueline {B}outin and {D}avid {A}ntoine}, 
    1057810599  title = {{R}emote estimates of marine primary productivity in the southern ocean from {CARIOCA} drifters and satellite based observations}, 
    1057910600  booktitle = {WCRP}, 
    … …  
    1152911550        and thus refuting the assumption that birds will ultimately adapt 
    1153011551        to being banded. {I}ndeed, banded birds still arrived later for breeding 
    11531         at the study site and had longer foraging trips even after 10#years. 
     11552        at the study site and had longer foraging trips even after 10 years. 
    1153211553        {O}ne of our major findings is that responses of flipper-banded penguins 
    1153311554        to climate variability (that is, changes in sea surface temperature 
    … …  
    1177511796        of the WSR induced a strong perturbation in the deep flow field during 
    1177611797        the southward journey. {T}he height of the SFZ crests clearly sets 
    11777         the lower limit of the SPDW in the {O}na {B}asin. {A}n enhanced $\delta$3He 
     11798        the lower limit of the SPDW in the {O}na {B}asin. {A}n enhanced $\delta^{3}$He 
    1177811799        signature is confined to the north of the {P}olar {F}ront between 
    1177911800        55.5°S and 56.5°S in the 1500-2200 m depth range. {I}t 
    … …  
    1502315044        mode waters ventilation in the {I}ndian sector are identified with 
    1502415045        different circulation pathways and source water masses: (a) just 
    15025         north of {K}erguelen, where 4.2 {S}v of lighter {S}ubantarctic {M}ode 
     15046        north of {K}erguelen, where 4.2 {Sv} of lighter {S}ubantarctic {M}ode 
    1502615047        {W}aters ({SAMW}); $sigma$026.5) are exported-originating in the 
    1502715048        {A}tlantic and {A}gulhas {R}etroflection regions; (b) {SW} of {A}ustralia, 
    15028         where 6.5 {S}v of medium {SAMW} ($sigma$026.6) are ventilated-originating 
     15049        where 6.5 {Sv} of medium {SAMW} ($sigma$026.6) are ventilated-originating 
    1502915050        in the southern and denser {A}gulhas {R}etroflection region; (c) 
    1503015051        {SW} of {T}asmania and along the {S}outh {A}ustralian coast, where 
    15031         3 {S}v of denser {SAMW} ($sigma$026.75) are ventilated-originating 
     15052        3 {Sv} of denser {SAMW} ($sigma$026.75) are ventilated-originating 
    1503215053        from three sources: {L}eeuwin {C}urrent waters, {T}asman {S}ea ({P}acific) 
    1503315054        waters and {A}ntarctic {S}urface {W}aters. {I}n all cases, modelled 
    … …  
    1850818529 
    1850918530@ARTICLE{ErraiouiBouzidEtAl:OCM:2009, 
    18510   author = {{H}assan {E}r-{R}aioui and {S}aida {B}ouzid and {M}ohammed {M}arhraoui and {A}lain {S}aliot}, 
     18531  author = {{H}assan {E}r-{R}aioui and {S}aïda {B}ouzid and {M}ohammed {M}arhraoui and {A}lain {S}aliot}, 
    1851118532  title = {{H}ydrocarbon pollution of the {M}editerranean coastline of {M}orocco}, 
    1851218533  journal = {{O}cean \& {C}oastal {M}anagement}, 
    … …  
    1982019841 
    1982119842@INPROCEEDINGS{LucioDegallierEtAl:SC:2010, 
    19822   author = {{PS}. Lúcio and {N}icolas {D}égallier and MSS. {C}oelho and FD. da {S}ilva and MHC. {S}pyrides and LF. {A}raújo and CPC {M}acêdo and {C}hristophe {E}. {M}enkès and {M}atthieu {L}engaigne and {R}.Souza and EB {B}esserra ans LP {C}avalti and RAF {A}raujo}, 
     19843  author = {{PS}. Lúcio and {N}icolas {D}égallier and MSS. {C}oelho and FD. da {S}ilva and MHC. {S}pyrides and LF. {A}raújo and CPC {M}acêdo and {C}hristophe {E}. {M}enkès and {M}atthieu {L}engaigne and {R}.Souza and EB {B}esserra and LP {C}avalti and RAF {A}raujo}, 
    1982319844  title = {{U}so de previsões climáticas em um modelo de risco de transmissão de doenças vetoriais clima-dependentes. O caso do dengue no NEB}, 
    1982419845  booktitle = {{S}egunda {C}onferência {I}nternacional sobre {C}lima, {S}ustentabilidade e 
    … …  
    2041420435        ({ACC}) crossing the {K}erguelen {P}lateau were directly observed 
    2041520436        during the 2009 {T}rack cruise. {T}he net eastward transport to the 
    20416         south of the {H}eard/Mc{D}onald {I}slands is estimated as 56 {S}v 
    20417         (1 {S}v = 106 m3 s-1), 43 {S}v of which is tightly channelled into 
     20437        south of the {H}eard/Mc{D}onald {I}slands is estimated as 56 {Sv} 
     20438        (1 {Sv} = $10^{6} m^{3} s^{-1}), 43 {Sv} of which is tightly channelled into 
    2041820439        the {F}awn {T}rough that appears as a predominant cross-plateau gateway 
    2041920440        of circumpolar flow associated with the {S}outhern {ACC} {F}ront 
    20420         ({SACCF}). {T}here are also two secondary passages, with one (6 {S}v) 
     20441        ({SACCF}). {T}here are also two secondary passages, with one (6 {Sv}) 
    2042120442        being attached to the nearshore slope just south of the {H}eard/Mc{D}onald 
    20422         {I}slands and the other (7 {S}v) passing through the northern {P}rincess 
    20423         {E}lizabeth {T}rough. {W}ith an additional 2 {S}v inferred just south 
     20443        {I}slands and the other (7 {Sv}) passing through the northern {P}rincess 
     20444        {E}lizabeth {T}rough. {W}ith an additional 2 {Sv} inferred just south 
    2042420445        of the {K}erguelen {I}slands, the transport across the entire plateau 
    20425         amounts to 58 {S}v, accounting for ~40% of the total {ACC} transport 
    20426         transiting through the region, 147-152 {S}v, quantities consistent 
     20446        amounts to 58 {Sv}, accounting for ~40% of the total {ACC} transport 
     20447        transiting through the region, 147-152 {Sv}, quantities consistent 
    2042720448        with other independent estimates in the {I}ndian sector of the {S}outhern 
    2042820449        {O}cean.}, 
    … …  
    2147821499        meridional overturning response at multidecadal time scales to freshwater 
    2147921500        flux perturbation: for typical amplitudes of {G}reat {S}alinity {A}nomalies, 
    21480         initial perturbations can alter the circulation by +2.25 {S}v (1 
    21481         {S}v # 106 m3 s-1; i.e., 12.5% of the mean circulation) at most; 
     21501        initial perturbations can alter the circulation by +2.25 {Sv} (1 
     21502        {Sv} = $10^{6} m^{3} s^{-1}$; i.e., 12.5% of the mean circulation) at most; 
    2148221503        stochastic perturbations with amplitudes typical of the interannual 
    2148321504        variability of the freshwater flux in midlatitudes induce a circulation 
    21484         variability with a standard deviation of 1 {S}v (i.e., 5.5% of the 
     21505        variability with a standard deviation of 1 {Sv} (i.e., 5.5% of the 
    2148521506        mean circulation) at most.}, 
    2148621507  aerestype = {ACL}, 
    … …  
    2406724088  ads={2008JCli...21.5603I}, 
    2406824089  hal_id={hal-00770003}, 
    24069   comment =  {20130104 : pb nom/prénom cdbm dans base ads}, 
     24090  comment = {20130104 : pb nom/prénom cdbm dans base ads}, 
    2407024091} 
    2407124092 
    … …  
    2434224363@ARTICLE{LazarethLietardEtAl:GRA:2008, 
    2434324364  author = {{C}laire {E}. {L}azareth and {C}écile {L}ietard and {C}atherine {P}ierre and {L}uc {O}rtlieb}, 
    24344   title = {{I}nter-individual and inter-site reproducibility of $\delta ^{18}{O}$ profiles across {P}rotothaca thaca (Bivalvia, {V}eneridae) shells from {P}eru and {C}hile}, 
     24365  title = {{I}nter-individual and inter-site reproducibility of $\delta^{18}{O}$ profiles across {P}rotothaca thaca (Bivalvia, {V}eneridae) shells from {P}eru and {C}hile}, 
    2434524366  journal = {{G}eophysical {R}esearch {A}bstracts}, 
    2434624367  year = {2008}, 
    … …  
    2453424555@ARTICLE{LietardPierre:JGL:2008, 
    2453524556  author = {{C}écile {L}ietard and {C}atherine {P}ierre}, 
    24536   title = {{H}igh-resolution isotopic records ($\delta^{18}{O}$ and $\delta ^{13}{C}$) and cathodoluminescence study of lucinid shells from methane seeps of the {E}astern {M}editerranean}, 
     24557  title = {{H}igh-resolution isotopic records ($\delta^{18}{O}$ and $\delta^{13}{C}$) and cathodoluminescence study of lucinid shells from methane seeps of the {E}astern {M}editerranean}, 
    2453724558  journal = {{G}eo-{M}arine {L}etters}, 
    2453824559  year = {2008}, 
    … …  
    2606826089  audience = {non spécifiée}, 
    2606926090  doi = {10.1002/qj.185}, 
    26070   keywords = {{ERA}-40 # {NCEP}2 # {AMMA} # {AERONET} # radiosondes}, 
     26091  keywords = {{ERA}-40; {NCEP}2 ;{AMMA} ; {AERONET} ; radiosondes}, 
    2607126092  language = {{A}nglais}, 
    2607226093  loceanaffectation = {ird}, 
    … …  
    2726927290        of leaf waxes indicate an arid to semi-arid climate with a long lasting 
    2727027291        dry season. {A}n abrupt change towards much wetter conditions occurred 
    27271         within ca. 500 years from 17.3 to 16.8 ka, as shown by a 50 # decrease 
     27292        within ca. 500 years from 17.3 to 16.8 ka, as shown by a 50 \textperthousand decrease 
    2727227293        in {D}/{H} ratios and a marked increase in {H} isotopic fractionation 
    2727327294        of leaf waxes. {T}his abrupt isotopic change coincides with a major 
    … …  
    2783027851 
    2783127852@ARTICLE{LacombeGarconEtAl:MC:2007, 
    27832   author = {{M}arielle {L}acombe and {V}éronique {G}arçon and {M}aurice {C}omtat and {L}ouise {O}riol and {J}oël {S}udre and {D}anièle {T}houron and {N}adine {L}e {B}ris and {C}hristine {P}rovost}, 
     27853  author = {{M}arielle {L}acombe and {V}éronique {G}arçon and {M}aurice {C}omtat and {L}ouise {O}riol and {J}oël {S}udre and {D}anièle {T}houron and {N}adine {{L}e {B}ris} and {C}hristine {P}rovost}, 
    2783327854  title = {{Silicate determination in sea water : toward a reagentless electrochemical method}}, 
    2783427855  journal = {{M}arine {C}hemistry}, 
    … …  
    2901729038  volume = {37}, 
    2901829039  pages = {484-500}, 
    29019   abstract = {{W}e investigated the distributions and $\delta ^{13}{C}$ values of 
     29040  abstract = {{W}e investigated the distributions and $\delta^{13}{C}$ values of 
    2902029041        lipid biomarkers in authigenic methane-related carbonate crusts formed 
    2902129042        on eastern {M}editerranean mud volcanoes. {A}highly diverse suite 
    … …  
    2981829839        chronology development, sediment structure, elemental, organic, and 
    2981929840        mineralogical compositions of a box core collected at 300m depth 
    29820         off {P}isco, central {P}eru. {A}n average sedimentation rate of 2.2mmy\&\#8722;1 
    29821         was estimated from downcore excess 210Pb activities for the last 
     29841        off {P}isco, central {P}eru. {A}n average sedimentation rate of 2.2mm$y^{-1}$ 
     29842        was estimated from downcore excess $^{210}Pb$ activities for the last 
    2982229843        100-150 years. {E}xtending this rate further downcore indicates that 
    2982329844        a slump located at 52 cm depth from the top of the core can be correlated 
    … …  
    2986929890  timestamp = {20120419}, 
    2987029891  hal_id={hal-00084924}, 
     29892   pdf={http://hal-insu.archives-ouvertes.fr/docs/00/08/49/24/PDF/adgeo-6-119.pdf}, 
    2987129893} 
    2987229894 
    … …  
    3106231084  timestamp = {20120419}, 
    3106331085  hal_id={hal-00331140}, 
    31064   comment =  {20121115 : doublon hal-00331122 pas exactement ni le même titre ni le même journal}, 
     31086  comment = {20121115 : doublon hal-00331122 pas exactement ni le même titre ni le même journal}, 
    3106531087} 
    3106631088 
    … …  
    3267932701 
    3268032702@INPROCEEDINGS{MerlivatCaniauxEtAl:OD:2005, 
    32681   author = {{L}iliane {M}erlivat and {G}uy {C}aniaux and {L}eticia {B}arbero-{M}unoz}, 
     32703  author = {{L}iliane {M}erlivat and {G}uy {C}aniaux and {L}eticia {B}arbero-{M}uñoz}, 
    3268232704  title = {{D}iurnal variations of air-sea flux of {CO$_{2}$}, ocean {CO$_{2}$} partial pressure, {SST} and mixed layer depth along drifter trajectories in the {N}ortheastern {A}tlantic}, 
    3268332705  booktitle = {37th {L}iège {C}olloquium on {O}cean {D}ynamics: {G}as {T}ransfer 
    … …  
    3509435116  timestamp = {20120419}, 
    3509535117  hal_id = {hal-00153947}, 
    35096 comment = {20121115 : mauvais ordre auteurs dans hal hal-00153947  {L}aurent {M}ortier <mortier@locean-ipsl.upmc.fr>}, 
     35118comment = {20121115 : mauvais ordre auteurs dans hal hal-00153947 {L}aurent {M}ortier <mortier@locean-ipsl.upmc.fr>}, 
    3509735119} 
    3509835120 
    … …  
    3788137903  timestamp = {20120419}, 
    3788237904  url = {http://www.documentation.ird.fr/hor/fdi:010016639}, 
    37883   hal_id =  {hal-00153959} 
     37905  hal_id = {hal-00153959} 
    3788437906} 
    3788537907 
    … …  
    3855438576  school = {{U}niversité de {P}aris {VI}}, 
    3855538577  year = {1990}, 
     38578  date= {1990-05-02}, 
    3855638579  type = {{T}hèse de doctorat}, 
    38557   note = {2 mai 1990}, 
    3855838580  loceanbibid = {00023}, 
    3855938581  pages = {175}, 
    … …  
    3856238584 
    3856338585@ARTICLE{MolinariOlsonEtAl:JGR:1990, 
    38564   author = {{R}obert {L}.  {M}olinari and {D}onald {O}lson and {G}illes {R}everdin}, 
     38586  author = {{R}obert {L}. {M}olinari and {D}onald {O}lson and {G}illes {R}everdin}, 
    3856538587  title = {{S}urface current distributions in the tropical {I}ndian {O}cean derived from compilations of surface buoys trajectories}, 
    3856638588  journal = {{J}ournal of {G}eophysical {R}esearch}, 

  • branches/bibliolocean/src/biblio_biber_biblatex.tex

    r307 r309  
    2727\usepackage[frenchb]{babel} 
    2828\usepackage[latin1]{inputenc} 
     29\usepackage[T1]{fontenc} 
    2930\usepackage{csquotes} 
     31% uncomment following line for debug style 
     32%\usepackage[backend=biber,style=debug]{biblatex} 
    3033\usepackage[backend=biber]{biblatex} 
     34% ok reading \usepackage[backend=biber,style=reading]{biblatex} 
    3135\bibliography{ginette} 
    3236\begin{document} 
    3337% force to include all entry of the bibliography ++ 
     38%++ 1998 pas ok \nocite{*} 
    3439\nocite{*} 
    3540%++ ok \autocite{LebloisQuirionEtAl:EP:2013} 
     41 
     42%11 \autocite[cf AA][CC]{ArchambeauPierreEtAl:JMS:1998} 
     43 
     44%22 \autocite[cf BB][DD]{BartheletBonyEtAl:CRASPEaPS:1998} 
     45 
    3646\printbibliography 
    3747 

  • branches/bibliolocean/src/biblio_split.sh

    r117 r309  
    6262# Once splitted each entry can be an input of biblio processing. 
    6363# 
    64 # for example, here is how to produce an RTF file from each splitted reference:: 
     64# For example, here is how to produce an RTF file from each splitted reference:: 
    6565#  
    6666#  $ for file in /tmp/locean_biblio_split/b????_*.bib 
    … …  
    7878#   $ rm /tmp/fplod/gtbiblio/b????_*.rtf 
    7979# 
    80 # 
     80# You can also run pdflatex+biber from each splitted reference:: 
     81# 
     82#  $ for filebib in /tmp/locean_biblio_split/b????_*.bib 
     83#  do 
     84#    filetex=/tmp/locean_biblio_split/$(basename ${filebib} .bib).tex 
     85#    echo $filetex 
     86#    read a 
     87#    sed -e "s@ginette@${filebib}@" biblio_biber_biblatex.tex > ${filetex}  
     88#    pdflatex -output-directory /tmp/locean_biblio_split/ ${filetex} 
     89#    biber /tmp/locean_biblio_split/$(basename ${filetex} .tex).bcf 
     90#    pdflatex -output-directory /tmp/locean_biblio_split/ ${filetex} 
     91#    pdflatex -output-directory /tmp/locean_biblio_split/ ${filetex} 
     92#  done 
     93#   
    8194# TODO 
    8295# ==== 

  • branches/bibliolocean/src/genbib.sh

    r307 r309  
    2020# pb avec l'apostrophe dans les noms d'auteurs avec bibtool 
    2121# 
     22# pb biber avec nom (last name) composé entouré de {} 
     23#   solution sans doute = passer en nom, prénom (pas à la main !!!) 
     24# 
     25# pb biber pour manger toutes les références 
     26# 
    2227# find missing hal/tel reference with bibtool 
    2328# 
    … …  
    2530# 
    2631# good looking of \delta on jabref outputs 
    27 # 
    28 # 180 et 13C sideupper 
    29 # 
    30 # check for all chemical and physical expressions 
    3132# 
    3233# ++ doublons 
    … …  
    524525   # 
    525526   # remove temporary latex files 
     527ls ${dirwww}/${biblioref}.${style}* 
    526528   rm ${dirwww}/$(basename ${biblioref}.${style}.bbl) ${dirwww}/$(basename ${biblioref}.${style}.blg) ${dirwww}/$(basename ${biblioref}.${style}.log) ${dirwww}/$(basename ${biblioref}.${style}.aux) 2> /dev/null 
    527529   # 
    … …  
    541543else 
    542544   style=biber 
     545   option_pdflatex=-interaction=nonstopmode 
    543546   # processing bibliography with pdflatex (${dirwww}/${biblioref}.${style}.pdf) 
    544547   rm ${dirwww}/$(basename ${biblioref}.${style}.log .log).* 2> /dev/null 
    545548   sed -e "s@ginette@${biblioref}@" biblio_biber_biblatex.tex > ${biblioref}.${style}.tex 
    546    pdflatex -output-directory ${dirwww} ${biblioref}.${style}.tex 
    547    biber ${dirwww}/$(basename ${biblioref}.${style}) 
     549 
     550   # only 2012 (memory exceed with everything 
     551   iyear=2012 
     552   iyear=1996 
     553   iyear=1998 
     554   bibtool_command="bibtool -- 'select={year \"${iyear}\"}' ${biblioref} -o ${tmpdir}/tmp1.bib" 
     555   eval ${bibtool_command} 
     556   sed -e "s@ginette@${tmpdir}/tmp1.bib@" biblio_biber_biblatex.tex > ${biblioref}.${style}.tex 
     557   # 
     558   pdflatex ${option_pdflatex} -output-directory ${dirwww} ${biblioref}.${style}.tex 
     559   biber ${dirwww}/$(basename ${biblioref}.${style}).bcf 
    548560   #++ warnings 
    549    pdflatex -output-directory ${dirwww} ${biblioref}.${style}.tex 
    550    pdflatex -output-directory ${dirwww} ${biblioref}.${style}.tex 
     561   pdflatex ${option_pdflatex} -output-directory ${dirwww} ${biblioref}.${style}.tex 
     562   pdflatex ${option_pdflatex} -output-directory ${dirwww} ${biblioref}.${style}.tex 
    551563   # 
    552564   # remove temporary latex files 
    553    #++rm ${dirwww}/$(basename ${biblioref}.${style}.bbl) ${dirwww}/$(basename ${biblioref}.${style}.blg) ${dirwww}/$(basename ${biblioref}.${style}.log) ${dirwww}/$(basename ${biblioref}.${style}.aux) ${dirwww}/$(basename ${biblioref}.${style}.bcf) ${dirwww}/$(basename ${biblioref}.${style}.run.xml) 2> /dev/null 
     565   rm ${dirwww}/$(basename ${biblioref}.${style}.bbl) ${dirwww}/$(basename ${biblioref}.${style}.blg) ${dirwww}/$(basename ${biblioref}.${style}.log) ${dirwww}/$(basename ${biblioref}.${style}.aux) ${dirwww}/$(basename ${biblioref}.${style}.bcf) ${dirwww}/$(basename ${biblioref}.${style}.run.xml) 2> /dev/null 
    554566   echo "cf. ${biblioref}.${style}.tex and ${dirwww}/*biber*" #++ 
    555567   # 
    556    #++rm ${biblioref}.${style}.tex 2> /dev/null 
     568   rm ${biblioref}.${style}.tex 2> /dev/null 
    557569fi 
    558570unset tool 
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