末次冰期以来北太平洋中层水演化:研究进展与展望
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摘要
北太平洋中层水(NPIW)作为全球海洋经向翻转环流的一个重要组成部分,在区域海洋环境和全球气候变化中扮演着重要角色。本研究对NPIW演化及其对气候变化的影响最新进展进行了评述。认为NPIW形成及通风演化对全球气候变化响应十分敏感。而且高纬气候信号通过这一"海洋通道"传递到北太平洋低纬海域。另一方面,东亚夏季风通过影响黑龙江进入鄂霍次克海的径流量,从而对NPIW的形成和水团组成产生影响。在千年尺度,NPIW通风过程与大西洋经向翻转流(AMOC)呈反相位变化,这与AMOC千年尺度震荡所引发的北太洋海表温、盐变化相关。与NPIW相关的物理过程和生物过程可能是触发冰期大气CO_2浓度变化的一个重要机制。
North Pacific Intermediate Water(NPIW),one of the key components of global meridional overturning circulation,plays an important role in regulating regional oceanic environment and global climate change.In this study,we review the state-of-the-art of NPIW evolution and its effect on climate change.We suggest that the NPIW is very sensitive to the response of global climate change.Moreover,climatic signal in high-latitude can be propagated to the low-latitude in the North Pacific through NPIW via the "oceanic tunnel".On the other hand,East Asian Summer Monsoon can also exert influence on the formation and composition of NPIW through affecting the precipitation in the drainage basin and subsequent runoff of the Amur River to the Okhotsk Sea.On millennial time scales,the ventilation seesaw occurs between the NPIW and the Atlantic Meridional Overturning Circulation(AMOC),which is associated with the variations,induced by AMOC,in sea surface temperature and salinity.Both physical and biological processes related to the changes in the NPIW could have contributed to the fluctuations of atmospheric concentrations of CO_2 over glacial cycles.
North Pacific Intermediate Water(NPIW),one of the key components of global meridional overturning circulation,plays an important role in regulating regional oceanic environment and global climate change.In this study,we review the state-of-the-art of NPIW evolution and its effect on climate change.We suggest that the NPIW is very sensitive to the response of global climate change.Moreover,climatic signal in high-latitude can be propagated to the low-latitude in the North Pacific through NPIW via the "oceanic tunnel".On the other hand,East Asian Summer Monsoon can also exert influence on the formation and composition of NPIW through affecting the precipitation in the drainage basin and subsequent runoff of the Amur River to the Okhotsk Sea.On millennial time scales,the ventilation seesaw occurs between the NPIW and the Atlantic Meridional Overturning Circulation(AMOC),which is associated with the variations,induced by AMOC,in sea surface temperature and salinity.Both physical and biological processes related to the changes in the NPIW could have contributed to the fluctuations of atmospheric concentrations of CO_2 over glacial cycles.
引文
[1]WARREN B A.Why is no deep water formed in the North Pacific?[J].Journal of Marine Research,1983,41(2):327-347.
[2]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):327-347.
[3]BROECKER W S,PENG T H,JOUZEL J,et al.The magnitude of global fresh-water transports of importance to ocean circulation[J].Climate Dynamics,1990,4(2):73-79.
[4]TALLEY L D.Distribution and formation of North Pacific Intermediate Water[J].Journal of Physical Oceanography,1993,23(3):517-537.
[5]YOU Y,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.
[6]SHIMIZU Y,IWAO T,YASUDA I,et al.Formation process of North Pacific Intermediate Water Revealed by profiling floats set to drift on 26.7σθisopycnal surface[J].Journal of Oceanography,2004,60(2):453-462.
[7]SARMIENTO J L,GRUBER N,BRZEZINSKI M A,et al.High-latitude controls of thermocline nutrients and low latitude biological productivity[J].Nature,2004,427(6969):56-60.
[8]HARRISON P J,WHITNEY F A,TSUDA A,et al.Nutrient and plankton dynamics in the NE and NW Gyres of the Subarctic Pacific Ocean[J].Journal of Oceanography,2004,60(1):93-117.
[9]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.
[10]ITOU M,ONO T,NORIKI S.Provenance of intermediate waters in the western North Pacific deduced from thermodynamicimprint onδ13 C of DIC[J].Journal of Geophysical Research:Oceans,2003,108(C11):3347.DOI:10.1029/2002JC001746.
[11]YOU Y.The pathway and circulation of North Pacific Intermediate Water[J].Geophysical Research Letters,2003,30(24):2291.DOI:10.1029/2003GL018561.
[12]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.
[13]LIU Z,ALEXANDER M.Atmospheric bridge,oceanic tunnel,and global climatic teleconnections[J].Reviews of Geophysics,2007,45(2):RG2005.DOI:10.1029/2005RG000172.
[14]ZHENG Y,VAN GEEN A,ANDERSON R F,et al.Intensification of the Northeast Pacific oxygen minimum zone during the B?lling-Aller?d Warm Period[J].Paleoceanography,2000,15(5):528-536.
[15]DAI M,CAO Z,GUO X,et al.Why are some marginal seas sources of atmospheric CO2?[J].Geophysical Research Letters,2013,40(10):2154-2158.
[16]BINGHAM F M,LUKAS R.The distribution of intermediate water in the western equatorial Pacific during JanuaryFebruary 1986[J].Deep Sea Research Part I:Oceanographic Research Papers,1995,42(9):1545-1573.
[17]LYNCH-STIEGLITZ J,MARCHITTO T M.Tracers of past ocean circulation[M]∥HOLLAND H D,TUREKIAN K K.Treatise on geochemistry.2nd ed.Oxford:Academic Press,2014:435-451.
[18]RAHMSTORF S,FEULNER G.Paleoclimatic ocean circulation and sea-level changes[M]∥SLENDER G,GRIFFIES S M,GOULD J,et al.Ocean circulation and climate:a 21century perspective.2nd ed.Oxford:Academic Press,2013:31-56.
[19]MCCAVE I N,MANIGHETTI B,ROBINSON S G.Sortable silt and fine sediment size/composition slicing:parameters for palaeocurrent speed and palaeoceanography[J].Paleoceanography,1995,10(3):593-610.
[20]YU E F,FRANCOIS R,BACON M P.Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data[J].Nature,1996,379(6567):689-694.
[21]RUTBERG R L,HEMMING S R,GOLDSTEIN S L.Reduced North Atlantic Deep Water flux to the glacial southern ocean inferred from neodymium isotope ratios[J].Nature,2000,405(6789):935-938.
[22]CARTAPANIS O,TACHIKAWA K,BARD E.Latitudinal variations in intermediate depth ventilation and biological production over northeastern Pacific Oxygen Minimum Zones during the last 60ka[J].Quaternary Science Reviews,2012,53:24-38.
[23]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.
[24]SHIBAHARA A,OHKUSHI K,KENNETT J P,et al.Late Quaternary changes in intermediate water oxygenation and oxygen minimum zone,northern Japan:a benthic foraminiferal perspective[J].Paleoceanography,2007,22(3):PA3213.DOI:10.1029/2005PA001234.
[25]HAYES C T,ANDERSON R F,JACCARD S L,et al.A new perspective on boundary scavenging in the North Pacific Ocean[J].Earth and Planetary Science Letters,2013,369/370:86-97.
[26]HAYES C T,ANDERSON R F,FLEISHER M Q,et al.Biogeography in 231Pa/230 Th ratios and a balanced 231Pa budget for the Pacific Ocean[J].Earth and Planetary Science Letters,2014,391:307-318.
[27]FRANK M.Radiogenic isotopes:tracers of past ocean circulation and erosional input[J].Reviews of Geophysics,2002,40(1):RG2002.DOI:10.1029/2000RG000094.
[28]GUTJAHR M,FRANK M,STIRLING C H,et al.Tracing the Nd isotope evolution of North Atlantic Deep and Intermediate Waters in the western North Atlantic since the Last Glacial Maximum from Blake Ridge sediments[J].Earth and Planetary Science Letters,2008,266(1/2):61-77.
[29]CHEN T Y,FRANK M,HALEY B A,et al.Variations of North Atlantic inflow to the central Arctic Ocean over the last 14million years inferred from hafnium and neodymium isotopes[J].Earth and Planetary Science Letters,2012,353:82-92.
[30]HORIKAWA K,ASAHARA Y,YAMAMOTO K,et al.Intermediate water formation in the Bering Sea during glacial periods:evidence from neodymium isotope ratios[J].Geology,2010,38(5):435-438.
[31]HALEY B A,FRANK M,SPIELHAGEN R F,et al.Radiogenic isotope record of Arctic Ocean circulation and weathering inputs of the past 15 million years[J].Paleoceanography,2008,23(1).PAIS13.DOI:10.1029/2007PA001486.
[32]XIE R C,MARCANTONIO F,SCHMIDT M W.Deglacial variability of Antarctic Intermediate Water penetration into the North Atlantic from authigenic neodymium isotope ratios[J].Paleoceanography,2012,27(3).PA322.DOI:10.1029/2012PA002337.
[33]YOU Y.Frontal densification and displacement:a scenario of North Pacific Intermediate Water formation[J].Deep Sea Research Part II:Topical Studies in Oceanography,2010,57(13/14):1171-1176.
[34]AMAKAWA H,NOZAKI Y,ALIBO D S,et al.Neodymium isotopic variations in Northwest Pacific waters[J].Geochimica et Cosmochimica Acta,2004,68(4):715-727.
[35]RELLA S F,TADA R,NAGASHIMA K,et al.Abrupt changes of intermediate water properties on the northeastern slope of the Bering Sea during the last glacial and deglacial period[J].Paleoceanography,2012,27:PA3203.DOI:10.1029/2011PA002205.
[36]LEMBKE-JENE L,TIEDEMANN R,NURNBERG D,et al.Deglacial variability in Okhotsk Sea Intermediate Water ventilation and biogeochemistry:implications for North Pacific nutrient supply and productivity[J].Quaternary Science Reviews,2017,160:116-137.
[37]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.
[38]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.
[39]KEIGWIN L D.Glacial-age hydrography of the far northwest Pacific Ocean[J].Paleoceanography,1998,13(4):323-339.
[40]KEIGWIN L D.Late Pleistocene-Holocene paleoceanography and ventilation of the Gulf of California[J].Journal of Oceanography,2002,58(2):421-432.
[41]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.
[42]RAE J W B,SARNTHEIN M,FOSTER G L,et al.Deep water formation in the North Pacific and deglacial CO2rise[J].Paleoceanography,2014,29(6):645-667.
[43]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.
[44]CANNARIATO K G,KENNETT J P.Climatically related millennial-scale fluctuations in strength of California margin oxygen-minimum zone during the past 60ka[J].Geology,1999,27(11):975-978.
[45]NAMEROFF T J,CALVERT S E,MURRAY J W.Glacialinterglacial variability in the eastern tropical North Pacific oxygen minimum zone recorded by redox-sensitive trace metals[J].Paleoceanography,2004,19(1):PA1010.DOI:10.1029/2003pa000912.
[46]CHENG H,EDWARDS R L,SINHA A,et al.The Asian monsoon over the past 640000years and ice age terminations[J].Nature,2016,534(7609):640-646.
[47]MCMANUS J F,FRANCOIS R,GHERARDI J M,et al.Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes[J].Nature,2004,428(6985):834-837.
[48]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.
[49]KAO S J,LIU K K,HSU S C,et al.North Pacific-wide spreading of isotopically heavy nitrogen during the last deglaciation:evidence from the western Pacific[J].Biogeosciences,2008,5(6):1641-1650.
[50]WAHYUDI,MINAGAWA M.Response of Benthic Foraminifera to organic carbon accumulation rates in the Okinawa Trough[J].Journal of Oceanography,1997,53:411-420.
[51]ZHENG X,KAO S,CHEN Z,et al.Deepwater circulation variation in the South China Sea since the Last Glacial Maximum[J].Geophysical Research Letters,2016,43(16):8590-8599.
[52]WEI G J,HUANG C Y,WANG C C,et al.High-resolution benthic foraminiferδ13C records in the South China Sea during the last 150ka[J].Marine Geology,2006,232(3/4):227-235.
[53]SHI X,WU Y,ZOU J,et al.Multiproxy reconstruction for Kuroshio responses to northern hemispheric oceanic climate and the Asian Monsoon since Marine Isotope Stage 5.1(~88ka)[J].Climate of the Past,2014,10(5):1735-1750.
[54]WAN S,JIAN Z.Deep water exchanges between the South China Sea and the Pacific since the last glacial period[J].Paleoceanography,2014,29(12):1162-1178.
[55]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.
[56]LEDUC G,VIDAL L,TACHIKAWA K,et al.Changes in Eastern Pacific ocean ventilation at intermediate depth over the last 150kyr BP[J].Earth and Planetary Science Letters,2010,298(1/2):217-228.
[57]NOBLE T L,PIOTROWSKI A M,MCCAVE I N.Neodymium isotopic composition of intermediate and deep waters in the glacial southwest Pacific[J].Earth and Planetary Science Letters,2013,384:27-36.
[58]石学法,邹建军,王昆山.鄂霍次克海晚第四纪以来古环境演化[J].海洋地质与第四纪地质,2011,31(6):1-12.
[59]GORBARENKO S A,BASOV I A,CHEKHOVSKAYA M P,et al.Orbital and millennium scale environmental changes in the southern Bering Sea during the last glacial-Holocene:geochemical and paleontological evidence[J].Deep-Sea Research PartⅡ:Topical Studies in Oceanography,2005,52(16/17/18):2174-2185.
[60]KATSUKI K,TAKAHASHI K.Diatoms as paleoenvironmental proxies for seasonal productivity,sea-ice and surface circulation in the Bering Sea during the late Quaternary[J].Deep-Sea Research PartⅡ:Topical Studies in Oceanography,2005,52(16/17/18):2110-2130.
[61]SAKAMOTO T,IKEHARA M,AOKI K,et al.Ice-rafted debris(IRD)-based sea-ice expansion events during the past100kyrs in the Okhotsk Sea[J].Deep-Sea Research PartⅡ:Topical Studies in Oceanography,2005,52(16/17/18):2275-2301.
[62]SEKI O,SAKAMOTO T,SAKAI S,et al.Large changes in seasonal sea ice distribution and productivity in the Sea of Okhotsk during the deglaciations[J].Geochemistry,Geophysics,Geosystems,2009,10:Q10007.DOI:10010.11029/12009GC002613.
[63]TERNOIS Y,KAWAMURA K,KEIGWIN L,et al.A biomarker approach for assessing marine and terrigenous inputs to the sediments of Sea of Okhotsk for the last 27000years[J].Geochimica et Cosmochimica Acta,2001,65(5):791-802.
[64]MATUL A,ABELMANN A,TIEDEMANN R,et al.Late Quaternary polycystine radiolarian datum events in the Sea of Okhotsk[J].Geo-Marine Letters,2002,22(1):25-32.
[65]NUERNBERG D,TIEDEMANN R.Environmental change in the Sea of Okhotsk during the last 1.1 million years[J].Paleoceanography,2004,19(4):PA4011.DOI:4010.1029/2004PA001023.
[66]孙烨忱,王汝建,陈建芳,等.鄂霍次克海南部晚第四纪的古海洋学记录[J].海洋地质与第四纪地质,2009,29(2):83-90.
[67]ITAKI T,IKEHARA K.Middle to late Holocene changes of the Okhotsk Sea Intermediate Water and their relation to atmospheric circulation[J].Geophysical Research Letters,2004,31(24):L24309.DOI:24310.21029/22004GL021384.
[68]OKAZAKI Y,TAKAHASHI K,KATSUKI K,et al.Late Quaternary paleoceanographic changes in the southwestern Okhotsk Sea:evidence from geochemical,radiolarian,and diatom records[J].Deep-Sea Research PartⅡ:Topical Studies in Oceanography,2005,52(16/17/18):2332-2350.
[69]KATSUKI K,KHIM B K,ITAKI T,et al.Sea-ice distribution and atmospheric pressure patterns in southwestern Okhotsk Sea since the Last Glacial Maximum[J].Global and Planetary Change,2010,72(3):99-107.
[70]DUPLESSY J C,ARNOLD M,BARD E,et al.AMS 14C study of transient events and of the ventilation rate of the Pacific intermediate water during the last deglaciation[J].Radiocarbon,1989,31(3):493-502.
[71]AHAGON N,OHKUSHI K,UCHIDA M,et al.Mid-depth circulation in the northwest Pacific during the last deglaciation:evidence from foraminiferal radiocarbon ages[J].Geophysical Research Letters,2003,30(21):2097.DOI:10.1029/2003GL018287.
[72]AHAGON N,Uchida M.Transient response of mid-depth circulation in the northwest Pacific around the Younger Dryas event inferred from AMS 14C ages of foraminifera[J].Nuclear Instruments and Methods in Physics Research Section B:Beam Interactions with Materials and Atoms,2004,223:466-470.
[73]RELLA S F,UCHIDA M.A southern ocean trigger for Northwest Pacific ventilation during the Holocene?[J].Scientific Reports,2014,4:4046.DOI:10.1038/srep04046.
[74]HU A X,MEEHL G A,OTTO-BLIESNER B L,et al.Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes[J].Nature Geoscience,2010,3(2):118-121.
[75]North Greenland Ice Core Project Members.High-resolution record of Northern Hemisphere climate extending into the last interglacial period[J].Nature,2004,431(7005):147-151.
[76]TAKAHASHI K.The Bering Sea and paleoceanography[J].Deep-Sea Research PartⅡ:Topical Studies in Oceanography,2005,52(16/17/18):2080-2091.
[77]NAKATSUKA T,WATANABE K,HANDA N,et al.Glacial to interglacial surface nutrient variations of Bering deep basins recorded byδ13C andδ15 N of sedimentary organicmatter[J].Paleoceanography,1995,10(6):1047-1061.
[78]邹建军,石学法,白亚之,等.末次冰消期以来白令海古环境及古生产力演化[J].地球科学:中国地质大学学报,2012,37(增刊1):1-10.
[79]OKAZAKI Y,TAKAHASHI K,ASAHI H,et al.Productivity changes in the Bering Sea during the late Quaternary[J].Deep Sea Research Part II:Topical Studies in Oceanography,2005,52(16/17/18):2150-2162.
[80]COOK M S,KEIGWIN L D,SANCETTA C A.The deglacial history of surface and intermediate water of the Bering Sea[J].Deep-Sea Research PartⅡ:Topical Studies in Oceanography,2005,52(16/17/18):2163-2173.
[81]KIM S,KHIM B K,UCHIDA M,et al.Millennial-scale paleoceanographic events and implication for the intermediatewater ventilation in the northern slope area of the Bering Sea duriing the last 71kyrs[J].Global and Planetary Change,2011,79(1/2):89-98.
[82]ITAKI T,KIM S,RELLA S F,et al.Millennial-scale variations of late Pleistocene radiolarian assemblages in the Bering Sea related to environments in shallow and deep waters[J].Deep Sea Research Part II:Topical Studies in Oceanography,2012,61/62/63/64:127-144.
[83]GORBARENKO S A,WANG P,WANG R,et al.Orbital and suborbital environmental changes in the southern Bering Sea during the last 50kyr[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2010,286(1/2):97-106.
[84]CRUSIUS J,PEDERSEN T F,KIENAST S,et al.Influence of northwest Pacific productivity on North Pacific Inter-mediate Water oxygen concentrations during the B?lling-ller?d interval(14.7-12.9ka)[J].Geology,2004,32(7):633-636.
[85]CHIKAMOTO M O,MENVIEL L,ABE-OUCHI A,et al.Variability in North Pacific intermediate and deep water ventilation during Heinrich events in two coupled climate models[J].Deep Sea Research Part II:Topical Studies in Oceanography,2012,61/62/63/64:114-126.
[86]MENVIEL L,ENGLAND M H,MEISSNER K J,et al.Atlantic-Pacific seesaw and its role in outgassing CO2 during Heinrich events[J].Paleoceanography,2014,29(1):58-70.
[87]RODRíGUEZ-SANZ L,MORTYN P G,HERGUERA J C,et al.Hydrographic changes in the tropical and extratropical Pacific during the last deglaciation[J].Paleoceanography,2013,28(3):529-538.
[88]RIETHDORF J-R,MAX L,NURNBERG D,et al.Deglacial development of(sub)sea surface temperature and salinity in the subarctic northwest Pacific:implications for upper-ocean stratification[J].Paleoceanography,2013,28(1):91-104.
[89]OKUMURA Y M,DESER C,HU A,et al.North Pacific climate response to freshwater forcing in the subarctic North Atlantic:oceanic and atmospheric pathways[J].Journal of Climate,2009,22(6):1424-1445.
[90]CAVALIERI D J,PARKINSON C L.On the relationship between atmospheric circulation and the fluctuations in the sea ice extents of the Bering and Okhotsk Seas[J].Journal of Geophysical Research:Oceans,1987,92(C7):7141-7162.
[91]SAENKO O A,SCHMITTNER A,WEAVER A J.The Atlantic-Pacific seesaw[J].Journal of Climate,2004,17(11):2033-2038.
[92]MEHEUST M,STEIN R,FAHL K,et al.High-resolution IP25-based reconstruction of sea-ice variability in the western North Pacific and Bering Sea during the past 18000years[J].Geo-Marine Letters,2016,36(2):101-111.
[93]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.
[94]NAKATSUKA T,FUJIMUNE T,YOSHIKAWA C,et al.Biogenic and lithogenic particle fluxes in the western region of the Sea of Okhotsk:implications for lateral material transport and biological productivity[J].Journal of Geophysical Research:Oceans,2004,109(C9):C09S13.DOI:10.1029/2003JC001908.
[95]NISHIOKA J,ONO T,SAITO H,et al.Iron supply to the western subarctic Pacific:importance of iron export from the Sea of Okhotsk[J].Journal of Geophysical Research:Oceans,2007,112(C10):C10012.DOI:10.1029/2006JC004055.
[96]FISCHER H,WAHLEN M,SMITH J,et al.Ice core records of atmospheric CO2around the Last Three Glacial Terminations[J].Science,1999,283(5408):1712-1714.
[97]BOSTOCK H C,OPDYKE B N,WILLIAMS M J M.Characterising the intermediate depth waters of the Pacific Ocean usingδ13C and other geochemical tracers[J].Deep Sea Research Part I:Oceanographic Research Papers,2010,57(7):847-859.
[98]PICHEVIN L E,REYNOLDS B C,GANESHRAM R S,et al.Enhanced carbon pump inferred from relaxation of nutrient limitation in the glacial ocean[J].Nature,2009,459(7250):1114-1117.
[2]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):327-347.
[3]BROECKER W S,PENG T H,JOUZEL J,et al.The magnitude of global fresh-water transports of importance to ocean circulation[J].Climate Dynamics,1990,4(2):73-79.
[4]TALLEY L D.Distribution and formation of North Pacific Intermediate Water[J].Journal of Physical Oceanography,1993,23(3):517-537.
[5]YOU Y,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.
[6]SHIMIZU Y,IWAO T,YASUDA I,et al.Formation process of North Pacific Intermediate Water Revealed by profiling floats set to drift on 26.7σθisopycnal surface[J].Journal of Oceanography,2004,60(2):453-462.
[7]SARMIENTO J L,GRUBER N,BRZEZINSKI M A,et al.High-latitude controls of thermocline nutrients and low latitude biological productivity[J].Nature,2004,427(6969):56-60.
[8]HARRISON P J,WHITNEY F A,TSUDA A,et al.Nutrient and plankton dynamics in the NE and NW Gyres of the Subarctic Pacific Ocean[J].Journal of Oceanography,2004,60(1):93-117.
[9]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.
[10]ITOU M,ONO T,NORIKI S.Provenance of intermediate waters in the western North Pacific deduced from thermodynamicimprint onδ13 C of DIC[J].Journal of Geophysical Research:Oceans,2003,108(C11):3347.DOI:10.1029/2002JC001746.
[11]YOU Y.The pathway and circulation of North Pacific Intermediate Water[J].Geophysical Research Letters,2003,30(24):2291.DOI:10.1029/2003GL018561.
[12]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.
[13]LIU Z,ALEXANDER M.Atmospheric bridge,oceanic tunnel,and global climatic teleconnections[J].Reviews of Geophysics,2007,45(2):RG2005.DOI:10.1029/2005RG000172.
[14]ZHENG Y,VAN GEEN A,ANDERSON R F,et al.Intensification of the Northeast Pacific oxygen minimum zone during the B?lling-Aller?d Warm Period[J].Paleoceanography,2000,15(5):528-536.
[15]DAI M,CAO Z,GUO X,et al.Why are some marginal seas sources of atmospheric CO2?[J].Geophysical Research Letters,2013,40(10):2154-2158.
[16]BINGHAM F M,LUKAS R.The distribution of intermediate water in the western equatorial Pacific during JanuaryFebruary 1986[J].Deep Sea Research Part I:Oceanographic Research Papers,1995,42(9):1545-1573.
[17]LYNCH-STIEGLITZ J,MARCHITTO T M.Tracers of past ocean circulation[M]∥HOLLAND H D,TUREKIAN K K.Treatise on geochemistry.2nd ed.Oxford:Academic Press,2014:435-451.
[18]RAHMSTORF S,FEULNER G.Paleoclimatic ocean circulation and sea-level changes[M]∥SLENDER G,GRIFFIES S M,GOULD J,et al.Ocean circulation and climate:a 21century perspective.2nd ed.Oxford:Academic Press,2013:31-56.
[19]MCCAVE I N,MANIGHETTI B,ROBINSON S G.Sortable silt and fine sediment size/composition slicing:parameters for palaeocurrent speed and palaeoceanography[J].Paleoceanography,1995,10(3):593-610.
[20]YU E F,FRANCOIS R,BACON M P.Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data[J].Nature,1996,379(6567):689-694.
[21]RUTBERG R L,HEMMING S R,GOLDSTEIN S L.Reduced North Atlantic Deep Water flux to the glacial southern ocean inferred from neodymium isotope ratios[J].Nature,2000,405(6789):935-938.
[22]CARTAPANIS O,TACHIKAWA K,BARD E.Latitudinal variations in intermediate depth ventilation and biological production over northeastern Pacific Oxygen Minimum Zones during the last 60ka[J].Quaternary Science Reviews,2012,53:24-38.
[23]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.
[24]SHIBAHARA A,OHKUSHI K,KENNETT J P,et al.Late Quaternary changes in intermediate water oxygenation and oxygen minimum zone,northern Japan:a benthic foraminiferal perspective[J].Paleoceanography,2007,22(3):PA3213.DOI:10.1029/2005PA001234.
[25]HAYES C T,ANDERSON R F,JACCARD S L,et al.A new perspective on boundary scavenging in the North Pacific Ocean[J].Earth and Planetary Science Letters,2013,369/370:86-97.
[26]HAYES C T,ANDERSON R F,FLEISHER M Q,et al.Biogeography in 231Pa/230 Th ratios and a balanced 231Pa budget for the Pacific Ocean[J].Earth and Planetary Science Letters,2014,391:307-318.
[27]FRANK M.Radiogenic isotopes:tracers of past ocean circulation and erosional input[J].Reviews of Geophysics,2002,40(1):RG2002.DOI:10.1029/2000RG000094.
[28]GUTJAHR M,FRANK M,STIRLING C H,et al.Tracing the Nd isotope evolution of North Atlantic Deep and Intermediate Waters in the western North Atlantic since the Last Glacial Maximum from Blake Ridge sediments[J].Earth and Planetary Science Letters,2008,266(1/2):61-77.
[29]CHEN T Y,FRANK M,HALEY B A,et al.Variations of North Atlantic inflow to the central Arctic Ocean over the last 14million years inferred from hafnium and neodymium isotopes[J].Earth and Planetary Science Letters,2012,353:82-92.
[30]HORIKAWA K,ASAHARA Y,YAMAMOTO K,et al.Intermediate water formation in the Bering Sea during glacial periods:evidence from neodymium isotope ratios[J].Geology,2010,38(5):435-438.
[31]HALEY B A,FRANK M,SPIELHAGEN R F,et al.Radiogenic isotope record of Arctic Ocean circulation and weathering inputs of the past 15 million years[J].Paleoceanography,2008,23(1).PAIS13.DOI:10.1029/2007PA001486.
[32]XIE R C,MARCANTONIO F,SCHMIDT M W.Deglacial variability of Antarctic Intermediate Water penetration into the North Atlantic from authigenic neodymium isotope ratios[J].Paleoceanography,2012,27(3).PA322.DOI:10.1029/2012PA002337.
[33]YOU Y.Frontal densification and displacement:a scenario of North Pacific Intermediate Water formation[J].Deep Sea Research Part II:Topical Studies in Oceanography,2010,57(13/14):1171-1176.
[34]AMAKAWA H,NOZAKI Y,ALIBO D S,et al.Neodymium isotopic variations in Northwest Pacific waters[J].Geochimica et Cosmochimica Acta,2004,68(4):715-727.
[35]RELLA S F,TADA R,NAGASHIMA K,et al.Abrupt changes of intermediate water properties on the northeastern slope of the Bering Sea during the last glacial and deglacial period[J].Paleoceanography,2012,27:PA3203.DOI:10.1029/2011PA002205.
[36]LEMBKE-JENE L,TIEDEMANN R,NURNBERG D,et al.Deglacial variability in Okhotsk Sea Intermediate Water ventilation and biogeochemistry:implications for North Pacific nutrient supply and productivity[J].Quaternary Science Reviews,2017,160:116-137.
[37]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.
[38]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.
[39]KEIGWIN L D.Glacial-age hydrography of the far northwest Pacific Ocean[J].Paleoceanography,1998,13(4):323-339.
[40]KEIGWIN L D.Late Pleistocene-Holocene paleoceanography and ventilation of the Gulf of California[J].Journal of Oceanography,2002,58(2):421-432.
[41]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.
[42]RAE J W B,SARNTHEIN M,FOSTER G L,et al.Deep water formation in the North Pacific and deglacial CO2rise[J].Paleoceanography,2014,29(6):645-667.
[43]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.
[44]CANNARIATO K G,KENNETT J P.Climatically related millennial-scale fluctuations in strength of California margin oxygen-minimum zone during the past 60ka[J].Geology,1999,27(11):975-978.
[45]NAMEROFF T J,CALVERT S E,MURRAY J W.Glacialinterglacial variability in the eastern tropical North Pacific oxygen minimum zone recorded by redox-sensitive trace metals[J].Paleoceanography,2004,19(1):PA1010.DOI:10.1029/2003pa000912.
[46]CHENG H,EDWARDS R L,SINHA A,et al.The Asian monsoon over the past 640000years and ice age terminations[J].Nature,2016,534(7609):640-646.
[47]MCMANUS J F,FRANCOIS R,GHERARDI J M,et al.Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes[J].Nature,2004,428(6985):834-837.
[48]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.
[49]KAO S J,LIU K K,HSU S C,et al.North Pacific-wide spreading of isotopically heavy nitrogen during the last deglaciation:evidence from the western Pacific[J].Biogeosciences,2008,5(6):1641-1650.
[50]WAHYUDI,MINAGAWA M.Response of Benthic Foraminifera to organic carbon accumulation rates in the Okinawa Trough[J].Journal of Oceanography,1997,53:411-420.
[51]ZHENG X,KAO S,CHEN Z,et al.Deepwater circulation variation in the South China Sea since the Last Glacial Maximum[J].Geophysical Research Letters,2016,43(16):8590-8599.
[52]WEI G J,HUANG C Y,WANG C C,et al.High-resolution benthic foraminiferδ13C records in the South China Sea during the last 150ka[J].Marine Geology,2006,232(3/4):227-235.
[53]SHI X,WU Y,ZOU J,et al.Multiproxy reconstruction for Kuroshio responses to northern hemispheric oceanic climate and the Asian Monsoon since Marine Isotope Stage 5.1(~88ka)[J].Climate of the Past,2014,10(5):1735-1750.
[54]WAN S,JIAN Z.Deep water exchanges between the South China Sea and the Pacific since the last glacial period[J].Paleoceanography,2014,29(12):1162-1178.
[55]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.
[56]LEDUC G,VIDAL L,TACHIKAWA K,et al.Changes in Eastern Pacific ocean ventilation at intermediate depth over the last 150kyr BP[J].Earth and Planetary Science Letters,2010,298(1/2):217-228.
[57]NOBLE T L,PIOTROWSKI A M,MCCAVE I N.Neodymium isotopic composition of intermediate and deep waters in the glacial southwest Pacific[J].Earth and Planetary Science Letters,2013,384:27-36.
[58]石学法,邹建军,王昆山.鄂霍次克海晚第四纪以来古环境演化[J].海洋地质与第四纪地质,2011,31(6):1-12.
[59]GORBARENKO S A,BASOV I A,CHEKHOVSKAYA M P,et al.Orbital and millennium scale environmental changes in the southern Bering Sea during the last glacial-Holocene:geochemical and paleontological evidence[J].Deep-Sea Research PartⅡ:Topical Studies in Oceanography,2005,52(16/17/18):2174-2185.
[60]KATSUKI K,TAKAHASHI K.Diatoms as paleoenvironmental proxies for seasonal productivity,sea-ice and surface circulation in the Bering Sea during the late Quaternary[J].Deep-Sea Research PartⅡ:Topical Studies in Oceanography,2005,52(16/17/18):2110-2130.
[61]SAKAMOTO T,IKEHARA M,AOKI K,et al.Ice-rafted debris(IRD)-based sea-ice expansion events during the past100kyrs in the Okhotsk Sea[J].Deep-Sea Research PartⅡ:Topical Studies in Oceanography,2005,52(16/17/18):2275-2301.
[62]SEKI O,SAKAMOTO T,SAKAI S,et al.Large changes in seasonal sea ice distribution and productivity in the Sea of Okhotsk during the deglaciations[J].Geochemistry,Geophysics,Geosystems,2009,10:Q10007.DOI:10010.11029/12009GC002613.
[63]TERNOIS Y,KAWAMURA K,KEIGWIN L,et al.A biomarker approach for assessing marine and terrigenous inputs to the sediments of Sea of Okhotsk for the last 27000years[J].Geochimica et Cosmochimica Acta,2001,65(5):791-802.
[64]MATUL A,ABELMANN A,TIEDEMANN R,et al.Late Quaternary polycystine radiolarian datum events in the Sea of Okhotsk[J].Geo-Marine Letters,2002,22(1):25-32.
[65]NUERNBERG D,TIEDEMANN R.Environmental change in the Sea of Okhotsk during the last 1.1 million years[J].Paleoceanography,2004,19(4):PA4011.DOI:4010.1029/2004PA001023.
[66]孙烨忱,王汝建,陈建芳,等.鄂霍次克海南部晚第四纪的古海洋学记录[J].海洋地质与第四纪地质,2009,29(2):83-90.
[67]ITAKI T,IKEHARA K.Middle to late Holocene changes of the Okhotsk Sea Intermediate Water and their relation to atmospheric circulation[J].Geophysical Research Letters,2004,31(24):L24309.DOI:24310.21029/22004GL021384.
[68]OKAZAKI Y,TAKAHASHI K,KATSUKI K,et al.Late Quaternary paleoceanographic changes in the southwestern Okhotsk Sea:evidence from geochemical,radiolarian,and diatom records[J].Deep-Sea Research PartⅡ:Topical Studies in Oceanography,2005,52(16/17/18):2332-2350.
[69]KATSUKI K,KHIM B K,ITAKI T,et al.Sea-ice distribution and atmospheric pressure patterns in southwestern Okhotsk Sea since the Last Glacial Maximum[J].Global and Planetary Change,2010,72(3):99-107.
[70]DUPLESSY J C,ARNOLD M,BARD E,et al.AMS 14C study of transient events and of the ventilation rate of the Pacific intermediate water during the last deglaciation[J].Radiocarbon,1989,31(3):493-502.
[71]AHAGON N,OHKUSHI K,UCHIDA M,et al.Mid-depth circulation in the northwest Pacific during the last deglaciation:evidence from foraminiferal radiocarbon ages[J].Geophysical Research Letters,2003,30(21):2097.DOI:10.1029/2003GL018287.
[72]AHAGON N,Uchida M.Transient response of mid-depth circulation in the northwest Pacific around the Younger Dryas event inferred from AMS 14C ages of foraminifera[J].Nuclear Instruments and Methods in Physics Research Section B:Beam Interactions with Materials and Atoms,2004,223:466-470.
[73]RELLA S F,UCHIDA M.A southern ocean trigger for Northwest Pacific ventilation during the Holocene?[J].Scientific Reports,2014,4:4046.DOI:10.1038/srep04046.
[74]HU A X,MEEHL G A,OTTO-BLIESNER B L,et al.Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes[J].Nature Geoscience,2010,3(2):118-121.
[75]North Greenland Ice Core Project Members.High-resolution record of Northern Hemisphere climate extending into the last interglacial period[J].Nature,2004,431(7005):147-151.
[76]TAKAHASHI K.The Bering Sea and paleoceanography[J].Deep-Sea Research PartⅡ:Topical Studies in Oceanography,2005,52(16/17/18):2080-2091.
[77]NAKATSUKA T,WATANABE K,HANDA N,et al.Glacial to interglacial surface nutrient variations of Bering deep basins recorded byδ13C andδ15 N of sedimentary organicmatter[J].Paleoceanography,1995,10(6):1047-1061.
[78]邹建军,石学法,白亚之,等.末次冰消期以来白令海古环境及古生产力演化[J].地球科学:中国地质大学学报,2012,37(增刊1):1-10.
[79]OKAZAKI Y,TAKAHASHI K,ASAHI H,et al.Productivity changes in the Bering Sea during the late Quaternary[J].Deep Sea Research Part II:Topical Studies in Oceanography,2005,52(16/17/18):2150-2162.
[80]COOK M S,KEIGWIN L D,SANCETTA C A.The deglacial history of surface and intermediate water of the Bering Sea[J].Deep-Sea Research PartⅡ:Topical Studies in Oceanography,2005,52(16/17/18):2163-2173.
[81]KIM S,KHIM B K,UCHIDA M,et al.Millennial-scale paleoceanographic events and implication for the intermediatewater ventilation in the northern slope area of the Bering Sea duriing the last 71kyrs[J].Global and Planetary Change,2011,79(1/2):89-98.
[82]ITAKI T,KIM S,RELLA S F,et al.Millennial-scale variations of late Pleistocene radiolarian assemblages in the Bering Sea related to environments in shallow and deep waters[J].Deep Sea Research Part II:Topical Studies in Oceanography,2012,61/62/63/64:127-144.
[83]GORBARENKO S A,WANG P,WANG R,et al.Orbital and suborbital environmental changes in the southern Bering Sea during the last 50kyr[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2010,286(1/2):97-106.
[84]CRUSIUS J,PEDERSEN T F,KIENAST S,et al.Influence of northwest Pacific productivity on North Pacific Inter-mediate Water oxygen concentrations during the B?lling-ller?d interval(14.7-12.9ka)[J].Geology,2004,32(7):633-636.
[85]CHIKAMOTO M O,MENVIEL L,ABE-OUCHI A,et al.Variability in North Pacific intermediate and deep water ventilation during Heinrich events in two coupled climate models[J].Deep Sea Research Part II:Topical Studies in Oceanography,2012,61/62/63/64:114-126.
[86]MENVIEL L,ENGLAND M H,MEISSNER K J,et al.Atlantic-Pacific seesaw and its role in outgassing CO2 during Heinrich events[J].Paleoceanography,2014,29(1):58-70.
[87]RODRíGUEZ-SANZ L,MORTYN P G,HERGUERA J C,et al.Hydrographic changes in the tropical and extratropical Pacific during the last deglaciation[J].Paleoceanography,2013,28(3):529-538.
[88]RIETHDORF J-R,MAX L,NURNBERG D,et al.Deglacial development of(sub)sea surface temperature and salinity in the subarctic northwest Pacific:implications for upper-ocean stratification[J].Paleoceanography,2013,28(1):91-104.
[89]OKUMURA Y M,DESER C,HU A,et al.North Pacific climate response to freshwater forcing in the subarctic North Atlantic:oceanic and atmospheric pathways[J].Journal of Climate,2009,22(6):1424-1445.
[90]CAVALIERI D J,PARKINSON C L.On the relationship between atmospheric circulation and the fluctuations in the sea ice extents of the Bering and Okhotsk Seas[J].Journal of Geophysical Research:Oceans,1987,92(C7):7141-7162.
[91]SAENKO O A,SCHMITTNER A,WEAVER A J.The Atlantic-Pacific seesaw[J].Journal of Climate,2004,17(11):2033-2038.
[92]MEHEUST M,STEIN R,FAHL K,et al.High-resolution IP25-based reconstruction of sea-ice variability in the western North Pacific and Bering Sea during the past 18000years[J].Geo-Marine Letters,2016,36(2):101-111.
[93]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.
[94]NAKATSUKA T,FUJIMUNE T,YOSHIKAWA C,et al.Biogenic and lithogenic particle fluxes in the western region of the Sea of Okhotsk:implications for lateral material transport and biological productivity[J].Journal of Geophysical Research:Oceans,2004,109(C9):C09S13.DOI:10.1029/2003JC001908.
[95]NISHIOKA J,ONO T,SAITO H,et al.Iron supply to the western subarctic Pacific:importance of iron export from the Sea of Okhotsk[J].Journal of Geophysical Research:Oceans,2007,112(C10):C10012.DOI:10.1029/2006JC004055.
[96]FISCHER H,WAHLEN M,SMITH J,et al.Ice core records of atmospheric CO2around the Last Three Glacial Terminations[J].Science,1999,283(5408):1712-1714.
[97]BOSTOCK H C,OPDYKE B N,WILLIAMS M J M.Characterising the intermediate depth waters of the Pacific Ocean usingδ13C and other geochemical tracers[J].Deep Sea Research Part I:Oceanographic Research Papers,2010,57(7):847-859.
[98]PICHEVIN L E,REYNOLDS B C,GANESHRAM R S,et al.Enhanced carbon pump inferred from relaxation of nutrient limitation in the glacial ocean[J].Nature,2009,459(7250):1114-1117.