北太平洋大洋钻探研究进展

张亚南; 仲义; 陈艇; 赵德博; 王敦繁; 盖聪聪; 姜兆霞; 蒋晓东; 刘青松

doi:10.16562/j.cnki.0256-1492.2022062501

北太平洋大洋钻探研究进展

1.
南方科技大学海洋科学与工程系海洋磁学中心，深圳 518055

2.
重庆师范大学长江上游湿地科学研究重庆市重点实验室，重庆 400047

3.
中国科学院海洋研究所海洋地质与环境重点实验室，青岛 266071

4.
中国海洋大学海底科学与探测技术教育部重点实验室，青岛 266100

基金项目: 国家自然科学基金重点项目“南海与东菲律宾海协同演化研究”（92158208）；国家自然科学基金“上新世亚北极太平洋硅藻种群特征及其环境控制因素”（41904069）；同济大学海洋地质国家重点实验室开放课题“晚第四纪以来亚北极太平洋地区高-低纬度气候系统响应机制研究”（MGK202209）；重庆师范大学博士启动/人才引进项目“三峡库区消落带沉积物环境磁学特征及其对重金属污染的指示”（20XLB021）

详细信息

作者简介: 张亚南（1994—），男，博士，主要从事古海洋沉积方面的研究工作，E-mail：yananzhang9@163.com

通讯作者: 刘青松（1972—），男，教授，博士生导师，主要从事海洋磁学方面的研究，E-mail：qsliu@sustech.edu.cn

中图分类号: P736

收稿日期: 2022-06-25

修回日期: 2022-08-02

录用日期: 2022-08-02

刊出日期: 2022-10-28

Research progress of ocean drilling in the North Pacific Ocean: Paleoceanography and paleoclimate

1.
Southern University of Science and Technology, Department of Ocean Science and Engineering, Shenzhen 518055, China

2.
Chongqing Normal University, Chongqing key laboratory of wetland science research in the upper Yangtze River, Chongqing 400047, China

3.
Institute of Oceanology, Chinese Academy of Sciences, Key Laboratory of Marine Geology and Environment, Qingdao 266071, China

4.
Ocean University of China, Key Laboratory of Submarine Geosciences and Prospecting Techniques, Qingdao 266100, China

More Information

Corresponding author: LIU Qingsong, qsliu@sustech.edu.cn

Received Date: 25 June 2022

Revised Date: 02 August 2022

Accepted Date: 02 August 2022

Publish Date: 28 October 2022

摘要

摘要:
北太平洋作为全球大洋环流的重要组成部分，在高低纬间热量和物质的传输与再分配方面起到重要的调控作用，进而影响到地球气候系统。基于过去50多年来的大洋钻探工作，前人在北太平洋地球科学的研究上取得了一系列的成果。本文回顾了北太平洋古海洋和古气候方面的研究进展，包括：（1）东亚夏季风和西部边界流演化，以及其对高低纬热量、水汽的传输；（2）北太平洋中层水和深层水的性质变化、分布范围和驱动机制，以及冰期旋回中水体垂直交换作用的气候响应；（3）风尘输入对亚洲内陆古环境的反映，及其对北太平洋生产力的铁肥效应。尽管前人针对上述科学问题都开展了相应的研究工作，但目前在对北太平洋上述几方面的认识上仍然存在着分歧。基于对前人研究的总结概括，本文最后提出了未来北太平洋研究的关键科学问题，强调了多圈层、多系统角度对深入认识过去地球气候系统变化的重要性，并对未来大洋航次开展的理想靶区进行了展望。
- 大洋钻探 /
- 东亚夏季风 /
- 西部边界流 /
- 风尘 /
- 生产力 /
- 北太平洋
Abstract:
As an important part of global ocean circulation, the North Pacific Ocean plays a key role in regulating the transfer and redistribution of heat and matter between high and low latitudes, thus affecting the Earth’s climate system. Based on the ocean drilling programs over 50 years in the past, many achievements in geoscience have been made. We reviewed the progresses of paleoclimate research in the North Pacific in the following aspects: (1) the evolution of the East Asian summer monsoon and the western boundary current, as well as their contributions to the transportation of heat and water vapor between high and low latitudes in North Pacific; (2) changes in water property, distribution, and the driving mechanisms of the Pacific Deep Water and North Pacific Intermediate Water, as well as the climatic response of their interaction during glacial-interglacial cycles; (3) the response of aeolian flux to the Asian inland and its iron fertilization effect on the North Pacific productivity. Previous studies have addressed those scientific problems, uncertain issued remain controversial. We therefore proposed the key scientific issues for future research in the North Pacific Ocean, and emphasized the importance of multi-layer and multi-system perspectives for deciphering the past changes of the Earth's climate system. Finally, we suggested the ideal target areas for ocean drilling program in North Pacific in the future.
- ocean drilling /
- East Asian summer monsoon /
- western boundary current /
- eolian dust /
- productivity /
- North Pacific

HTML全文

图 1 北太平洋（＞35°N）古海洋与古气候大洋钻探航次及站位

Figure 1.

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图 2 晚第四纪东亚夏季风记录对比

Figure 2.

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图 3 北太平洋海表温度及表层环流

Figure 3.

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图 4 北太平洋中层水（NPIW）演化及其气候响应（850 ka以来）

Figure 4.

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图 5 北太平洋风尘通量记录对比

Figure 5.

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图 6 北太平洋生产力变化模式

Figure 6.

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图 7 北太平洋多圈层耦合过程示意图

Figure 7.

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表 1 北太平洋古海洋与古气候大洋钻探航次

Table 1. The ocean drilling expeditions in the North Pacific

航次	钻探区域	主要研究目标	钻探站位	时间
Leg 86/88	西北太平洋	风尘、黑潮延伸流	576—581	1982
Leg 145	亚北极太平洋	风尘、NPIW	881—887	1993
Leg 198	沙莰基隆起	深水环流	1207—1214	2001
323	白令海	NPIW	U1339—1345	2009
341	阿拉斯加大陆边缘	NPIW	U1417—1421	2013
346	日本海	东亚季风	U1422—1430	2013

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参考文献(139)

[1]	Worne S, Kender S, Swann G E A, et al. Coupled climate and subarctic Pacific nutrient upwelling over the last 850, 000 years [J]. Earth and Planetary Science Letters, 2019, 522: 87-97. doi: 10.1016/j.jpgl.2019.06.028
[2]	Jaccard S L, Haug G H, Sigman D M, et al. Glacial/interglacial changes in subarctic north pacific stratification [J]. Science, 2005, 308(5724): 1003-1006. doi: 10.1126/science.1108696
[3]	Takahashi K, Ravelo A, Alvarez-Zarikian C. Pliocene-Pleistocene paleoceanography and climate history of the Bering Sea[R]. Scientific Prospectus, IODP, 323, 2009: 3-4,doi: 10.2204/iodp.sp.323.2009.
[4]	Gray W R, Rae J W B, Wills R C J, et al. Deglacial upwelling, productivity and CO₂ outgassing in the North Pacific Ocean [J]. Nature Geoscience, 2018, 11(5): 340-344. doi: 10.1038/s41561-018-0108-6
[5]	Paulmier A, Ruiz-Pino D. Oxygen minimum zones (OMZs) in the modern ocean [J]. Progress in Oceanography, 2009, 80(3-4): 113-128. doi: 10.1016/j.pocean.2008.08.001
[6]	Schmidtko S, Stramma L, Visbeck M. Decline in global oceanic oxygen content during the past five decades [J]. Nature, 2017, 542(7641): 335-339. doi: 10.1038/nature21399
[7]	Deutsch C, Brix H, Ito T, et al. Climate-forced variability of ocean hypoxia [J]. Science, 2011, 333(6040): 336-339. doi: 10.1126/science.1202422
[8]	Shao Y P, Wyrwoll K H, Chappell A, et al. Dust cycle: An emerging core theme in Earth system science [J]. Aeolian Research, 2011, 2(4): 181-204. doi: 10.1016/j.aeolia.2011.02.001
[9]	Forster P, Ramaswamy V, Artaxo P, et al. Changes in atmospheric constituents and in radiative forcing[C]//Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press, 2007: 129-234.
[10]	Martin J H. Glacial-interglacial CO₂ change: The iron hypothesis [J]. Paleoceanography, 1990, 5(1): 1-13. doi: 10.1029/PA005i001p00001
[11]	Mitchell B G, Brody E A, Holm-Hansen O, et al. Light limitation of phytoplankton biomass and macronutrient utilization in the Southern Ocean [J]. Limnology and Oceanography, 1991, 36(8): 1662-1677. doi: 10.4319/lo.1991.36.8.1662
[12]	Li D W, Zheng L W, Jaccard S L, et al. Millennial-scale ocean dynamics controlled export productivity in the subtropical North Pacific [J]. Geology, 2017, 45(7): 651-654. doi: 10.1130/G38981.1
[13]	Lam P J, Robinson L F, Blusztajn J, et al. Transient stratification as the cause of the North Pacific productivity spike during deglaciation [J]. Nature Geoscience, 2013, 6(8): 622-626. doi: 10.1038/NGEO1873
[14]	Schlitzer R. Ocean data view[EB/OL]. 2022(2022-04-04). https://odv.awi.de.
[15]	Ogi M, Tachibana Y. Influence of the annual Arctic Oscillation on the negative correlation between Okhotsk Sea ice and Amur River discharge [J]. Geophysical Research Letters, 2006, 33(8): L08709. doi: 10.1029/2006GL025838
[16]	Shcherbina A Y, Talley L D, Rudnick D L. Direct observations of North Pacific ventilation: Brine rejection in the Okhotsk Sea [J]. Science, 2003, 302(5652): 1952-1955. doi: 10.1126/science.1088692
[17]	Emile-Geay J, Cane M A, Naik N, et al. Warren revisited: Atmospheric freshwater fluxes and "Why is no deep water formed in the North Pacific'' [J]. Journal of Geophysical Research:Oceans, 2003, 108(C6): 3178. doi: 10.1029/2001JC001058
[18]	Wang P X, Wang B, Cheng H, et al. The global monsoon across time scales: Mechanisms and outstanding issues [J]. Earth-Science Reviews, 2017, 174: 84-121. doi: 10.1016/j.earscirev.2017.07.006
[19]	Maher B A, Thompson R. Oxygen isotopes from Chinese caves: records not of monsoon rainfall but of circulation regime [J]. Journal of Quaternary Science, 2012, 27(6): 615-624. doi: 10.1002/jqs.2553
[20]	Parker S E, Harrison S P, Comas-Bru L, et al. A data-model approach to interpreting speleothem oxygen isotope records from monsoon regions [J]. Climate of the Past, 2021, 17(3): 1119-1138. doi: 10.5194/cp-17-1119-2021
[21]	Caley T, Roche D M, Renssen H. Orbital Asian summer monsoon dynamics revealed using an isotope-enabled global climate model [J]. Nature Communications, 2014, 5: 5371. doi: 10.1038/ncomms6371
[22]	Liu J B, Chen J H, Zhang X J, et al. Holocene East Asian summer monsoon records in northern China and their inconsistency with Chinese stalagmite δ¹⁸O records [J]. Earth-Science Reviews, 2015, 148: 194-208. doi: 10.1016/j.earscirev.2015.06.004
[23]	Rao Z G, Jia G D, Li Y X, et al. Asynchronous evolution of the isotopic composition and amount of precipitation in north China during the Holocene revealed by a record of compound-specific carbon and hydrogen isotopes of long-chain n-alkanes from an alpine lake [J]. Earth and Planetary Science Letters, 2016, 446: 68-76. doi: 10.1016/j.jpgl.2016.04.027
[24]	Cheng H, Edwards R L, Sinha A, et al. The Asian monsoon over the past 640, 000 years and ice age terminations [J]. Nature, 2016, 534(7609): 640-646. doi: 10.1038/nature18591
[25]	Cheng H, Zhang H W, Cai Y J, et al. Orbital-scale Asian summer monsoon variations: Paradox and exploration [J]. Science China Earth Sciences, 2021, 64(4): 529-544. doi: 10.1007/s11430-020-9720-y
[26]	Zhang H W, Zhang X, Cai Y J, et al. A data-model comparison pinpoints Holocene spatiotemporal pattern of East Asian summer monsoon [J]. Quaternary Science Reviews, 2021, 261: 106911. doi: 10.1016/j.quascirev.2021.106911
[27]	Beck J W, Zhou W J, Li C, et al. A 550, 000-year record of East Asian monsoon rainfall from ¹⁰Be in loess [J]. Science, 2018, 360(6391): 877-881. doi: 10.1126/science.aam5825
[28]	Sun Y B, Kutzbach J, An Z S, et al. Astronomical and glacial forcing of East Asian summer monsoon variability [J]. Quaternary Science Reviews, 2015, 115: 132-142. doi: 10.1016/j.quascirev.2015.03.009
[29]	Hao Q Z, Wang L, Oldfield F, et al. Delayed build-up of Arctic ice sheets during 400, 000-year minima in insolation variability [J]. Nature, 2012, 490(7420): 393-396. doi: 10.1038/nature11493
[30]	Clemens S C, Holbourn A, Kubota Y, et al. Precession-band variance missing from East Asian monsoon runoff [J]. Nature Communications, 2018, 9(1): 3364. doi: 10.1038/s41467-018-05814-0
[31]	Zhao D B, Wan S M, Lu Z Y, et al. Response of heterogeneous rainfall variability in East Asia to Hadley circulation reorganization during the late Quaternary [J]. Quaternary Science Reviews, 2020, 247: 106562. doi: 10.1016/j.quascirev.2020.106562
[32]	Igarashi Y, Oba T. Fluctuations in the East Asian monsoon over the last 144ka in the northwest Pacific based on a high-resolution pollen analysis of IMAGES core MD01-2421 [J]. Quaternary Science Reviews, 2006, 25(13-14): 1447-1459. doi: 10.1016/j.quascirev.2005.11.011
[33]	Morley J J, Heusser L E. Role of orbital forcing in East Asian monsoon climates during the last 350 kyr: evidence from terrestrial and marine climate proxies from core RC14‐99 [J]. Paleoceanography, 1997, 12(3): 483-493. doi: 10.1029/97PA00213
[34]	Thomas E K, Clemens S C. Prell W L, et al. Temperature and leaf wax δ²H records demonstrate seasonal and regional controls on Asian monsoon proxies [J]. Geology, 2014, 42(12): 1075-1078. doi: 10.1130/G36289.1
[35]	Kong X H, Zhou W J, Beck J W, et al. Loess magnetic susceptibility flux: a new proxy of East Asian monsoon precipitation [J]. Journal of Asian Earth Sciences, 2020, 201: 104489. doi: 10.1016/j.jseaes.2020.104489
[36]	Sun Y B, Wang T, Yin Q Z, et al. A review of orbital-scale monsoon variability and dynamics in East Asia during the Quaternary [J]. Quaternary Science Reviews, 2022, 288: 107593. doi: 10.1016/j.quascirev.2022.107593
[37]	Gu Z Y, Lal D, Liu T S, et al. Five million year ¹⁰Be record in Chinese loess and red-clay: climate and weathering relationships [J]. Earth and Planetary Science Letters, 1996, 144(1-2): 273-287. doi: 10.1016/0012-821X(96)00156-2
[38]	Sun Y B, An Z S, Clemens S C, et al. Seven million years of wind and precipitation variability on the Chinese Loess Plateau [J]. Earth and Planetary Science Letters, 2010, 297(3-4): 525-535. doi: 10.1016/j.jpgl.2010.07.004
[39]	Dai G W, Zhang Z S, Otterå O H, et al. A modeling study of the tripole pattern of East China precipitation over the past 425 ka [J]. Journal of Geophysical Research:Atmospheres, 2021, 126(7): e2020JD033513.
[40]	陈大可, 连涛. 厄尔尼诺-南方涛动研究新进展[J]. 科学通报, 2020, 65(35):4001-4003 doi: 10.1360/TB-2020-1219 CHEN Dake, LIAN Tao. Frontier of El Niño-Southern oscillation research [J]. Chinese Science Bulletin, 2020, 65(35): 4001-4003. doi: 10.1360/TB-2020-1219
[41]	Hu D X, Wu L X, Cai W J, et al. Pacific western boundary currents and their roles in climate [J]. Nature, 2015, 522(7556): 299-308. doi: 10.1038/nature14504
[42]	Navarra G G, Di Lorenzo E. Poleward shift and intensified variability of Kuroshio-Oyashio extension and North Pacific Transition Zone under climate change [J]. Climate Dynamics, 2021, 56(7-8): 2469-2486. doi: 10.1007/s00382-021-05677-0
[43]	Wang L, Li T, Zhou T J. Intraseasonal SST variability and air-sea interaction over the Kuroshio Extension region during boreal summer [J]. Journal of Climate, 2012, 25(5): 1619-1634. doi: 10.1175/JCLI-D-11-00109.1
[44]	Tittensor D P, Mora C, Jetz W, et al. Global patterns and predictors of marine biodiversity across taxa [J]. Nature, 2010, 466(7310): 1098-1101. doi: 10.1038/nature09329
[45]	Noto M, Yasuda I. Population decline of the Japanese sardine, Sardinops melanostictus, in relation to sea surface temperature in the Kuroshio Extension [J]. Canadian Journal of Fisheries and Aquatic Sciences, 1999, 56(6): 973-983. doi: 10.1139/f99-028
[46]	Zhang Y, Zhang Z G, Chen D K, et al. Strengthening of the Kuroshio current by intensifying tropical cyclones [J]. Science, 2020, 368(6494): 988-993. doi: 10.1126/science.aax5758
[47]	Wu L X, Cai W J, Zhang L P, et al. Enhanced warming over the global subtropical western boundary currents [J]. Nature Climate Change, 2012, 2(3): 161-166. doi: 10.1038/NCLIMATE1353
[48]	Vats N, Mishra S, Singh R K, et al. Paleoceanographic changes in the East China Sea during the last~400 kyr reconstructed using planktic foraminifera [J]. Global and Planetary Change, 2020, 189: 103173. doi: 10.1016/j.gloplacha.2020.103173
[49]	Lam A R, Leckie R M. Subtropical to temperate late Neogene to Quaternary planktic foraminiferal biostratigraphy across the Kuroshio Current Extension, Shatsky Rise, northwest Pacific Ocean [J]. PLoS One, 2020, 15(7): e0234351. doi: 10.1371/journal.pone.0234351
[50]	Gallagher S J, Kitamura A, Iryu Y, et al. The Pliocene to recent history of the Kuroshio and Tsushima Currents: a multi-proxy approach [J]. Progress in Earth and Planetary Science, 2015, 2(1): 17. doi: 10.1186/s40645-015-0045-6
[51]	Gallagher S J, Wallace M W, Li C L, et al. Neogene history of the West Pacific Warm Pool, Kuroshio and Leeuwin currents [J]. Paleoceanography, 2009, 24(1): PA1206. doi: 10.1029/2008PA001660
[52]	Lam A R, MacLeod K G, Schilling S H, et al. Pliocene to earliest pleistocene (5-2.5 Ma) reconstruction of the Kuroshio current extension reveals a dynamic current [J]. Paleoceanography and Paleoclimatology, 2021, 36(9): e2021PA004318. doi: 10.1029/2021PA004318
[53]	LaRiviere J P, Ravelo A C, Crimmins A, et al. Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing [J]. Nature, 2012, 486(7401): 97-100. doi: 10.1038/nature11200
[54]	Venti N L, Billups K, Herbert T D. Increased sensitivity of the Plio-Pleistocene northwest Pacific to obliquity forcing [J]. Earth and Planetary Science Letters, 2013, 384: 121-131. doi: 10.1016/j.jpgl.2013.10.007
[55]	Rakestraw N W. The oceans: Their physics, chemistry, and general biology (Sverdrup, H. U.; Johnson, Martin W.; Fleming, Richard H.) [J]. Journal of Chemical Education, 1943, 20(10): 517. doi: 10.1021/ed020p517.1
[56]	Talley L D. An Okhotsk Sea water anomaly: implications for ventilation in the North Pacific [J]. Deep Sea Research Part A. Oceanographic Research Papers, 1991, 38: S171-S190. doi: 10.1016/S0198-0149(12)80009-4
[57]	Yasuda I, Kouketsu S, Katsumata K, et al. Influence of Okhotsk sea intermediate water on the Oyashio and North Pacific intermediate water [J]. Journal of Geophysical Research:Oceans, 2002, 107(C12): 3237. doi: 10.1029/2001JC001037
[58]	You Y Z, Suginohara N, Fukasawa M, et al. Roles of the Okhotsk sea and gulf of alaska in forming the north pacific intermediate water [J]. Journal of Geophysical Research:Oceans, 2000, 105(C2): 3253-3280. doi: 10.1029/1999JC900304
[59]	You Y Z. Implications of cabbeling on the formation and transformation mechanism of North Pacific Intermediate Water [J]. Journal of Geophysical Research:Oceans, 2003, 108(C5): 3134. doi: 10.1029/2001JC001285
[60]	Talley L D. Distribution and formation of North Pacific intermediate water [J]. Journal of Physical Oceanography, 1993, 23(3): 517-537. doi: 10.1175/1520-0485(1993)023<0517:DAFONP>2.0.CO;2
[61]	Sigman D M, Jaccard S L, Haug G H. Polar ocean stratification in a cold climate [J]. Nature, 2004, 428(6978): 59-63. doi: 10.1038/nature02357
[62]	Haug G H, Sigman D M. Polar twins [J]. Nature Geoscience, 2009, 2(2): 91-92. doi: 10.1038/ngeo423
[63]	Studer A S, Martínez-Garcia A, Jaccard S L, et al. Enhanced stratification and seasonality in the Subarctic Pacific upon Northern Hemisphere Glaciation-New evidence from diatom-bound nitrogen isotopes, alkenones and archaeal tetraethers [J]. Earth and Planetary Science Letters, 2012, 351-352: 84-94. doi: 10.1016/j.jpgl.2012.07.029
[64]	Burls N J, Fedorov A V, Sigman D M, et al. Active Pacific meridional overturning circulation (PMOC) during the warm Pliocene [J]. Science Advances, 2017, 3(9): e1700156. doi: 10.1126/sciadv.1700156
[65]	Kender S, Ravelo A C, Worne S, et al. Closure of the Bering strait caused Mid-Pleistocene transition cooling [J]. Nature Communications, 2018, 9(1): 5386. doi: 10.1038/s41467-018-07828-0
[66]	Cook M S, Ravelo A C, Mix A, et al. Tracing subarctic Pacific water masses with benthic foraminiferal stable isotopes during the LGM and late Pleistocene [J]. Deep Sea Research Part Ⅱ:Topical Studies in Oceanography, 2016, 125-126: 84-95. doi: 10.1016/j.dsr2.2016.02.006
[67]	Sagawa T, Ikehara K. Intermediate water ventilation change in the subarctic northwest Pacific during the last deglaciation [J]. Geophysical Research Letters, 2008, 35(24): L24702. doi: 10.1029/2008GL035133
[68]	Matsumoto K, Oba T, Lynch-Stieglitz J, et al. Interior hydrography and circulation of the glacial Pacific Ocean [J]. Quaternary Science Reviews, 2002, 21(14-15): 1693-1704. doi: 10.1016/s0277-3791(01)00142-1
[69]	Keigwin L D. Glacial-age hydrography of the far northwest Pacific Ocean [J]. Paleoceanography, 1998, 13(4): 323-339. doi: 10.1029/98PA00874
[70]	Keigwin L D. Late Pleistocene-Holocene paleoceanography and ventilation of the Gulf of California [J]. Journal of Oceanography, 2002, 58(2): 421-432. doi: 10.1023/A:1015830313175
[71]	Ohkushi K, Itaki T, Nemoto N. Last Glacial-Holocene change in intermediate-water ventilation in the Northwestern Pacific [J]. Quaternary Science Reviews, 2003, 22(14): 1477-1484. doi: 10.1016/S0277-3791(03)00082-9
[72]	Max L, Rippert N, Lembke-Jene L, et al. Evidence for enhanced convection of North Pacific Intermediate Water to the low-latitude Pacific under glacial conditions [J]. Paleoceanography, 2017, 32(1): 41-55. doi: 10.1002/2016PA002994
[73]	Jang K, Huh Y, Han Y. Authigenic Nd isotope record of North Pacific Intermediate Water formation and boundary exchange on the Bering Slope [J]. Quaternary Science Reviews, 2017, 156: 150-163. doi: 10.1016/j.quascirev.2016.11.032
[74]	Knudson K P, Ravelo A C. North Pacific intermediate water circulation enhanced by the closure of the Bering Strait [J]. Paleoceanography, 2015, 30(10): 1287-1304. doi: 10.1002/2015PA002840
[75]	Lisiecki L E, Raymo M E. A Pliocene-Pleistocene stack of 57 globally distributed benthic δ¹⁸O records [J]. Paleoceanography, 2005, 20(1): PA1003. doi: 10.1029/2004PA001071
[76]	Bereiter B, Lüthi D, Siegrist M, et al. Mode change of millennial CO₂ variability during the last glacial cycle associated with a bipolar marine carbon seesaw [J]. Proceedings of the National Academy of Sciences of the United States of America, 2012, 109(25): 9755-9760. doi: 10.1073/pnas.1204069109
[77]	Rohling E J, Grant K, Bolshaw M, et al. Antarctic temperature and global sea level closely coupled over the past five glacial cycles [J]. Nature Geoscience, 2009, 2(7): 500-504. doi: 10.1038/ngeo557
[78]	Sosdian S, Rosenthal Y. Deep-sea temperature and ice volume changes across the Pliocene-Pleistocene climate transitions [J]. Science, 2009, 325(5938): 306-310. doi: 10.1126/science.1169938
[79]	Horikawa K, Kozaka Y, Okazaki Y, et al. Neodymium isotope records from the Northwestern Pacific: Implication for deepwater ventilation at Heinrich Stadial 1 [J]. Paleoceanography and Paleoclimatology, 2021, 36(10): e2021PA004312. doi: 10.1029/2021PA004312
[80]	Okazaki Y, Timmermann A, Menviel L, et al. Deepwater formation in the North Pacific during the Last Glacial termination [J]. Science, 2010, 329(5988): 200-204. doi: 10.1126/science.1190612
[81]	Kim S, Khim B K, Ikehara K, et al. Millennial-scale changes of surface and bottom water conditions in the northwestern Pacific during the last deglaciation [J]. Global and Planetary Change, 2017, 154: 33-43. doi: 10.1016/j.gloplacha.2017.04.009
[82]	Detlef H, Sosdian S M, Belt S T, et al. Late quaternary sea-ice and sedimentary redox conditions in the eastern Bering Sea-implications for ventilation of the mid-depth North Pacific and an Atlantic-Pacific seesaw mechanism [J]. Quaternary Science Reviews, 2020, 248: 106549. doi: 10.1016/j.quascirev.2020.106549
[83]	Rae J W B, Sarnthein M, Foster G L, et al. Deep water formation in the North Pacific and deglacial CO₂ rise [J]. Paleoceanography, 2014, 29(6): 645-667. doi: 10.1002/2013PA002570
[84]	Du J H, Haley B A, Mix A C, et al. Flushing of the deep Pacific Ocean and the deglacial rise of atmospheric CO₂ concentrations [J]. Nature Geoscience, 2018, 11(10): 749-755. doi: 10.1038/s41561-018-0205-6
[85]	Max L, Lembke-Jene L, Riethdorf J R, et al. Pulses of enhanced North Pacific Intermediate Water ventilation from the Okhotsk Sea and Bering Sea during the last deglaciation [J]. Climate of the Past, 2014, 10(2): 591-605. doi: 10.5194/cp-10-591-2014
[86]	Jaccard S L, Galbraith E D. Direct ventilation of the North Pacific did not reach the deep ocean during the last deglaciation [J]. Geophysical Research Letters, 2013, 40(1): 199-203. doi: 10.1029/2012GL054118
[87]	Ohkushi K, Hara N, Ikehara M, et al. Intensification of North Pacific intermediate water ventilation during the Younger Dryas [J]. Geo-Marine Letters, 2016, 36(5): 353-360. doi: 10.1007/s00367-016-0450-x
[88]	Gong X, Lembke-Jene L, Lohmann G, et al. Enhanced North Pacific deep-ocean stratification by stronger intermediate water formation during Heinrich Stadial 1 [J]. Nature Communications, 2019, 10(1): 656. doi: 10.1038/s41467-019-08606-2
[89]	Talley L D. Closure of the global overturning circulation through the Indian, Pacific, and Southern Oceans: Schematics and transports [J]. Oceanography, 2013, 26(1): 80-97. doi: 10.5670/oceanog.2013.07
[90]	Houghton R A. Balancing the global carbon budget [J]. Annual Review of Earth and Planetary Sciences, 2007, 35: 313-347. doi: 10.1146/annurev.earth.35.031306.140057
[91]	Zeebe R E. History of seawater carbonate chemistry, atmospheric CO₂, and ocean acidification [J]. Annual Review of Earth and Planetary Sciences, 2012, 40: 141-165. doi: 10.1146/annurev-earth-042711-105521
[92]	Jacobel A W, Anderson R F, Jaccard S L, et al. Deep Pacific storage of respired carbon during the last ice age: perspectives from bottom water oxygen reconstructions [J]. Quaternary Science Reviews, 2020, 230: 106065. doi: 10.1016/j.quascirev.2019.106065
[93]	Jaccard S L, Galbraith E D, Sigman D M, et al. Subarctic Pacific evidence for a glacial deepening of the oceanic respired carbon pool [J]. Earth and Planetary Science Letters, 2009, 277(1-2): 156-165. doi: 10.1016/j.jpgl.2008.10.017
[94]	Hu R, Piotrowski A M. Neodymium isotope evidence for glacial-interglacial variability of deepwater transit time in the Pacific Ocean [J]. Nature Communications, 2018, 9(1): 4709. doi: 10.1038/s41467-018-07079-z
[95]	Wan S, Jian Z M, Gong X, et al. Deep water[CO₃²⁻] and circulation in the south China sea over the last glacial cycle [J]. Quaternary Science Reviews, 2020, 243: 106499. doi: 10.1016/j.quascirev.2020.106499
[96]	de la Fuente M, Skinner L, Calvo E, et al. Increased reservoir ages and poorly ventilated deep waters inferred in the glacial Eastern Equatorial Pacific [J]. Nature Communications, 2015, 6: 7420. doi: 10.1038/ncomms8420
[97]	Skinner L C, Primeau F, Freeman E, et al. Radiocarbon constraints on the glacial ocean circulation and its impact on atmospheric CO₂ [J]. Nature Communications, 2017, 8: 16010. doi: 10.1038/ncomms16010
[98]	Yu J M, Anderson R F, Jin Z D, et al. Responses of the deep ocean carbonate system to carbon reorganization during the Last Glacial-interglacial cycle [J]. Quaternary Science Reviews, 2013, 76: 39-52. doi: 10.1016/j.quascirev.2013.06.020
[99]	Jaccard S L, Galbraith E D. Large climate-driven changes of oceanic oxygen concentrations during the last deglaciation [J]. Nature Geoscience, 2012, 5(2): 151-156. doi: 10.1038/ngeo1352
[100]	Lund D C. Deep Pacific ventilation ages during the last deglaciation: Evaluating the influence of diffusive mixing and source region reservoir age [J]. Earth and Planetary Science Letters, 2013, 381: 52-62. doi: 10.1016/j.jpgl.2013.08.032
[101]	Lund D C, Mix A C, Southon J. Increased ventilation age of the deep northeast Pacific Ocean during the last deglaciation [J]. Nature Geoscience, 2011, 4(11): 771-774. doi: 10.1038/ngeo1272
[102]	Janecek T R, Rea D K. Eolian deposition in the northeast Pacific Ocean: Cenozoic history of atmospheric circulation [J]. Geological Society of America Bulletin, 1983, 94(6): 730-738. doi: 10.1130/0016-7606(1983)94<730:EDITNP>2.0.CO;2
[103]	Janecek T R. Eolian sedimentation in the northwest Pacific Ocean: A preliminary examination of the data from Deep Sea Drilling Project sites 576 and 578[R]. Initial Reports, DSDP, 86, 1985: 589-603. doi: 10.2973/dsdp.proc.86.126.1985.
[104]	Anderson C H, Murray R W, Dunlea A G, et al. Aeolian delivery to Ulleung Basin, Korea (Japan Sea), during development of the East Asian Monsoon through the last 12 Ma [J]. Geological Magazine, 2020, 157(5): 806-817. doi: 10.1017/S001675681900013X
[105]	Zhang W F, Chen J, Ji J F, et al. Evolving flux of Asian dust in the North Pacific Ocean since the late Oligocene [J]. Aeolian Research, 2016, 23: 11-20. doi: 10.1016/j.aeolia.2016.09.004
[106]	Rea D K, Snoeckx H, Joseph L H. Late Cenozoic Eolian deposition in the North Pacific: Asian drying, Tibetan uplift, and cooling of the northern hemisphere [J]. Paleoceanography, 1998, 13(3): 215-224. doi: 10.1029/98PA00123
[107]	Jiang X D, Zhao X, Zhao X Y, et al. Abyssal manganese nodule recording of global cooling and Tibetan Plateau uplift impacts on Asian aridification [J]. Geophysical Research Letters, 2022, 49(3): e2021GL096624. doi: 10.1029/2021GL096624
[108]	Zhang Q, Liu Q S, Roberts A P, et al. Mechanism for enhanced eolian dust flux recorded in North Pacific Ocean sediments since 4.0 Ma: aridity or humidity at dust source areas in the Asian interior? [J]. Geology, 2020, 48(1): 77-81. doi: 10.1130/G46862.1
[109]	Shi Z G, Liu X D, An Z S, et al. Simulated variations of eolian dust from inner Asian deserts at the mid-Pliocene, last glacial maximum, and present day: contributions from the regional tectonic uplift and global climate change [J]. Climate Dynamics, 2011, 37(11-12): 2289-2301. doi: 10.1007/s00382-011-1078-1
[110]	Abell J T, Winckler G, Anderson R F, et al. Poleward and weakened westerlies during Pliocene warmth [J]. Nature, 2021, 589(7840): 70-75. doi: 10.1038/s41586-020-03062-1
[111]	Serno S, Winckler G, Anderson R F, et al. Change in dust seasonality as the primary driver for orbital-scale dust storm variability in East Asia [J]. Geophysical Research Letters, 2017, 44(8): 3796-3805. doi: 10.1002/2016GL072345
[112]	Zhang W F, Li G J, Chen J. The application of Neodymium isotope as a chronostratigraphic tool in North Pacific sediments [J]. Geological Magazine, 2020, 157(5): 768-776. doi: 10.1017/S001675681900089X
[113]	McGee D, Broecker W S, Winckler G. Gustiness: the driver of glacial dustiness? [J]. Quaternary Science Reviews, 2010, 29(17-18): 2340-2350. doi: 10.1016/j.quascirev.2010.06.009
[114]	Nagashima K, Tada R, Tani A, et al. Millennial-scale oscillations of the westerly jet path during the last glacial period [J]. Journal of Asian Earth Sciences, 2011, 40(6): 1214-1220. doi: 10.1016/j.jseaes.2010.08.010
[115]	Luetscher M, Boch R, Sodemann H, et al. North Atlantic storm track changes during the Last Glacial Maximum recorded by Alpine speleothems [J]. Nature Communications, 2015, 6: 6344. doi: 10.1038/ncomms7344
[116]	Vandenberghe J, Renssen H, van Huissteden K, et al. Penetration of Atlantic westerly winds into Central and East Asia [J]. Quaternary Science Reviews, 2006, 25(17-18): 2380-2389. doi: 10.1016/j.quascirev.2006.02.017
[117]	Broecker W S. Glacial to interglacial changes in ocean chemistry [J]. Progress in Oceanography, 1982, 11(2): 151-197. doi: 10.1016/0079-6611(82)90007-6
[118]	Broecker W S. Ocean chemistry during glacial time [J]. Geochimica et Cosmochimica Acta, 1982, 46(10): 1689-1705. doi: 10.1016/0016-7037(82)90110-7
[119]	Harada N, Sato M, Shiraishi A, et al. Characteristics of alkenone distributions in suspended and sinking particles in the northwestern North Pacific [J]. Geochimica et Cosmochimica Acta, 2006, 70(8): 2045-2062. doi: 10.1016/j.gca.2006.01.024
[120]	Takahashi T, Sutherland S C, Wanninkhof R, et al. Climatological mean and decadal change in surface ocean pCO₂, and net sea-air CO₂ flux over the global oceans [J]. Deep Sea Research Part Ⅱ:Topical Studies in Oceanography, 2009, 56(8-10): 554-577. doi: 10.1016/j.dsr2.2008.12.009
[121]	Rae J W B, Gray W R, Wills R C J, et al. Overturning circulation, nutrient limitation, and warming in the Glacial North Pacific [J]. Science Advances, 2020, 6(50): eabd1654. doi: 10.1126/sciadv.abd1654
[122]	Haug G H, Sigman D M, Tiedemann R, et al. Onset of permanent stratification in the subarctic Pacific Ocean [J]. Nature, 1999, 401(6755): 779-782. doi: 10.1038/44550
[123]	Snoeckx H D, Rea D K, Jones C E, et al. Aeolian and silica deposition in the central North Pacific: Results from sites 885/886 [R]. Scientific Results, ODP, 145, 1995: 219-230, doi: 10.2973/odp.proc.sr.145.123.1995.
[124]	Iwasaki S, Takahashi K, Kanematsu Y, et al. Paleoproductivity and paleoceanography of the last 4.3 Myrs at IODP Expedition 323 Site U1341 in the Bering Sea based on biogenic opal content [J]. Deep Sea Research Part Ⅱ:Tropical Studies in Oceanography, 2016, 125-126: 145-154. doi: 10.1016/j.dsr2.2015.04.005
[125]	Stroynowski Z, Ravelo A C, Andreasen D. A Pliocene to recent history of the Bering Sea at Site U1340A, IODP Expedition 323 [J]. Paleoceanography, 2015, 30(12): 1641-1656. doi: 10.1002/2015PA002866
[126]	Jaccard S L, Galbraith E D, Sigman D M, et al. A pervasive link between Antarctic ice core and subarctic Pacific sediment records over the past 800 kyrs [J]. Quaternary Science Reviews, 2010, 29(1-2): 206-212. doi: 10.1016/j.quascirev.2009.10.007
[127]	Knudson K P, Ravelo A C. Enhanced subarctic Pacific stratification and nutrient utilization during glacials over the last 1.2Myr [J]. Geophysical Research Letters, 2015, 42(22): 9870-9879. doi: 10.1002/2015GL066317
[128]	Maeda L, Kawahata H, Nohara M. Fluctuation of biogenic and abiogenic sedimentation on the Shatsky Rise in the western north Pacific during the late Quaternary [J]. Marine Geology, 2002, 189(3-4): 197-214. doi: 10.1016/S0025-3227(02)00405-X
[129]	Amo M, Minagawa M. Sedimentary record of marine and terrigenous organic matter delivery to the Shatsky Rise, western North Pacific, over the last 130 kyr [J]. Organic Geochemistry, 2003, 34(9): 1299-1312. doi: 10.1016/S0146-6380(03)00113-X
[130]	Burgay F, Spolaor A, Gabrieli J, et al. Atmospheric iron supply and marine productivity in the glacial North Pacific Ocean [J]. Climate of the Past, 2021, 17(1): 491-505. doi: 10.5194/cp-17-491-2021
[131]	Moore C M, Mills M M, Arrigo K R, et al. Processes and patterns of oceanic nutrient limitation [J]. Nature Geoscience, 2013, 6(9): 701-710. doi: 10.1038/ngeo1765
[132]	Knudson K P, Ravelo A C, Aiello I W, et al. Causes and timing of recurring subarctic Pacific hypoxia [J]. Science Advances, 2021, 7(23): eabg2906. doi: 10.1126/sciadv.abg2906
[133]	Han Y X, Zhao T L, Song L C, et al. A linkage between Asian dust, dissolved iron and marine export production in the deep ocean [J]. Atmospheric Environment, 2011, 45(25): 4291-4298. doi: 10.1016/j.atmosenv.2011.04.078
[134]	Müller J, Romero O, Cowan E A, et al. Cordilleran ice-sheet growth fueled primary productivity in the Gulf of Alaska, northeast Pacific Ocean [J]. Geology, 2018, 46(4): 307-310. doi: 10.1130/g39904.1
[135]	Kim S, Takahashi K, Khim B K, et al. Biogenic opal production changes during the Mid-Pleistocene Transition in the Bering Sea (IODP Expedition 323 Site U1343) [J]. Quaternary Research, 2014, 81(1): 151-157. doi: 10.1016/j.yqres.2013.10.001
[136]	Jaccard S L, Hayes C T, Martínez-García 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
[137]	Weber M E, Bailey I, Hemming S R, et al. Antiphased dust deposition and productivity in the Antarctic Zone over 1.5 million years [J]. Nature Communications, 2022, 13(1): 2044. doi: 10.1038/s41467-022-29642-5
[138]	Koffman B G, Yoder M F, Methven T, et al. Glacial dust surpasses both volcanic ash and desert dust in its iron fertilization potential [J]. Global Biogeochemical Cycles, 2021, 35(4): e2020GB006821. doi: 10.1029/2020GB006821
[139]	Walczak M H, Mix A C, Cowan E A, et al. Phasing of millennial-scale climate variability in the Pacific and Atlantic Oceans [J]. Science, 2020, 370(6517): 716-720. doi: 10.1126/science.aba7096

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北太平洋大洋钻探研究进展

作者简介: 张亚南（1994—），男，博士，主要从事古海洋沉积方面的研究工作，E-mail：yananzhang9@163.com

通讯作者: 刘青松（1972—），男，教授，博士生导师，主要从事海洋磁学方面的研究，E-mail：qsliu@sustech.edu.cn

Research progress of ocean drilling in the North Pacific Ocean: Paleoceanography and paleoclimate

Corresponding author: LIU Qingsong, qsliu@sustech.edu.cn

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