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晚更新世阿蒙森海生产力和冰筏输入的变化对表层海洋环境和西南极冰盖演化的指示

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张静渊, 肖文申, 王汝建, 樊加恩, 王含章, 杨如意. 晚更新世阿蒙森海生产力和冰筏输入的变化对表层海洋环境和西南极冰盖演化的指示[J]. 海洋地质与第四纪地质, 2023, 43(2): 136-144. doi: 10.16562/j.cnki.0256-1492.2023020802
引用本文: 张静渊, 肖文申, 王汝建, 樊加恩, 王含章, 杨如意. 晚更新世阿蒙森海生产力和冰筏输入的变化对表层海洋环境和西南极冰盖演化的指示[J]. 海洋地质与第四纪地质, 2023, 43(2): 136-144. doi: 10.16562/j.cnki.0256-1492.2023020802
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ZHANG Jingyuan, XIAO Wenshen, WANG Rujian, FAN Jiaen, WANG Hanzhang, YANG Ruyi. Changes in productivity and ice-rafting input in the Amundsen Sea during the Late Pleistocene: Implications on the evolution of surface-ocean environment and the West Antarctic Ice Sheet[J]. Marine Geology & Quaternary Geology, 2023, 43(2): 136-144. doi: 10.16562/j.cnki.0256-1492.2023020802
Citation: ZHANG Jingyuan, XIAO Wenshen, WANG Rujian, FAN Jiaen, WANG Hanzhang, YANG Ruyi. Changes in productivity and ice-rafting input in the Amundsen Sea during the Late Pleistocene: Implications on the evolution of surface-ocean environment and the West Antarctic Ice Sheet[J]. Marine Geology & Quaternary Geology, 2023, 43(2): 136-144. doi: 10.16562/j.cnki.0256-1492.2023020802
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晚更新世阿蒙森海生产力和冰筏输入的变化对表层海洋环境和西南极冰盖演化的指示

  • 同济大学海洋地质国家重点实验室，上海 200092

  • 基金项目: 国家自然科学基金“第四纪冰期旋回中南大洋中深层水向中低纬太平洋的入侵及其气候效应”（42030401）；自然资源部国家海洋局极地考察办专项“南极重点海域对气候变化的响应和影响”子课题（01-03-02D）
详细信息
    作者简介: 张静渊（2000—），男，硕士研究生，专业方向为海洋地质学与古环境研究，E-mail：2231674@tongji.edu.cn
    通讯作者: 肖文申（1982—），男，博士，副教授，从事古海洋与古气候研究，E-mail：wxiao@tongji.edu.cn

  • 中图分类号: P736.2

Changes in productivity and ice-rafting input in the Amundsen Sea during the Late Pleistocene: Implications on the evolution of surface-ocean environment and the West Antarctic Ice Sheet

  • State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China

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    摘要

  • 阿蒙森海是当前全球变暖背景下西南极冰盖消融的核心区域。本文分析了中国第34次南极考察采集自阿蒙森海的ANT34-A5-7岩芯中生产力和冰筏碎屑含量等指标，旨在重建研究区深海氧同位素MIS 6期以来表层海洋环境和西南极冰盖演化历史。研究结果显示，阿蒙森海生产力呈现间冰期高、冰期低的特征。在末次间冰期（MIS 5.5）具有比当前更高的生产力水平，同时伴随着西南极冰盖的严重消融。这个现象归因于MIS 5.5更暖的海表温度、更少的海冰覆盖，以及向南入侵的绕极深层水的上涌。该研究结果可对预测未来气候变化提供必要的理论依据。

    The Amundsen Sea is the core area of the melting West Antarctic Ice Sheet (WAIS) in the recent global warming process. Productivity proxies and ice rafted debris (IRD) contents in core ANT34-A5-7 collected from the Amundsen Sea during the 34th Chinese Antarctic Research Expedition were investigated, to reveal the changes of the surface-ocean environment and the evolution history of the WAIS since the MIS (Marine Isotope Stage) 6. Results show increased (decreased) productivity during interglacial (glacial) periods. In particular, the higher productivity level than the Holocene productivity ones during the MIS 5.5 was accompanied by significant WAIS melting. These findings could be interpreted as warmer sea surface, less sea ice, and stronger upwelling of the circum-polar deep water in the Amundsen Sea during the MIS 5.5. This study provided valuable information for predicting future climate changes.

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  • 图 1  阿蒙森海区域概况及研究站位

    Figure 1. 

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    图 2  南极冰芯EDC指示的南极温度变化[36]、全球海平面[37]、全球大洋底栖有孔虫LR04-δ18O曲线[32]与A5-7岩芯XRF-Ca/Al、-Si/Al，火山灰丰度（VG），IRD（>150 μm）含量对比（a）以及年龄控制点与线性沉积速率（b）

    Figure 2. 

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    图 3  南极EDC冰芯CO2浓度 [39]、温度变化 [36]、海冰覆盖指标ssNa+通量 [40]及风尘指标nssCa2+通量 [40]，德雷克海峡PS97/093-2岩芯XRF-Zr/Rb [41]，与A5-7岩芯有孔虫丰度、XRF-Ca/Al、-Si/Al、生物硅含量（opal）、有机碳与氮含量（TOC、TN）、有机碳氮比值 （C/N）、IRD含量（＞150 μm）和磁化率记录进行对比

    Figure 3. 

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    表 1  南极阿蒙森海ANT34-A5-7岩芯AMS 14C测年数据及其校正年龄

    Table 1.  Result and calibration of AMS 14C dating data of core A5-7

    深度/cm测试材料14C年龄/aBP碳储库和老碳校正年龄/aBP日历年 /aBP
    0～2有机碳12476±298645±297807±207
    2～4有机碳14081±3410250±3410091±274
    2～4N. pachyderma11550±3010250±3010091±222
    50～52有机碳25121±7321290±7323286±307
    74～76有机碳20168±5016337±5017524±282
    90～92有机碳26389±8422558±8424542±364
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    • 参考文献(69)
  • [1]

    The IMBIE Team. Mass balance of the Antarctic Ice Sheet from 1992 to 2017 [J]. Nature, 2018, 558(7709): 219-222. doi: 10.1038/s41586-018-0179-y

    [2]

    Shepherd A, Fricker H A, Farrell S L. Trends and connections across the Antarctic cryosphere [J]. Nature, 2018, 558(7709): 223-232. doi: 10.1038/s41586-018-0171-6

    [3]

    Mouginot J, Rignot E, Scheuchl B. Sustained increase in ice discharge from the Amundsen Sea Embayment, West Antarctica, from 1973 to 2013 [J]. Geophysical Research Letters, 2014, 41(5): 1576-1584. doi: 10.1002/2013GL059069

    [4]

    Larter R D, Anderson J B, Graham A G C, et al. Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum [J]. Quaternary Science Reviews, 2014, 100: 55-86. doi: 10.1016/j.quascirev.2013.10.016

    [5]

    Joughin I, Alley R B, Holland D M. Ice-sheet response to oceanic forcing [J]. Science, 2012, 338(6111): 1172-1176. doi: 10.1126/science.1226481

    [6]

    Alley K E, Scambos T A, Siegfried M R, et al. Impacts of warm water on Antarctic ice shelf stability through basal channel formation [J]. Nature Geoscience, 2016, 9(4): 290-293. doi: 10.1038/ngeo2675

    [7]

    Holland D M, Nicholls K W, Basinski A. The Southern Ocean and its interaction with the Antarctic Ice Sheet [J]. Science, 2020, 367(6484): 1326-1330. doi: 10.1126/science.aaz5491

    [8]

    Hillenbrand C D, Smith J A, Hodell D A, et al. West Antarctic Ice Sheet retreat driven by Holocene warm water incursions [J]. Nature, 2017, 547(7661): 43-48. doi: 10.1038/nature22995

    [9]

    Scherer R P, Aldahan A, Tulaczyk S, et al. Pleistocene collapse of the West Antarctic ice sheet [J]. Science, 1998, 281(5373): 82-85. doi: 10.1126/science.281.5373.82

    [10]

    Hillenbrand C D, Kuhn G, Frederichs T. Record of a Mid-Pleistocene depositional anomaly in West Antarctic continental margin sediments: an indicator for ice-sheet collapse? [J]. Quaternary Science Reviews, 2009, 28(13-14): 1147-1159. doi: 10.1016/j.quascirev.2008.12.010

    [11]

    Pollard D, DeConto R M. Modelling West Antarctic ice sheet growth and collapse through the past five million years [J]. Nature, 2009, 458(7236): 329-332. doi: 10.1038/nature07809

    [12]

    Hearty P J, Kindler P, Cheng H, et al. A +20 m middle Pleistocene sea-level highstand (Bermuda and the Bahamas) due to partial collapse of Antarctic ice [J]. Geology, 1999, 27(4): 375-378. doi: 10.1130/0091-7613(1999)027<0375:AMMPSL>2.3.CO;2

    [13]

    Kindler P, Hearty P J. Elevated marine terraces from Eleuthera (Bahamas) and Bermuda: sedimentological, petrographic and geochronological evidence for important deglaciation events during the middle Pleistocene [J]. Global and Planetary Change, 2000, 24(1): 41-58. doi: 10.1016/S0921-8181(99)00068-5

    [14]

    李永斌, 王汝建, 武力, 等. 南极罗斯海扇区晚更新世以来冰筏碎屑记录反映的冰川动力学史[J]. 第四纪研究, 2021, 41(3):662-677 doi: 10.11928/j.issn.1001-7410.2021.03.04

    LI Yongbin, WANG Rujian, WU Li, et al. Glacial dynamics evolutions revealed by ice-rafted detritus record from the Ross Sea Sector of the Southern Ocean since Late Pleistocene [J]. Quaternary Sciences, 2021, 41(3): 662-677. doi: 10.11928/j.issn.1001-7410.2021.03.04

    [15]

    Talley L D, Pickard G L, Emery W J, et al. Descriptive Physical Oceanography: An Introduction[M]. 6th ed. London: Academic Press, 2011.

    [16]

    Walker D P, Brandon M A, Jenkins A, et al. Oceanic heat transport onto the Amundsen Sea shelf through a submarine glacial trough [J]. Geophysical Research Letters, 2007, 34(2): L02602.

    [17]

    Jacobs S S, Jenkins A, Giulivi C F, et al. Stronger ocean circulation and increased melting under Pine Island Glacier ice shelf [J]. Nature Geoscience, 2011, 4(8): 519-523. doi: 10.1038/ngeo1188

    [18]

    Turner J, Orr A, Gudmundsson G H, et al. Atmosphere-ocean-ice interactions in the Amundsen Sea Embayment, West Antarctica [J]. Reviews of Geophysics, 2017, 55(1): 235-276. doi: 10.1002/2016RG000532

    [19]

    Jenkins A, Dutrieux P, Jacobs S, et al. Decadal ocean forcing and Antarctic ice sheet response: Lessons from the Amundsen Sea [J]. Oceanography, 2016, 29(4): 106-117. doi: 10.5670/oceanog.2016.103

    [20]

    Parkinson C L, Cavalieri D J. Antarctic sea ice variability and trends, 1979-2010 [J]. Cryosphere, 2012, 6(4): 871-880. doi: 10.5194/tc-6-871-2012

    [21]

    Orsi A H, Whitworth III T, Nowlin Jr W D. On the meridional extent and fronts of the Antarctic circumpolar current [J]. Deep Sea Research Part I:Oceanographic Research Papers, 1995, 42(5): 641-673. doi: 10.1016/0967-0637(95)00021-W

    [22]

    Assmann K M, Hellmer H H, Jacobs S S. Amundsen Sea ice production and transport [J]. Journal of Geophysical Research, 2005, 110(C12): C12013. doi: 10.1029/2004JC002797

    [23]

    Lythe M B, Vaughan D G, the BEDMAP Consortium. BEDMAP: a new ice thickness and subglacial topographic model of Antarctica [J]. Journal of Geophysical Research, 2001, 106(B6): 11335-11351. doi: 10.1029/2000JB900449

    [24]

    鞠梦珊, 陈志华, 赵仁杰, 等. 晚第四纪南极阿蒙森海扇区冰盖与古生产力旋回变化[J]. 海洋学报, 2019, 41(9):40-51

    JU Mengshan, CHEN Zhihua, ZHAO Renjie, et al. Late Quaternary cyclic variations of ice sheet and paleoproductivity in the Amundsen Sea sector, Antarctica [J]. Haiyang Xuebao, 2019, 41(9): 40-51.

    [25]

    Berkman P A, Forman S L. Pre-bomb radiocarbon and the reservoir correction for calcareous marine species in the Southern Ocean [J]. Geophysical Research Letters, 1996, 23(4): 363-366. doi: 10.1029/96GL00151

    [26]

    Gordon J E, Harkness D D. Magnitude and geographic variation of the radiocarbon content in Antarctic marine life: implications for reservoir corrections in radiocarbon dating [J]. Quaternary Science Reviews, 1992, 11(7-8): 697-708. doi: 10.1016/0277-3791(92)90078-M

    [27]

    Domack E, Leventer A, Dunbar R, et al. Chronology of the Palmer Deep site, Antarctic Peninsula: a Holocene palaeoenvironmental reference for the circum-Antarctic [J]. The Holocene, 2001, 11(1): 1-9. doi: 10.1191/095968301673881493

    [28]

    Stuiver M, Reimer P J. Extended 14C data base and revised Calib 3.0 14C age calibration program [J]. Radiocarbon, 1993, 35(1): 215-230. doi: 10.1017/S0033822200013904

    [29]

    Heaton T J, Köhler P, Butzin M, et al. Marine20-the marine radiocarbon age calibration curve (0-55, 000 Cal Bp) [J]. Radiocarbon, 2020, 62(4): 779-820. doi: 10.1017/RDC.2020.68

    [30]

    Mortlock R A, Froelich P N. A simple method for the rapid determination of biogenic opal in pelagic marine sediments [J]. Deep Sea Research Part A. Oceanographic Research Papers, 1989, 36(9): 1415-1426. doi: 10.1016/0198-0149(89)90092-7

    [31]

    Xiao W S, Frederichs T, Gersonde R, et al. Constraining the dating of late Quaternary marine sediment records from the Scotia Sea (Southern Ocean) [J]. Quaternary Geochronology, 2016, 31: 97-118. doi: 10.1016/j.quageo.2015.11.003

    [32]

    Lisiecki L E, Raymo M E. A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records [J]. Paleoceanography, 2005, 20(1): PA1003.

    [33]

    Wu L, Wang R J, Xiao W S, et al. Productivity-climate coupling recorded in Pleistocene sediments off Prydz Bay (East Antarctica) [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2017, 485: 260-270. doi: 10.1016/j.palaeo.2017.06.018

    [34]

    Hillenbrand C D, Fütterer D K, Grobe H, et al. No evidence for a Pleistocene collapse of the West Antarctic Ice Sheet from continental margin sediments recovered in the Amundsen Sea [J]. Geo-Marine Letters, 2002, 22(2): 51-59. doi: 10.1007/s00367-002-0097-7

    [35]

    Hillenbrand C D, Moreton S G, Caburlotto A, et al. Volcanic time-markers for Marine Isotopic Stages 6 and 5 in Southern Ocean sediments and Antarctic ice cores: implications for tephra correlations between palaeoclimatic records [J]. Quaternary Science Reviews, 2008, 27(5-6): 518-540. doi: 10.1016/j.quascirev.2007.11.009

    [36]

    Jouzel J, Masson-Delmotte V, Cattani O, et al. Orbital and millennial Antarctic climate variability over the past 800, 000 years [J]. Science, 2007, 317(5839): 793-796. doi: 10.1126/science.1141038

    [37]

    Miller K G, Mountain G S, Wright J D, et al. A 180-million-year record of sea level and ice volume variations from continental margin and deep-sea isotopic records [J]. Oceanography, 2011, 24(2): 40-53. doi: 10.5670/oceanog.2011.26

    [38]

    Turney C S M, Fogwill C J, Golledge N R, et al. Early Last Interglacial ocean warming drove substantial ice mass loss from Antarctica [J]. Proceedings of the National Academy of Sciences of the United States of America, 2020, 117(8): 3996-4006. doi: 10.1073/pnas.1902469117

    [39]

    Lüthi D, Le Floch M, Bereiter B, et al. High-resolution carbon dioxide concentration record 650, 000-800, 000 years before present [J]. Nature, 2008, 453(7193): 379-382. doi: 10.1038/nature06949

    [40]

    Wolff E W, Fischer H, Fundel F, et al. Southern Ocean sea-ice extent, productivity and iron flux over the past eight glacial cycles [J]. Nature, 2006, 440(7083): 491-496. doi: 10.1038/nature04614

    [41]

    Toyos M H, Lamy F, Lange C B, et al. Antarctic circumpolar current dynamics at the Pacific Entrance to the Drake Passage over the past 1.3 million years [J]. Paleoceanography and Paleoclimatology, 2020, 35(7): e2019PA003773.

    [42]

    Anderson R F, Barker S, Fleisher M, et al. Biological response to millennial variability of dust and nutrient supply in the Subantarctic South Atlantic Ocean [J]. Philosophical Transactions of the Royal Society A:Mathematical, Physical and Engineering Sciences, 2014, 372(2019): 20130054. doi: 10.1098/rsta.2013.0054

    [43]

    Stein R. Accumulation of organic carbon in marine sediments[D]. Doctor Dissertation of Universität Giessen, 1991.

    [44]

    Meyers P A. Preservation of elemental and isotopic source identification of sedimentary organic matter [J]. Chemical Geology, 1994, 114(3-4): 289-302. doi: 10.1016/0009-2541(94)90059-0

    [45]

    Thornton S F, McManus J. Application of organic carbon and nitrogen stable isotope and C/N ratios as source indicators of organic matter provenance in estuarine systems: evidence from the Tay Estuary, Scotland [J]. Estuarine, Coastal and Shelf Science, 1994, 38(3): 219-233. doi: 10.1006/ecss.1994.1015

    [46]

    Hillenbrand C D, Grobe H, Diekmann B, et al. Distribution of clay minerals and proxies for productivity in surface sediments of the Bellingshausen and Amundsen seas (West Antarctica) - Relation to modern environmental conditions [J]. Marine Geology, 2003, 193(3-4): 253-271. doi: 10.1016/S0025-3227(02)00659-X

    [47]

    Diekmann B. Sedimentary patterns in the late Quaternary Southern Ocean [J]. Deep Sea Research Part II:Topical Studies in Oceanography, 2007, 54(21-22): 2350-2366. doi: 10.1016/j.dsr2.2007.07.025

    [48]

    Billups K, York K, Bradtmiller L I. Water column stratification in the Antarctic Zone of the southern ocean during the mid-Pleistocene climate transition [J]. Paleoceanography and Paleoclimatology, 2018, 33(5): 432-442. doi: 10.1029/2018PA003327

    [49]

    Esper O, Gersonde R, Kadagies N. Diatom distribution in southeastern Pacific surface sediments and their relationship to modern environmental variables [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 287(1-4): 1-27. doi: 10.1016/j.palaeo.2009.12.006

    [50]

    Pudsey C J, Howe J A. Quaternary history of the Antarctic Circumpolar Current: evidence from the Scotia Sea [J]. Marine Geology, 1998, 148(1-2): 83-112. doi: 10.1016/S0025-3227(98)00014-0

    [51]

    Chadwick M, Allen C S, Sime L C, et al. Reconstructing Antarctic winter sea-ice extent during Marine isotope Stage 5e [J]. Climate of the Past, 2022, 18(1): 129-146. doi: 10.5194/cp-18-129-2022

    [52]

    Crosta X, Kohfeld K E, Bostock H C, et al. Antarctic sea ice over the past 130 000 years - Part 1: a review of what proxy records tell us [J]. Climate of the Past, 2022, 18(8): 1729-1756. doi: 10.5194/cp-18-1729-2022

    [53]

    Chadwick M, Allen C S, Sime L C, et al. How does the Southern Ocean palaeoenvironment during Marine Isotope Stage 5e compare to the modern? [J]. Marine Micropaleontology, 2022, 170: 102066. doi: 10.1016/j.marmicro.2021.102066

    [54]

    Robinson R S, Sigman D M. Nitrogen isotopic evidence for a poleward decrease in surface nitrate within the ice age Antarctic [J]. Quaternary Science Reviews, 2008, 27(9-10): 1076-1090. doi: 10.1016/j.quascirev.2008.02.005

    [55]

    Sigman D M, Hain M P, Haug G H. The polar ocean and glacial cycles in atmospheric CO2 concentration [J]. Nature, 2010, 466(7302): 47-55. doi: 10.1038/nature09149

    [56]

    Anderson J B, Shipp S S, Lowe A L, et al. The Antarctic Ice Sheet during the Last Glacial Maximum and its subsequent retreat history: a review [J]. Quaternary Science Reviews, 2002, 21(1-3): 49-70. doi: 10.1016/S0277-3791(01)00083-X

    [57]

    Studer A S, Sigman D M, Martínez-García A, et al. Antarctic Zone nutrient conditions during the last two glacial cycles [J]. Paleoceanography, 2015, 30(7): 845-862. doi: 10.1002/2014PA002745

    [58]

    Horn M G, Beucher C P, Robinson R S, et al. Southern ocean nitrogen and silicon dynamics during the last deglaciation [J]. Earth and Planetary Science Letters, 2011, 310(3-4): 334-339. doi: 10.1016/j.jpgl.2011.08.016

    [59]

    Jaccard S L, Hayes C T, Martínez-Garcia A, et al. Two modes of change in southern ocean productivity over the past million years [J]. Science, 2013, 339(6126): 1419-1423. doi: 10.1126/science.1227545

    [60]

    Sigman D M, Fripiat F, Studer A S, et al. The Southern Ocean during the ice ages: a review of the Antarctic surface isolation hypothesis, with comparison to the North Pacific [J]. Quaternary Science Reviews, 2021, 254: 106732. doi: 10.1016/j.quascirev.2020.106732

    [61]

    Sigman D M, Boyle E A. Palaeoceanography: Antarctic stratification and glacial CO2 [J]. Nature, 2001, 412(6847): 606. doi: 10.1038/35088132

    [62]

    Toggweiler J R, Russell J L, Carson S R. Midlatitude westerlies, atmospheric CO2, and climate change during the ice ages [J]. Paleoceanography, 2006, 21(2): PA2005.

    [63]

    Martínez-García A, Sigman D M, Ren H J, et al. Iron fertilization of the Subantarctic Ocean during the last ice age [J]. Science, 2014, 343(6177): 1347-1350. doi: 10.1126/science.1246848

    [64]

    Anderson R F, Ali S, Bradtmiller L I, et al. Wind-driven upwelling in the southern ocean and the deglacial rise in atmospheric CO2 [J]. Science, 2009, 323(5920): 1443-1448. doi: 10.1126/science.1167441

    [65]

    Wu S Z, Lembke-Jene L, Lamy F, et al. Orbital- and millennial-scale Antarctic Circumpolar Current variability in Drake Passage over the past 140, 000 years [J]. Nature Communications, 2021, 12(1): 3948. doi: 10.1038/s41467-021-24264-9

    [66]

    Gordon A L. Interocean exchange of thermocline water [J]. Journal of Geophysical Research, 1986, 91(C4): 5037-5046. doi: 10.1029/JC091iC04p05037

    [67]

    Dutton A, Carlson A E, Long A J, et al. Sea-level rise due to polar ice-sheet mass loss during past warm periods [J]. Science, 2015, 349(6244): aaa4019. doi: 10.1126/science.aaa4019

    [68]

    Dutton A, Lambeck K. Ice volume and sea level during the last interglacial [J]. Science, 2012, 337(6091): 216-219. doi: 10.1126/science.1205749

    [69]

    Bareille G, Grousset F E, Labracherie M, et al. Origin of detrital fluxes in the Southeast Indian Ocean during the last climatic cycles [J]. Paleoceanography, 1994, 9(6): 799-819. doi: 10.1029/94PA01946

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收稿日期:  2023-02-08
修回日期:  2023-02-22
录用日期:  2023-02-22
刊出日期:  2023-04-28

目录

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