Sea-surface temperature and salinity changes in the northwest Pacific since the last glacial maximum

Journal of Quaternary Science

Volumn 19, Issue 4, 2004, Pages 335-346

  Oba, Tadamichi ^a   Murayama, Masafumi ^b  

^a HOKKAIDO UNIVERSITY   (Japan)

^b KOCHI UNIVERSITY   (Japan)

Author keywords

Benthic and planktonic foraminifera; Holocene and LGM; Northwest Pacific; Oxygen isotope; Palaeo SST and SSS

Indexed keywords

FORAMINIFERA; HOLOCENE; LAST GLACIAL MAXIMUM; OXYGEN ISOTOPE; PALEOCEANOGRAPHY; SEA SURFACE SALINITY; SEA SURFACE TEMPERATURE;

PACIFIC OCEAN; PACIFIC OCEAN (NORTHWEST);

FORAMINIFERA;

EID: 3142610887     PISSN: 02678179     EISSN: None     Source Type: Journal    
DOI: 10.1002/jqs.843     Document Type: Article

References (44)

1. 18O of the glacial deep ocean. Science 298: 1769-1773.
2. Arikawa R. 1983. Distribution and taxonomy of Globigerina pachyderma (Ehrenberg) off the Sanriku Coast, Northeast Honshu, Japan. Tohoku University Science Report, Second Series (Geology) 53: 103-157.
3. Chappell J. 2002. Sea level changes forced ice breakouts in the Last Glacial cycle: new results from coral terraces. Quaternary Science Reviews 21: 1229-1240.
4. Chappell J, Shackleton NJ. 1986. Oxygen isotopes and sea level. Nature 324: 137-140.
5. Chinzei K, Fujioka K, Kitazato H, Koizumi I, Oba T, Oda M, Okada H, Sakai T, Tanimura Y. 1987. Postglacial environmental change of the Pacific Ocean off the coasts of central Japan. Marine Micropaleontology 11: 273-291.
6. Duplessy JC, Labeyrie L, Waelbroeck C. 2002. Constraints on the ocean oxygen isotopic enrichment between the Last Glacial Maximum and the Holocene: paleoceanographic implications. Quaternary Science Reviews 21: 315-330.
7. 18O content of waters from natural sources. Geochimica Cosmochimica Acta 4: 213-224.
8. Fairbanks RG. 1989. A 17 000 year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep ocean circulation. Nature 342: 637-642.
9. Itou M. 2000. Deep-dwelling planktonic foraminifers as proxies of subsurface and intermediate waters. PhD thesis, Hokkaido University: 84.
10. Japan Oceanographic Data Center. 1995. Temperature Profile Data Set, CD-ROM JODC-1. Hydrographic Department Maritime Safety Agency: Tokyo.
11. Kallel N, Labeyrie LD, Arnold M, Okada H, Dudley WC, Duplessy JC. 1988. Evidence of cooling during the Younger Dryas in the western North Pacific, Oceanological Acta 11: 369-375.
12. Keigwin LD. 1998. Glacial-age hydrography of the far northwest Pacific Ocean. Paleoceanography 13: 323-339.
13. 13C system in the eastern equatorial Pacific. Deep-Sea Research 21: 211-227.
14. Labeyrie LD, Duplessy JC, Blanc PL. 1987. Variations in mode of formation and temperature of oceanic deep waters over the past 125 000 years. Nature 327: 477-482.
15. Labeyrie LD, Kallel N, Arnold M, Juillet-lelerc A, Maitre F, Duplessy JC, Shackleton NJ. 1990. Variability of the intermediate and deep waters in the north west Pacific ocean during the last deglaciation. Oceanological Acta (special volume) 10: 329-339.
16. Labeyrie LD, Duplessy C, Duprat J, Leclerc AJ, Moyes J, Michel E, Kallel N, Shackleton NJ. 1992. Changes in the vertical structure of the North Atlantic Ocean between glacial and modern times. Quaternary Science Reviews 11: 401-413.
17. Labeyrie LD, Cole J, Alverson K, Stocker T. 2002. The history of climate dynamics in the Late Quaternary. In Paleoclimates, Global Change and the Future, Alverson K, Bradley R, Pedersen T (eds). IGBP Series, Springer: Berlin; 33-62.
18. Lea DW, Pak DK, Spero HJ. 2000. Climate impact of late Quaternary equatorial Pacific sea surface temperature variations. Science 289(5486): 1719-1724.
19. Lea DW, Martin PA, Pak DK, Spero HJ. 2002. Reconstructing a 350 ky history of sea level using planktonic Mg/Ca and oxygen isotope records from a Cocos Ridge core. Quaternary Science Reviews 21: 283-293.
20. Machida H, Arai F. 1992. Atlas of Tephra in and around Japan. University of Tokyo Press: Tokyo; 276 pp.
21. Martin PA, Lea DW, Rosenthal Y, Shackleton NJ, Sarnthein M, Papenfuss T. 2002. Quaternary deep sea temperature histories derived from benthic foraminiferal Mg/Ca. Earth and Planetary Science Letters 198: 193-209.
22. Martinson DG, Pisias NG, Hays JD, Imbrie J, Moore TC, Shackleton NJ. 1987. Age dating and the orbital theory of the ice age: development of a high-resolution 0 to 300 000-year chronostratigraphy. Quaternary Research 27: 1-29.
23. 18O water using foraminiferal Mg. Earth and Planetary Science Letters 170(4): 417-432.
24. Matsumoto K, Oba T, Lynch-Stieglitz J, Yamamoto H. 2002. Interior hydrography and circulation of the glacial Pacific Ocean. Quaternary Science Review 21: 1693-4704.
25. Mix AC, Bard E, Schneider R. 2001. Environmental processes of the ice age: land, oceans, glaciers (EPILOG). Quaternary Science Reviews 20: 627-657.
26. Oba T. 1991. Oxygen isotope results from three piston cores: KT90-9, ST-1, 5 and 21. Science Reports of Hirosaki University 38: 65-71.
27. Oba T, Yamane M. 2002. Sea surface temperatures off the east coast of Japan at the last glacial maximum inferred from oxygen isotope of foraminiferal tests. In Marine Environment: The Past, Present and Future, Chen CTA (ed.). The Fuwen Press: Kaohsiung, Taiwan; 64-77.
28. Ohkushi K, Nemoto N, Murayama M, Nakamura T, Tsukawaki S. 2000, Paleoceanography of the Oyashio area during the last 20 000 years based on benthic foraminifera. The Quaternary Research 39: 439-449. (In Japanese with English abstract.)
29. O'Neil JR, Clayton RN, Mayeda T. 1969. Oxygen isotope fractionation in divalent m et al. carbonates. Journal of Chemical Physics 51: 5547-5558.
30. Park BK, Shin IC. 1998. Seasonal distribution of planktonic foraminifers in the East Sea (Sea of Japan), a large marginal sea of the northwest Pacific. Journal of Foraminiferal Research 28: 321-326.
31. Sautter LR, Thunell RC. 1991. Planktonic foraminiferal response to upwelling and seasonal hydrographic conditions: sediment trap results from San Pedro Basin, southern California bight. Journal of Foraminiferal Research 21: 347-363.
32. Schrag DP, Hampt G, Murra DW. 1996. The temperature and oxygen isotopic composition of the glacial ocean. Science 272: 1930-1932.
33. Schrag DP, Adkins JF, McIntyre K, Alexander JL, Hodell DA, Charles CD, McManus JF. 2002. The oxygen isotopic composition of seawater during the Last Glacial Maximum. Quaternary Science Reviews 21: 331-342.
34. Shackleton NJ. 1974. Attainment of isotopic equilibrium between ocean water and the benthic foraminifera genus Uvigerina: isotopic changes in the ocean during the last glacial. Colloques Internationaux du Centre National de la Recherche Scientifique 219: 203-209.
35. Shackleton NJ. 1987. Oxygen isotopes, ice volume and sea level. Quaternary Science Reviews 6: 183-190.
36. Shackleton NJ. 2000. The 100 000-year ice-age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity. Science 289: 1897-1902.
37. dw indicating deep-water source variations in the Northeast Atlantic, 0-34 cal. Ka BP. Geochemistry Geophysics Geosystems 4(12): 1525-2027.
38. 14C database and revised CALIB radiocarbon calibration program. Radio Carbon 35: 215-230.
39. Takemoto A, Oda M. 1997. New planktonic foraminiferal transfer functions for the Kuroshio-Oyashio Current region off Japan. Palontological Research 1: 291-310.
40. Thompson PR. 1981. Planktonic foraminifera in the western north Pacific during the past 150 000 years: comparison of modern and fossil assemblages. Palaeogeography, Palaeoclimatology, Palaeoecology 35: 241-279.
41. Thompson PR, Shackleton NJ. 1980. North Pacific palaeoceanography: late Quaternary coiling variations of planktonic foraminifer Neogloboquadrina pachyderma. Nature 287: 829-833.
42. Waelbroeck C, Labeyrie LD, Michel E, Duplessy JC, McManus JF, Lambeck K, Balbon E, Labracherie M. 2002. Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records. Quaternary Science Reviews 21: 295-305.
43. Yasuda I. 1997. The origin of the North Pacific Intermediate Water. Journal Geophysical Research 102: 893-909.
44. Yamane M, Oba T. 1999. Paleoceanographic change of the Sanriku area during the last 90 000 years based on the analysis of a sediment core (KH94-3, LM-8). The Quaternary Research 38: 1-16. (In Japanese with English abstract.)