Changeset 253
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- 09/27/12 12:59:57 (12 years ago)
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branches/bibliolocean/data/biblioref.bib
r252 r253 4 4 @PREAMBLE{"Bibliographie du LOCEAN"} 5 5 6 @article{MoreiraMoreiraTurcqEtAl:JP:2012, 7 author = {{L}. {S}. {M}oreira and {P}. {F}. {M}oreira-{T}urcq and {B}runo {T}urcq and {S}andrine {C}aquineau}, 8 Title = {Paleohydrological changes in an Amazonian floodplain lake: Santa Ninha Lake}, 9 journal = {{J}ournal of {P}aleolimnology}, 10 Year = {2012}, 11 Volume = {48}, 12 Number = {2}, 13 Pages = {339-350}, 14 Month = aug, 15 DOI = {10.1007/s10933-012-9601-x}, 16 Keywords = {Paleohydrology; Organic matter; Paleoenvironment; Amazon Basin; Floodplain lakes}, 17 loceanbibid = {01736}, 18 loceanaffectation = {cnrs}, 19 loceanteam = {paleoproxus}, 20 timestamp = {20120927}, 21 } 22 23 @article{CremierePierreEtAl:DSR:2012, 24 author = {{A}ntoine {C}remière and {C}atherine {P}ierre and {M}arie-{M}adeleine {B}lanc-{V}alleron {T}. {Z}itter and {N}. {C}agatay and {P}. {H}enry}, 25 Title = {Methane-derived authigenic carbonates along the North Anatolian fault system in the Sea of Marmara (Turkey)}, 26 journal = {{D}eep {S}ea {R}esearch {P}art {I}: {O}ceanographic {R}esearch {P}apers}, 27 Year = {2012}, 28 Volume = {66}, 29 Pages = {114-130}, 30 doi = {10.1016/j.dsr.2012.03.014}, 31 loceanbibid = {01735}, 32 loceanaffectation = {cnrs}, 33 loceanteam = {paleoproxus}, 34 timestamp = {20120927}, 35 } 36 37 @article{CaiLengaigneEtAl:N:2012, 38 author = {Wenju Cai and {M}atthieu {L}engaigne and Simon Borlace and Matthew Collins and Tim Cowan and Michael J. McPhaden and Axel Timmermann and Scott Power and Josephine Brown and {C}hristophe {E}. {M}enkès and Arona Ngari and Emmanuel M. Vincent and Matthew J. Widlansky}, 39 day = {16}, 40 doi = {10.1038/nature11358}, 41 journal = {Nature}, 42 month = aug, 43 number = {7411}, 44 pages = {365-369}, 45 publisher = {Nature Publishing Group, a division of Macmillan Publishers Limited. All Rights Reserved.}, 46 title = {More extreme swings of the South Pacific convergence zone due to greenhouse warming}, 47 volume = {488}, 48 year = {2012}, 49 loceanbibid = {01734}, 50 loceanaffectation = {ird}, 51 loceanteam = {varclim, phybiocar}, 52 timestamp = {20120927}, 53 } 6 54 @article{ZocatelliTurcEtAl:PPP:2012, 7 55 hal_id = {insu-00730933}, 8 56 url = {http://hal-insu.archives-ouvertes.fr/insu-00730933}, 9 title = { {Late Holocene paleoenvironmental changes in Northeast Brazil recorded by organic matter in lacustrine sediments of Lake Boqueir{\\~a}o}},57 title = {Late Holocene paleoenvironmental changes in Northeast Brazil recorded by organic matter in lacustrine sediments of Lake Boqueir{\\~a}o}, 10 58 loceanbibid = {01733}, 11 59 loceanaffectation = {ird}, … … 14 62 timestamp = {20120912}, 15 63 author = {Renata Zocatelli and {B}runo {T}urcq and Mohammed Boussafir and R.C. Cordeiro and Jean-Robert Disnar and R.L. Costa and {A}bdelfettah {S}ifeddine and Ana Luiza Spadano Albuquerque and M.C. Bernardes and and Jérémy Jacob}, 16 abstract = { {Northeast Brazil represents a key area in terms of Holocene environmental changes in South America due to its distinct semi-arid climate at near equatorial latitudes as well as to a wetter Early and Middle Holocene paleoclimate in comparison with other South America regions, which also experienced a reduced monsoon at that time. We studied the lacustrine sediments of Lake Boqueir{\\~a}o, which is located at 5\degreS latitude on the Brazilian Atlantic coast; it is directly influenced by displacement of the Intertropical Convergence Zone (ITCZ). A short (1 m) core "Boqc0701" was collected at a 7.5 m water depth during a seismic survey. Organic matter (OM) geochemical [Rock Eval Total Organic Carbon (TOC), Hydrogen Index (HI), Oxygen Index (OI)] and petrographical studies allowed us to distinguish five sedimentary intervals during the last 3 kyrs. Phase E (3000 to 2050 cal yr BP) presents the largest TOC, HI and OI fluctuations in the entire core. The most probable cause of these variations is a great instability in the lake level during this period. Phase 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. During 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. In phase B (1550 to 1470 cal yr BP), the OM quality and quantity (HI and TOC) indicate an algal contribution. During 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. These changes in lake level can be compared with other tropical South America high resolution records. A correspondence seems to exist between phases of low ENSO, cool North Atlantic Ocean and Boqueir{\\~a}o wet phases. We 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 North Atlantic was warm (Mann et al., 2009). A prolonged dryness occurred in Lake Boqueir{\\~a}o from 570 cal yrs BP until recent decades. This phase corresponds to the Little Ice Age characterized by a cooler North Atlantic Ocean (Mann et al., 2009). These data indicate that the teleconnection pattern between the tropical Atlantic, ENSO and Northeast Brazil rainfalls has changed in the past.}},64 abstract = {Northeast Brazil represents a key area in terms of Holocene environmental changes in South America due to its distinct semi-arid climate at near equatorial latitudes as well as to a wetter Early and Middle Holocene paleoclimate in comparison with other South America regions, which also experienced a reduced monsoon at that time. We studied the lacustrine sediments of Lake Boqueir{\\~a}o, which is located at 5\degreS latitude on the Brazilian Atlantic coast; it is directly influenced by displacement of the Intertropical Convergence Zone (ITCZ). A short (1 m) core "Boqc0701" was collected at a 7.5 m water depth during a seismic survey. Organic matter (OM) geochemical [Rock Eval Total Organic Carbon (TOC), Hydrogen Index (HI), Oxygen Index (OI)] and petrographical studies allowed us to distinguish five sedimentary intervals during the last 3 kyrs. Phase E (3000 to 2050 cal yr BP) presents the largest TOC, HI and OI fluctuations in the entire core. The most probable cause of these variations is a great instability in the lake level during this period. Phase 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. During 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. In phase B (1550 to 1470 cal yr BP), the OM quality and quantity (HI and TOC) indicate an algal contribution. During 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. These changes in lake level can be compared with other tropical South America high resolution records. A correspondence seems to exist between phases of low ENSO, cool North Atlantic Ocean and Boqueir{\\~a}o wet phases. We 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 North Atlantic was warm (Mann et al., 2009). A prolonged dryness occurred in Lake Boqueir{\\~a}o from 570 cal yrs BP until recent decades. This phase corresponds to the Little Ice Age characterized by a cooler North Atlantic Ocean (Mann et al., 2009). These data indicate that the teleconnection pattern between the tropical Atlantic, ENSO and Northeast Brazil rainfalls has changed in the past.}, 17 65 keywords = {Rock-Eval, organic petrography, macrophytes, algal, intertropical convergence.}, 18 66 language = {Anglais}, … … 30 78 @inproceedings{MeynadierDecoetlogon:hal-00723384, 31 79 url = {http://hal.archives-ouvertes.fr/hal-00723384}, 32 title = { {Impact of the air-sea coupling in the Gulf of Guinea on the Guinean coastal water cycle in boreal spring}},80 title = {Impact of the air-sea coupling in the Gulf of Guinea on the Guinean coastal water cycle in boreal spring}, 33 81 author = {{R}émi {M}eynadier and {G}aëlle {{d}e {C}oëtlogon} and {L}aurence {E}ymard {M}arion {L}educ-{L}eballeur and {S}ophie {B}astin and {S}erge {J}anicot and Olivier Bock and Cyrille Flamant}, 34 82 language = {Anglais}, 35 83 affiliation = {Institut Pierre-Simon-Laplace - IPSL , Laboratoire Atmosph{\`e}res, Milieux, Observations Spatiales - LATMOS , Universit{\'e} Paris 6, Pierre et Marie Curie - UPMC , Laboratoire d'Oc{\'e}anographie et du Climat : Exp{\'e}rimentations et Approches Num{\'e}riques - LOCEAN , Laboratoire de Recherche en G{\'e}od{\'e}sie, IGN - LAREG}, 36 booktitle = { {4th {AMMA} International Conference}},84 booktitle = {4th {AMMA} International Conference}, 37 85 address = {Toulouse, France}, 38 86 year = {2012}, … … 63 111 64 112 @article{DegallierMazurEtAl:Z:2012b, 65 66 67 68 69 70 71 72 73 74 113 author = {{N}icolas {D}égallier and Slawomir Mazur and Alexey K. Tishechkin and Michael S. Caterino}, 114 journal = {ZooKeys}, 115 publisher = {Pensoft Publishers}, 116 title = {A revision of the genus Kaszabister Mazur (Histeridae, Histerinae, Exosternini)}, 117 year = {2012}, 118 month = {06}, 119 volume = {199}, 120 url = {http://dx.doi.org/10.3897/zookeys.199.3245}, 121 pages = {71--89}, 122 doi = {10.3897/zookeys.199.3245}, 75 123 loceanaffectation = {ird}, 76 124 loceanbibid = {01730}, … … 1345 1393 est locean dans l'historire ++}, 1346 1394 doi = {10.3354/meps09498}, 1347 keywords = {{A}rea-restricted search * {D}ive classification * {D}rift dive * 1348 {F}ine-scale behaviour * {M}ovement analysis}, 1395 keywords = {{A}rea-restricted search * {D}ive classification * {D}rift dive * {F}ine-scale behaviour * {M}ovement analysis}, 1349 1396 language = {{A}nglais}, 1350 1397 loceanbibid = {01602}, … … 2025 2072 } 2026 2073 2027 @UNPUBLISHED{LevyFerrariEtAl:GRL: inpress,2028 author = {{M}arina {L}évy and {R} . {F}errari and {P}. {F}ranks and {A}. {M}artin and {P}.{R}ivière},2074 @UNPUBLISHED{LevyFerrariEtAl:GRL:2012, 2075 author = {{M}arina {L}évy and {R}affaele {F}errari and {P}eter J. S. {F}ranks and {A}drian P. {M}artin and {P}ascal {R}ivière}, 2029 2076 title = {{B}ringing physics to life at the submesoscale}, 2030 2077 year = {2012}, … … 2032 2079 aerestype = {ACL}, 2033 2080 doi = {10.1029/2012GL052756}, 2034 format = {in press},2035 2081 journal = {{G}eophysical {R}esearch {L}etters}, 2036 2082 loceanaffectation = {cnrs}, 2037 2083 loceanbibid = {01508}, 2038 2084 loceanteam = {phybiocar}, 2085 volume={39}, 2086 pages={L14602}, 2039 2087 timestamp = {20120419} 2040 2088 } 2041 2089 2042 2090 @ARTICLE{LevyIovinoEtAl:OM:2012, 2043 author = {{M}arina {L}évy and {D} .{I}ovino and {L}aure {R}esplandy and {P}atrice {K}lein and {G}urvan {M}adec and {A}nne-{M}arie {T}réguier and {S}ébastien {M}asson and {K}. {T}akahashi},2091 author = {{M}arina {L}évy and {D}oroteaciro {I}ovino and {L}aure {R}esplandy and {P}atrice {K}lein and {G}urvan {M}adec and {A}nne-{M}arie {T}réguier and {S}ébastien {M}asson and {K}. {T}akahashi}, 2044 2092 title = {{L}arge-scale impacts of submesoscale dynamics on phytoplankton : local and remote effects}, 2045 2093 journal = {{O}cean {M}odelling}, … … 6723 6771 } 6724 6772 6725 @UNPUBLISHED{MassonTerrayEtAl:CD:201 1online,6773 @UNPUBLISHED{MassonTerrayEtAl:CD:2012, 6726 6774 author = {{S}ébastien {M}asson and {P}ascal {T}erray and {G}urvan {M}adec and {J}ing-{J}ia {L}uo and {T}oshio {Y}amagata and {K}eiko {T}akahashi}, 6727 6775 title = {{I}mpact of intra-daily {SST} variability on {ENSO} characteristics in a coupled model}, 6728 note = {on line}, 6729 year = {2011}, 6776 year = {2012}, 6730 6777 aeresteam = {varclim,nemo}, 6731 6778 aerestype = {ACL}, 6732 6779 doi = {10.1007/s00382-011-1247-2}, 6733 format = {on line}, 6780 Volume={39}, 6781 number={3-4}, 6782 pages={681-707}, 6734 6783 issn = {0930-7575}, 6735 6784 journal = {{C}limate {D}ynamics}, … … 6959 7008 } 6960 7009 6961 @UNPUBLISHED{MoriokaTozukaEtAl:JC:2012 inpress,7010 @UNPUBLISHED{MoriokaTozukaEtAl:JC:2012, 6962 7011 author = {{Y}. {M}orioka and {T}. {T}ozuka and {S}ébastien {M}asson and {P}ascal {T}erray and {J}ing-{J}ia {L}uo and {T}. {Y}amagata}, 6963 7012 title = {{S}ubtropical dipole modes simulated in a coupled general circulation model}, … … 6965 7014 aeresteam = {varclim}, 6966 7015 aerestype = {ACL}, 6967 format = {in press},6968 7016 journal = {{J}ournal of {C}limate}, 7017 volume={25}, 7018 number={12}, 7019 pages={4029-4047}, 6969 7020 doi={10.1175/JCLI-D-11-00396.1}, 6970 7021 loceanaffectation = {ird,uvsq}, … … 8160 8211 } 8161 8212 8162 @UNPUBLISHED{TerrayKakithaEtAl:CD:201 1online,8213 @UNPUBLISHED{TerrayKakithaEtAl:CD:2012, 8163 8214 author = {{P}ascal {T}erray and {K}amala {K}akitha and {S}ébastien {M}asson and {G}urvan {M}adec and {A}. {K}. {S}ahai and {J}ing-{J}ia {L}uo and {T}oshio {Y}amagata}, 8164 8215 title = {{T}he role of the intra-daily {SST} variability in the {I}ndian monsoon variability and monsoon-{ENSO}-{IOD} relationships in a global coupled model}, 8165 note = {on line}, 8166 year = {2011}, 8216 year = {2012}, 8217 Volume={39}, 8218 number={3-4}, 8219 Pages={729-754}, 8167 8220 aeresteam = {varclim}, 8168 8221 aerestype = {ACL}, 8169 8222 doi = {10.1007/s00382-011-1240-9}, 8170 format = {on line},8171 8223 issn = {0930-7575}, 8172 8224 journal = {{C}limate {D}ynamics}, … … 11610 11662 11611 11663 @ARTICLE{LevyKleinEtAl:OM:2010, 11612 author = {{M}arina {L}évy and {P}atrice {K}lein and {A}nne-{M}arie {T}réguier and {D} .{I}ovino and {G}urvan {M}adec and {S}ébastien {M}asson and {K}eiko {T}akahashi},11664 author = {{M}arina {L}évy and {P}atrice {K}lein and {A}nne-{M}arie {T}réguier and {D}oroteaciro {I}ovino and {G}urvan {M}adec and {S}ébastien {M}asson and {K}eiko {T}akahashi}, 11613 11665 title = {{M}odifications of gyre circulation by sub-mesoscale physics}, 11614 11666 journal = {{O}cean {M}odelling},
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