Changeset 303 for branches

Timestamp:

02/04/13 16:00:41 (11 years ago)

Author:

pinsard

Message:

update from NM; fixes

File:

• branches/bibliolocean/data/biblioref.bib (modified) (13 diffs)

branches/bibliolocean/data/biblioref.bib

@@ -3 +3 @@
 
 @PREAMBLE{"Bibliographie du LOCEAN"}
+
+@article{SchusterMckinleyEtAl:B:2013,
+hal_id = {hal-00784593},
+loceanbibid = {01934},
+loceanteam= {phybiocar,caraus/snapo-co2},
+loceanaffectation={cnrs},
+timestamp = {20130204},
+title = {{An assessment of the Atlantic and Arctic sea-air {CO$_{2}$} fluxes, 1990-2009}},
+author = {U. Schuster and G. A. Mckinley and N. Bates and F. Chevallier and S. C. Doney and A. R. Fay and M. González-Dávila and N. Gruber and S. Jones and J. Krijnen and P. Landschützer and {N}athalie {L}efèvre and M. Manizza and J. Mathis and {N}icolas {M}etzl and A. Olsen and A. F. Rios and C. Rödenbeck and J. M. Santana-Casiano and T. Takahashi and R. Wanninkhof and A. J. Watson},
+abstract = {{The Atlantic and Arctic Oceans are critical components of the global carbon cycle. Here we quantify the net sea-air {CO$_{2}$} flux, for the first time, across different methodologies for consistent time and space scales for the Atlantic and Arctic basins. We present the long-term mean, seasonal cycle, interannual variability and trends in sea-air {CO$_{2}$} flux for the period 1990 to 2009, and assign an uncertainty to each. We use regional cuts from global observations and modeling products, specifically a p{CO$_{2}$}-based {CO$_{2}$} flux climatology, flux estimates from the inversion of oceanic and atmospheric data, and results from six ocean biogeochemical models. Additionally, we use basin-wide flux estimates from surface ocean p{CO$_{2}$} observations based on two distinct methodologies. Our estimate of the contemporary sea-air flux of {CO$_{2}$} (sum of anthropogenic and natural components) by the Atlantic between 40\degre S and 79\degre N is -0.49 $\pm$ 0.05 Pg C yr-1, and by the Arctic it is -0.12 $\pm$ 0.06 Pg C yr-1, leading to a combined sea-air flux of -0.61 $\pm$ 0.06 Pg C yr-1 for the two decades (negative reflects ocean uptake). We do find broad agreement amongst methodologies with respect to the seasonal cycle in the subtropics of both hemispheres, but not elsewhere. Agreement with respect to detailed signals of interannual variability is poor, and correlations to the North Atlantic Oscillation are weaker in the North Atlantic and Arctic than in the equatorial region and southern subtropics. Linear trends for 1995 to 2009 indicate increased uptake and generally correspond between methodologies in the North Atlantic, but there is disagreement amongst methodologies in the equatorial region and southern subtropics.}},
+language = {Anglais},
+affiliation = {Woods Hole Oceanographic Institution - WHOI , Centre for Ecology and Hydrology - CEH , Institut Pierre-Simon-Laplace - IPSL , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Instituto de Investigaciones Marinas , Max-Planck-Institut f{\"u}r Biogeochemie},
+pages = {607-627},
+journal = {Biogeosciences},
+volume = {10},
+audience = {internationale},
+doi = {10.5194/BG-10-607-2013},
+year = {2013},
+month = jan,
+}
+
+@article{RodenbeckKeelingEtAl:OSD:2012,
+hal_id = {hal-00784582},
+loceanbibid = {01933},
+loceanteam= {phybiocar,caraus/snapo-co2},
+loceanaffectation={cnrs},
+timestamp = {20130204},
+title = {{Sea-air {CO$_{2}$} flux estimated from SOCAT surface-ocean {CO$_{2}$} partial pressure data and atmospheric {CO$_{2}$} mixing ratio data}},
+author = {C. Rödenbeck and R. F. Keeling and D. C. E. Bakker and {N}icolas {M}etzl and A. Olsen and C. Sabine and M. Heimann},
+abstract = {{Surface-ocean {CO$_{2}$} partial pressure data have been assimilated into a simple diagnostic model of surface-ocean biogeochemistry to estimate the spatio-temporal {CO$_{2}$} partial pressure field and ultimately the sea-air {CO$_{2}$} fluxes. Results compare well with the widely used monthly climatology by Takahashi et al. (2009) but also contain some short-term and interannual variations. Fitting the same model to atmospheric {CO$_{2}$} data yields less robust but consistent estimates, confirming that using the partial pressure based estimates as ocean prior in atmospheric {CO$_{2}$} inversions may improve land {CO$_{2}$} flux estimates. Estimated seasonality of ocean-internal carbon sources and sinks is discussed in the light of observed nutrient variations.}},
+language = {Anglais},
+affiliation = {Max-Planck-Institut f{\"u}r Biogeochemie , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Max Planck institute for Biogeochemistry},
+pages = {2273-2326},
+journal = {Ocean Science Discussions},
+volume = {9},
+audience = {internationale},
+doi = {10.5194/OSD-9-2273-2012},
+year = {2012},
+month = jun,
+ads={2012OcScD...9.2273R},
+}
+
+@article{LentonTilbrookEtAl:BD:2013,
+loceanbibid = {01932},
+loceanteam= {phybiocar,caraus/snapo-co2},
+loceanaffectation={cnrs},
+timestamp = {20130204},
+hal_id = {hal-00784292},
+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},
+title={Sea-air {CO$_{2}$} fluxes in the Southern Ocean for the period 1990-2009},
+ads={2013BGD....10..285L},
+year={2013},
+pages = {285-333},
+journal = {Biogeosciences Discussions},
+volume = {10},
+audience = {internationale},
+doi = {10.5194/BGD-10-285-2013},
+month = jan,
+}
+
+@article{KellerJoosEtAl:T:2012,
+loceanbibid = {01931},
+loceanaffectation = {cnrs},
+loceanteam = {phybiocar,caraus/snapo-co2},
+timestamp = {20130204},
+author={Kathrin M. Keller and Fortunat Joos and Christoph C. Raible and Valentina Cocco and Thomas L. Frölicher and John P. Dunne and Marion Gehlen and Laurent Bopp and James C. Orr and Jerry Tjiputra and Christoph Heinze and Joachim Segschneider and {T}illa {R}oy and {N}icolas {M}etzl},
+year={2012},
+title={Variability of the Ocean Carbon Cycle in Response to the North Atlantic Oscillation},
+journal={Tellus B},
+volume={64},
+pages={18738},
+doi={10.3402/tellusb.v64i0.18738},
+}
 
 @article{SaracenoProvost:DSR:2012,
@@ -340 +413 @@
 timestamp = {20121123},
 hal_id = {hal-00756523},
-title = {{Surface Ocean CO2 Atlas (SOCAT) gridded data products}},
+title = {{Surface Ocean {CO$_{2}$} Atlas (SOCAT) gridded data products}},
 author = {C. L. Sabine and S. Hankin and H. Koyuk and D. C. E. Bakker and B. Pfeil and A. Olsen and {N}icolas {M}etzl and A. Kozyr and A. Fassbender and A. Manke and J. Malczyk and J. Akl and S. R. Alin and R. G. J. Bellerby and A. Borges and {J}acqueline {B}outin  and P. J. Brown and W.-J. Cai and F. P. Chavez and A. Chen and C. Cosca and R. A. Feely and M. González-Dávila and C. Goyet and N. Hardman-Mountford and C. Heinze and M. Hoppema and C. W. Hunt and D. Hydes and M. Ishii and T. Johannessen and R. M. Key and A. Körtzinger and P. Landschützer and S. K. Lauvset and {N}athalie {L}efèvre  and Andrew Lenton and {A}nna {L}ourantou  and {L}iliane {M}erlivat  and T. Midorikawa and L. Mintrop and C. Miyazaki and A. Murata and A. Nakadate and Y. Nakano and S. Nakaoka and Y. Nojiri and A. M. Omar and X. A. Padin and G.-H. Park and K. Paterson and F. F. Perez and D. Pierrot and A. Poisson and A. F. Ríos and J. Salisbury and J. M. Santana-Casiano and V. V. S. S. Sarma and R. Schlitzer and B. Schneider and U. Schuster and R. Sieger and I. Skjelvan and T. Steinhoff and T. Suzuki and T. Takahashi and K. Tedesco and M. Telszewski and H. Thomas and B. Tilbrook and D. Vandemark and T. Veness and A. J. Watson and R. Weiss and C. S. Wong and H. Yoshikawa-Inoue
 },
@@ -346 +419 @@
 affiliation = {Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN},
 pages = {781-804},
-journal = {10.5194/essdd--5--781--2012},
+journal = {Earth System Science Data Discussions},
+doi = {10.5194/essdd--5--781--2012},
 volume = {5},
 audience = {internationale},
@@ -358 +432 @@
 timestamp = {20121123},
 hal_id = {hal-00756509},
-title = {{A uniform, quality controlled Surface Ocean CO2 Atlas (SOCAT)}},
+title = {{A uniform, quality controlled Surface Ocean {CO$_{2}$} Atlas (SOCAT)}},
 author = {B. Pfeil and A. Olsen and D. C. E. Bakker and S. Hankin and H. Koyuk and A. Kozyr and J. Malczyk and A. Manke and {N}icolas {M}etzl and C. L. Sabine and J. Akl and S. R. Alin and R. G. J. Bellerby and A. Borges and {J}acqueline {B}outin and P. J. Brown and W.-J. Cai and F. P. Chavez and A. Chen and C. Cosca and A. J. Fassbender and R. A. Feely and M. González-Dávila and C. Goyet and N. Hardman-Mountford and C. Heinze and M. Hood and M. Hoppema and C. W. Hunt and D. Hydes and M. Ishii and T. Johannessen and S. D. Jones and R. M. Key and A. Körtzinger and P. Landschützer and S. K. Lauvset and {N}athalie {L}efèvre and A. Lenton and {A}nna {L}ourantou and {L}iliane {M}erlivat and T. Midorikawa and L. Mintrop and C. Miyazaki and A. Murata and A. Nakadate and Y. Nakano and S. Nakaoka and Y. Nojiri and A. M. Omar and X. A. Padin and G.-H. Park and K. Paterson and F. F. Perez and D. Pierrot and A. Poisson and A. F. Ríos and J. M. Santana-Casiano and J. Salisbury and V. V. S. S. Sarma and R. Schlitzer and B. Schneider and U. Schuster and R. Sieger and I. Skjelvan and T. Steinhoff and T. Suzuki and T. Takahashi and K. Tedesco and M. Telszewski and H. Thomas and B. Tilbrook and J. Tjiputra and D. Vandemark and T. Veness and R. Wanninkhof and A. J. Watson and R. Weiss and C. S. Wong and H. Yoshikawa-Inoue},
 language = {Anglais},
@@ -840 +914 @@
 loceanbibid = {01884},
 timestamp={20121115},
-title = {{Interannual-to-decadal variability of {N}orth {A}tlantic air-sea CO2 fluxes}},
+title = {{Interannual-to-decadal variability of {N}orth {A}tlantic air-sea {CO$_{2}$} fluxes}},
 author = {{S}. {R}aynaud and {O}livier {A}umont and K. B. {R}odgers and P. {Y}iou and J. C. {O}rr},
-abstract = {{The magnitude of the interannual variability of {N}orth {A}tlantic air-sea CO2 fluxes remains uncertain. {F}luxes inferred from atmospheric inversions have large variability, whereas those simulated by ocean models have small variability. {P}art of the difference is that unlike typical atmospheric inversions, ocean models come with spatial resolution at the sub-basin scale. {H}ere we explore sub-basin-scale spatiotemporal variability in the {N}orth {A}tlantic in one ocean model in order to better understand why the the {N}orth {A}tlantic basin may well contribute very little to the global variability of air-sea CO2 flux. {W}e made two simulations with a biogeochemical model coupled to a global ocean general circulation model (OGCM), which itself was forced by 55-year NCEP reanalysis fields. {I}n the first simulation, atmospheric CO2 was maintained at the preindustrial level (278 ppmv); in the second simulation, atmospheric CO2 followed the observed increase. {S}imulated air-sea CO2 fluxes and associated variables were analysed with a statistical tool known as multichannel singular spectrum analysis (MSSA). {W}e found that the subtropical gyre is not the largest contributor to the overall, basin-wide variability, in contrast to previous suggestions. {T}he subpolar gyre and the inter-gyre region (the transition area between subpolar and subtropical gyres) also contribute with multipolar anomalies at multiple frequencies: these tend to cancel one another in terms of the basin-wide air-sea CO2 flux. {W}e found a strong correlation between the air-sea CO2 fluxes and the {N}orth {A}tlantic {O}scillation (NAO), but only if one takes into account time lags as does MSSA (maximum r=0.64 for lags between 1 and 3 years). {T}he contribution of anthropogenic CO2 to total variability was negligible at interannual time scales, whereas at the decadal (13-year) time scale, it increased variability by 30\%.}},
+abstract = {{The magnitude of the interannual variability of {N}orth {A}tlantic air-sea {CO$_{2}$} fluxes remains uncertain. {F}luxes inferred from atmospheric inversions have large variability, whereas those simulated by ocean models have small variability. {P}art of the difference is that unlike typical atmospheric inversions, ocean models come with spatial resolution at the sub-basin scale. {H}ere we explore sub-basin-scale spatiotemporal variability in the {N}orth {A}tlantic in one ocean model in order to better understand why the the {N}orth {A}tlantic basin may well contribute very little to the global variability of air-sea {CO$_{2}$} flux. {W}e made two simulations with a biogeochemical model coupled to a global ocean general circulation model (OGCM), which itself was forced by 55-year NCEP reanalysis fields. {I}n the first simulation, atmospheric {CO$_{2}$} was maintained at the preindustrial level (278 ppmv); in the second simulation, atmospheric {CO$_{2}$} followed the observed increase. {S}imulated air-sea {CO$_{2}$} fluxes and associated variables were analysed with a statistical tool known as multichannel singular spectrum analysis (MSSA). {W}e found that the subtropical gyre is not the largest contributor to the overall, basin-wide variability, in contrast to previous suggestions. {T}he subpolar gyre and the inter-gyre region (the transition area between subpolar and subtropical gyres) also contribute with multipolar anomalies at multiple frequencies: these tend to cancel one another in terms of the basin-wide air-sea {CO$_{2}$} flux. {W}e found a strong correlation between the air-sea {CO$_{2}$} fluxes and the {N}orth {A}tlantic {O}scillation (NAO), but only if one takes into account time lags as does MSSA (maximum r=0.64 for lags between 1 and 3 years). {T}he contribution of anthropogenic {CO$_{2}$} to total variability was negligible at interannual time scales, whereas at the decadal (13-year) time scale, it increased variability by 30\%.}},
 language = {{A}nglais},
 affiliation = {{L}aboratoire des sciences du climat et de l'environnement - LSCE , {L}aboratoire d'océanographie dynamique et de climatologie - LODYC},
@@ -907 +981 @@
 loceanbibid = {01880},
 timestamp={20121115},
-title = {{Mesoscale variability of sea surface pCO2: {W}hat does it respond to?}},
+title = {{Mesoscale variability of sea surface p{CO$_{2}$}: {W}hat does it respond to?}},
 author = {{A}. {M}ahadevan and {M}arina {L}évy and {L}aurent {M}émery},
 language = {{A}nglais},
@@ -925 +999 @@
 title = {{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}},
 author = {{A}nne-{S}ophie {A}rchambeau and {C}atherine {P}ierre and {A}lain {P}oisson and {B}ernard {S}chauer},
-abstract = {{This study presents oceanic distributions of stable isotopes ($\delta$18O of water and $\delta$13C of $\Sigma$CO2) 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 CO2 derived from remineralization of organic matter. {A}long the {A}ntarctic continental shelf, between 2500 and 4000 m, a core of water with $\delta$18O values close to --0.1 is associated with a relative maximum in CFC-12 concentration, although this core is not detected by its temperature and salinity parameters. {T}his water mass, which corresponds to recently formed deep water, may originate from the eastward extension of the {W}eddell gyre or from bottom waters coming from the {E}ast and formed near {P}rydz {B}ay.}},
+abstract = {{This study presents oceanic distributions of stable isotopes ($\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$18O values close to --0.1 is associated with a relative maximum in CFC-12 concentration, although this core is not detected by its temperature and salinity parameters. {T}his water mass, which corresponds to recently formed deep water, may originate from the eastward extension of the {W}eddell gyre or from bottom waters coming from the {E}ast and formed near {P}rydz {B}ay.}},
 keywords = {{S}table isotopes; 18O; 13C; CFC-12; {A}ustral {O}cean},
 language = {{A}nglais},
@@ -1051 +1125 @@
 title = {{Ocean biogeochemistry exhibits contrasting responses to a large scale reduction in dust deposition}},
 author = {{A}. {T}agliabue and {L}aurent {B}opp and {O}livier {A}umont},
-abstract = {{Dust deposition of iron is thought to be an important control on ocean biogeochemistry and air-sea CO2 exchange. {I}n this study, we examine the impact of a large scale, yet climatically realistic, reduction in the aeolian {F}e input during a 240 year transient simulation. {I}n contrast to previous studies, we find that the ocean biogeochemical cycles of carbon and nitrogen are relatively insensitive (globally) to a 60\% reduction in {F}e input from dust. {N}et primary productivity (NPP) is reduced in the {F}e limited regions, but the excess macronutrients that result are able to fuel additional NPP elsewhere. {O}verall, NPP and air-sea CO2 exchange are only reduced by around 3\% between 1860 and 2100. {W}hile the nitrogen cycle is perturbed more significantly (by \~15\%), reduced N2 fixation is balanced by a concomitant decline in denitrification. {F}eedbacks between N2 fixation and denitrification are controlled by variability in surface utilization of inorganic nitrogen and subsurface oxygen consumption, as well as the direct influence of {F}e on N2 fixation. {O}verall, there is relatively little impact of reduced aeolian {F}e input (}},
+abstract = {{Dust deposition of iron is thought to be an important control on ocean biogeochemistry and air-sea {CO$_{2}$} exchange. {I}n this study, we examine the impact of a large scale, yet climatically realistic, reduction in the aeolian {F}e input during a 240 year transient simulation. {I}n contrast to previous studies, we find that the ocean biogeochemical cycles of carbon and nitrogen are relatively insensitive (globally) to a 60\% reduction in {F}e input from dust. {N}et primary productivity (NPP) is reduced in the {F}e limited regions, but the excess macronutrients that result are able to fuel additional NPP elsewhere. {O}verall, NPP and air-sea {CO$_{2}$} exchange are only reduced by around 3\% between 1860 and 2100. {W}hile the nitrogen cycle is perturbed more significantly (by \~15\%), reduced N2 fixation is balanced by a concomitant decline in denitrification. {F}eedbacks between N2 fixation and denitrification are controlled by variability in surface utilization of inorganic nitrogen and subsurface oxygen consumption, as well as the direct influence of {F}e on N2 fixation. {O}verall, there is relatively little impact of reduced aeolian {F}e input (}},
 language = {{A}nglais},
 affiliation = {{L}aboratoire des sciences du climat et de l'environnement - LSCE , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN},
@@ -2648 +2722 @@
 loceanbibid = {01779},
 timestamp = {20121107},
-title = {{Rapid paleoenvironmental variations in NE {B}razil during the {L}ateglacial. {I}nsights from {T}pS2, S3CO2 and S3CO {R}ock {E}val parameters.}},
+title = {{Rapid paleoenvironmental variations in NE {B}razil during the {L}ateglacial. {I}nsights from {T}pS2, S3CO2 and S3CO {R}ock {E}val parameters}},
   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},
 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.}},
@@ -2683 +2757 @@
 loceanbibid = {01777},
 timestamp = {20121107},
-title = {{Evidence of a shift in the cyclicity of {A}ntarctic seabird dynamics linked to climate.}},
+title = {{Evidence of a shift in the cyclicity of {A}ntarctic seabird dynamics linked to climate}},
 author = {{S}téphanie {J}enouvrier and {H}enri {W}eimerskirch and {C}hristophe {B}arbraud and {Y}oung-{H}yang {P}ark and {B}ernard {C}azelles},
 abstract = {{Ecosystems and populations are known to be influenced not only by long-term climatic trends, but also by other short-term climatic modes, such as interannual and decadal-scale variabilities. {B}ecause interactions between climatic forcing, biotic and abiotic components of ecosystems are subtle and complex, analysis of long-term series of both biological and physical factors is essential to understanding these interactions. {H}ere, we apply a wavelet analysis simultaneously to long-term datasets on the environment and on the populations and breeding success of three {A}ntarctic seabirds (southern fulmar, snow petrel, emperor penguin) breeding in {T}erre {A}délie, to study the effects of climate fluctuations on {A}ntarctic marine ecosystems. {W}e show that over the past 40 years, populations and demographic parameters of the three species fluctuate with a periodicity of 3-5 years that was also detected in sea-ice extent and the {S}outhern {O}scillation {I}ndex. {A}lthough the major periodicity of these interannual fluctuations is not common to different species and environmental variables, their cyclic characteristics reveal a significant change since 1980. {M}oreover, sliding-correlation analysis highlighted the relationships between environmental variables and the demography of the three species, with important change of correlation occurring between the end of the 1970s and the beginning of the 1980s. {T}hese results suggest that a regime shift has probably occurred during this period, significantly affecting the {A}ntarctic ecosystem, but with contrasted effects on the three species.}},
@@ -3390 +3464 @@
 author = {{R}enata {Z}ocatelli and {B}runo {T}urcq and {M}ohammed {B}oussafir and {R}.C. {C}ordeiro and {J}ean-{R}obert {D}isnar and {R}.L. {C}osta and {A}bdelfettah {S}ifeddine and {A}na {L}uiza {S}padano {A}lbuquerque and {M}.C. {B}ernardes and {J}érémy {J}acob},
 abstract = {{N}ortheast {B}razil represents a key area in terms of {H}olocene environmental changes in {S}outh {A}merica due to its distinct semi-arid climate at near equatorial latitudes as well as to a wetter {E}arly and {M}iddle {H}olocene paleoclimate in comparison with other {S}outh {A}merica regions, which also experienced a reduced monsoon at that time. {W}e studied the lacustrine sediments of {L}ake {B}oqueirão, which is located at 5°S latitude on the {B}razilian {A}tlantic coast; it is directly influenced by displacement of the {I}ntertropical {C}onvergence {Z}one (ITCZ). A short (1 m) core "Boqc0701" was collected at a 7.5 m water depth during a seismic survey. {O}rganic matter (OM) geochemical [Rock {E}val {T}otal {O}rganic {C}arbon (TOC), {H}ydrogen {I}ndex (HI), {O}xygen {I}ndex (OI)] and petrographical studies allowed us to distinguish five sedimentary intervals during the last 3 kyrs. {P}hase E (3000 to 2050 cal yr BP) presents the largest TOC, HI and OI fluctuations in the entire core. {T}he most probable cause of these variations is a great instability in the lake level during this period. {P}hase D (2050 to 1830 cal yr BP) is marked by an increase in sedimentation rate and a higher contribution from a well-preserved OM with an algal origin; this was interpreted as a higher and more stable lake level. {D}uring phase C (1830 to 1550 cal yrs BP), low HI and high OI indicate the input of more oxidized, degraded and detrital OM, reflecting a lower lake level. {I}n phase B (1550 to 1470 cal yr BP), the OM quality and quantity (HI and TOC) indicate an algal contribution. {D}uring phase A (1470 to 570 cal yr BP), the high stability of the proxies may be due to a deep environment where OM fluctuations are strongly buffered. {T}hese changes in lake level can be compared with other tropical {S}outh {A}merica high resolution records. A correspondence seems to exist between phases of low ENSO, cool {N}orth {A}tlantic {O}cean and {B}oqueirão wet phases. {W}e did not encounter this same pattern during the last 1050 yaers, during which the 1050-570 cal yrs BP interval was generally wet (although probable fluctuations are buffered in our proxies) while the {N}orth {A}tlantic was warm (Mann et al., 2009). A prolonged dryness occurred in {L}ake {B}oqueirão from 570 cal yrs BP until recent decades. {T}his phase corresponds to the {L}ittle {I}ce {A}ge characterized by a cooler {N}orth {A}tlantic {O}cean (Mann et al., 2009). {T}hese data indicate that the teleconnection pattern between the tropical {A}tlantic, ENSO and {N}ortheast {B}razil rainfalls has changed in the past.},
-keywords = {{R}ock-{E}val, organic petrography, macrophytes, algal, intertropical convergence.},
+keywords = {{R}ock-{E}val, organic petrography, macrophytes, algal, intertropical convergence},
 language = {{A}nglais},
 affiliation = {{I}nstitut des {S}ciences de la {T}erre d'{O}rléans - ISTO , LMI "PALEOTRACES" , {L}aboratoire d'{O}céanographie et du {C}limat : {E}xpérimentations et {A}pproches {N}umériques - LOCEAN , {D}epartamento de {G}eoquìmica , {D}epartamento de {G}eoquimica - DEPARTAMENTO DE GEOQUIMICA},
@@ -3477 +3551 @@
   year = {2011},
   address = {{A}capulco, {G}uerrero, {M}exico},
-  note = {{L}a {O}rganización {M}exicana de {M}eteorólogos, {A}.C.},
+  note = {{L}a {O}rganización {M}exicana de {M}eteorólogos, {A}.{C}.},
   date = {14 al 18 de noviembre del 2011},
   loceanaffectation = {ird},
@@ -10865 +10939 @@
 }
 
-@UNPUBLISHED{RacapePierreEtAl:JMS:2011submitted,
-  author = {{V}irginie {R}acapé and {C}atherine {P}ierre and {N}icolas {M}etzl and {C}laire {{L}o {M}onaco} and {G}illes {R}everdin and {A}. {O}lsen and {P}. {M}orin and {M}. {V}asquez-{R}odriguez and {A}. {R}ios and {F}. {P}erez},
+@UNPUBLISHED{RacapePierreEtAl:JMS:2012online,
+  author = {{V}irginie {R}acapé and {C}atherine {P}ierre and {N}icolas {M}etzl and {C}laire {{L}o {M}onaco} and {G}illes {R}everdin and {A}. {O}lsen and {P}. {M}orin and {M}. {V}asquez-{R}odriguez and {A}. {F}. {R}ios and {F}. {P}erez},
   title = {{A}nthropogenic carbon changes in the {I}rminger {B}asin (1981-2006): coupling $\delta^{13}{C}_{DIC}$ and {DIC} observations},
-  year = {2011},
+  year = {2012},
   aeresteam = {phybiocar, paleoproxus,caraus/snapo-co2},
   aerestype = {ACL},
-  format = {submitted},
+  format = {on line},
+  doi={10.1016/j.jmarsys.2012.12.005},
   journal = {{J}ournal of {M}arine {S}ystems},
   loceanaffectation = {cnrs},