Hostname: page-component-cd9895bd7-q99xh Total loading time: 0 Render date: 2024-12-26T17:25:24.408Z Has data issue: false hasContentIssue false
  • English
  • Français

Pollen and Radiolarian Records from Deep-Sea Core RC14-103: Climatic Reconstructions of Northeast Japan and Northwest Pacific for the Last 90,000 Years

Published online by Cambridge University Press:  20 January 2017

Linda E. Heusser  and
Joseph J. Morley
Linda E. Heusser
Affiliation:
Lamont-Doherty Geological Observatory, Columbia University, Palisades, New York 10964
Joseph J. Morley
Affiliation:
Lamont-Doherty Geological Observatory, Columbia University, Palisades, New York 10964
Get access Rights & Permissions [Opens in a new window]

Abstract

Using modern pollen and radiolarian distributions in sediments from the northwest Pacific and seas adjacent to Japan to interpret floral and faunal changes in core RC14-103 (44°02′N, 152°56′E), we recognize two major responses of the biota of eastern Hokkaido and the northwest Pacific to climatic changes since the last interglaciation. Relatively stable glacial environments (∼80,000–20,000 yr B.P.) were basically cold and wet (<4°C and ∼1000 mm mean annual temperature and precipitation, respectively) with boreal conijers and tundra/park-tundra on Hokkaido, and cool (<16°C) summer and cold (<1.0°C) winter surface temperatures offshore. Contrasting nonglacial environments (∼10,000–4000 yr B.P.) were warm and humid (>8°C and >1200 mm mean annual temperature and precipitation, respectively), supporting climax broadleaf deciduous forest with Quercus and Ulmus/Zelkova, with surface waters in the northwest Pacific characterized by warm (>1.5°C) winter and cold (10.4°–14.3°C) summer temperatures. Climatic evidence from RC14-103 shows a high degree of local and regional variation within the context of global climatic change. Correlative ocean and land records provide the detailed input necessary to assess local/regional responses to variations in other key elements (i.e., solar radiation, monsoonal variations) of the northeast Asian climate system.

Type
Research Article
Information
Quaternary Research , Volume 24 , Issue 1 , July 1985 , pp. 60 - 72
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Aleksandrova, A.N. Aleksandrov, S.M. (1974). Marine Holocene sediments of Sakhalin Doklady Akademii Nauk SSSR 216, 615–618 Google Scholar
Braytseva, O. Yevteyeva, I. Lupikinia, Y. Sulerzhitskiy, L. (1973). Subdivision and absolute geochronology of the Holocene peat bogs of Kamchatka Doklady Akademii Nauk SSSR 208, 916–919 Google Scholar
CLIMAP Project Members, (1981). Seasonal Reconstructions of the Earth's Surface at the Last Glacial Maximum Geological Society of America Map and Chart Series No. 36, Boulder, ColoGoogle Scholar
Fuji, N. (1975). Climatic change of the Wisconsin stage in the Japanese Island from the viewpoint of palynological research Horie, S. Paleolimnology of Lake Biwa and the Japanese Pleistocene Vol. 3, 321–351 Google Scholar
Fuji, N. (1976). Paleoclimatic and paleovegetational changes around Lake Biwa, central Japan during the past 100,000 years Horie, S. Paleolimnology of Lake Biwa and the Japanese Pleistocene Vol. 4, 316–356 Google Scholar
Fuji, N. (1977). Paleoclimatic and paleovegetational changes around Lake Biwa, central Japan during the past 100,000 years Fukui, E. The Climate of Japan Elsevier New York Google Scholar
Heusser, L. Shackleton, N. (1979). Direct marine-continental correlation: 150,000-year oxygen isotope-pollen record from the North Pacific Science (Washington, D.C.) 204, 837–839 CrossRefGoogle ScholarPubMed
Heusser, L. Stock, C. (1984). Preparation techniques for concentrating pollen from marine sediments and other sediments with low pollen density Palynology 8, 225–227 CrossRefGoogle Scholar
Imbrie, J. Hays, J. Martinson, D. McIntyre, A. Mix, A. Morley, J. Pisias, N. Prell, W. Shackleton, N. (1984). The orbital theory of Pleistocene climate: Support from a revised chronology of the marine 18O record Berger, A. Milankovitch and Climate Reidel Boston 269–305 Part IGoogle Scholar
Imbrie, J. Kipp, N. (1971). A new micropaleontological method for quantitative paleoclimatology: Application to a late Pleistocene Caribbean core Turekian, K. Late Cenozoic Glacial Ages Yale Univ. Press New Haven, Conn 71–181 Google Scholar
Kaifa, W. (1983). The sporo-pollen and algal assemblages from the sediments of the Okinawa though Oceanologia et Limnologia Sinica 13, 441–450 Google Scholar
Koroneva, E. (1957). Spore-pollen analysis of bottom sediments from the Sea of Okhotsk Trudy Institut Okeanologia Akademii Nauk SSR 22, 221–251 Google Scholar
Moore, T. Jr. (1973). Method of randomly distributing grains for microscopic examination Journal of Sedimentary Petrology 43, 904–906 Google Scholar
Moore, T.C. Jr. Burekle, L. Geitzenauer, B. Luz, B. Molina-Cruz, A. Robertson, J. Sachs, H. Sancetta, C. Thiede, J. Thompson, P. Wenkam, C. (1980). Marine Micropaleontology 5, 215–247 CrossRefGoogle Scholar
Moore, T.C. Jr. Heath, G.R. (1978). Sea floor sampling techniques Chemical Oceanography 7, 75–126 Google Scholar
Morley, J. Hays, J. (1979). Cycladophora davisiana: A stratigraphic tool for Pleistocene North Atlantic and interhemispheric correlation Earth and Planetary Science Letters 44, 383–389 CrossRefGoogle Scholar
Morley, J. Hays, J. Robertson, J. (1982). Stratigraphic framework for the late Pleistocene in the northwest Pacific Ocean Deep-Sea Research 29, 1485–1499 CrossRefGoogle Scholar
Nakamura, J. (1968). Palynological study on the Quaternary deposits in Hokkaido district. Vegetational change since the Wurm glacial age (V) Reports of the Kochi University, Natural Science 17, 39–51 Google Scholar
Nakamura, J. (1974). Palynological study on the Quaternary deposits in Hokkaido district. Vegetational change since the Wurm glacial age (V) Numata, M. The Flora and Vegetation of Japan Elsevier New York Google Scholar
Robertson, J.H. (1975). Glacial to Interglacial Oceanographic Changes in the Northwest Pacific, Including a Continuous Record of the Last 400,000 Years Ph.D. thesis Columbia University Google Scholar
Sancetta, C. (1979). Oceanography of the North Pacific during the last 18,000 years: Evidence from fossil diatoms Marine Micropaleontology 4, 103–123 CrossRefGoogle Scholar
Sarro, T. Heusser, L. Morley, J. (1984). Marine and continental environments of Japan: 60,000 years of record from the Sea of Japan and Honshu Geological Society of America Abstracts with Programs 16, 62 Google Scholar
Tatewaki, M. (1957). Geobotanical studies on the Kurile Islands Acta Horti Gotoburgensis 21, 43–123 Google Scholar
Thompson, P. (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 CrossRefGoogle Scholar
Tsuskada, M. (1960). Pollen analytical studies of postglacial age in Japan. IV. The Torii River area (five pollen diagrams of the Pleistocene) Journal of the Institute of Polytechnics, Osaka City University Series D 11, 91–99 Google Scholar
Tsukada, M. (1963). Umbrella pine, Sciadopitys verticillata: Past and present distribution in Japan Science (Washington, D.C.) 142, 1680–1681 CrossRefGoogle ScholarPubMed
Tsukada, M. (1967a). Pollen succession, absolute pollen frequency, and recurrence surfaces in central Japan American Journal of Botany 54, 821–831 CrossRefGoogle Scholar
Tsukada, M. (1967b). Vegetation and climate around 10,000 B.P. in central Japan American Journal of Science 265, 562–585 CrossRefGoogle Scholar
Tsukada, M. (1981a). Cryptomeria japonica D. Don. I. Pollen dispersal and logistic forest expansion Japanese Journal of Ecology 31, 371–383 Google Scholar
Tsukada, M. (1981b). The last 12,000 years—the vegetation history of Japan. II. New pollen zones Japanese Journal of Ecology 31, 201–215 Google Scholar
Tsukada, M. (1982). Cryptomeria japonica: Glacial refugia and late-glacial and postglacial migration Ecology 63, 1091–1105 CrossRefGoogle Scholar
Tsukada, M. (1983a). Man and vegetation in prehistoric Japan Encyclopedia of Japan Vol. 3 Kodansha New York 177–179 Google Scholar
Tsukada, M. (1983b). Vegetation and climate during the last glacial maximum in Japan Quaternary Research 19, 212–235 CrossRefGoogle Scholar
Tsukada, M. (1985). Map of yegetation during the last glacial maximum in Japan Quaternary Research. CrossRefGoogle Scholar
Vastano, A. Bernstein, R. (1984). Mesoscale features along the first Oyashio intrusion Journal of Geophysical Research 89, 587–596 CrossRefGoogle Scholar
Walter, H. (1973). Vegetation of the Earth Springer-Verlag New York Google Scholar
Wang, C. (1961). The Forests of China Harvard Univ. Press Cambridge, Mass Google Scholar
Wijmstra, T. van der Hammen, T. (1974). The last interglacial-glacial cycle: State of affairs of correlation between data obtained from the land and from the ocean Geologie en Mijnbouw 53, 386–392 Google Scholar
Woillard, G. (1978). Grande Pile peat bog: A continuous pollen record for the last 140,000 years Quaternary Research 9, 1–21 CrossRefGoogle Scholar