Sediment provenance variations in the southern Okhotsk Sea over the last 180 ka: Evidence from light and heavy minerals

[1]  G. Mollenhauer,et al.  Summer-temperature evolution on the Kamchatka Peninsula, Russian Far East, during the past 20,000 years , 2016 .

[2]  R. Stein,et al.  High-resolution IP25-based reconstruction of sea-ice variability in the western North Pacific and Bering Sea during the past 18,000 years , 2016, Geo-Marine Letters.

[3]  Min-Te Chen,et al.  Evidence of sea ice-driven terrigenous detritus accumulation and deep ventilation changes in the southern Okhotsk Sea during the last 180 ka , 2015 .

[4]  V. M. Pishchal’nik,et al.  Zoning the ice cover of the Sea of Okhotsk and the Sea of Japan , 2015, Herald of the Russian Academy of Sciences.

[5]  T. Nakatsuka,et al.  Distribution and transport processes of lithogenic material from the Amur River revealed by the Sr and Nd isotope ratios of sediments from the Sea of Okhotsk , 2014 .

[6]  K. Ohshima,et al.  What drives the southward drift of sea ice in the Sea of Okhotsk , 2014 .

[7]  P. Knutz,et al.  Ice-Rafted Debris (IRD) , 2014 .

[8]  D. Macdonald,et al.  Tying catchment to basin in a giant sediment routing system: a source-to-sink study of the Neogene–Recent Amur River and its delta in the North Sakhalin Basin , 2013 .

[9]  Peter A. Cawood,et al.  Provenance of North Atlantic ice-rafted debris during the last deglaciation--A new application of U-Pb rutile and zircon geochronology , 2013 .

[10]  C. Chen,et al.  Glacially derived material in an Inner Mongolian desert lake during Marine Isotope Stage 2 , 2012 .

[11]  Lester Lembke-Jene,et al.  Sea surface temperature variability and sea‐ice extent in the subarctic northwest Pacific during the past 15,000 years , 2012 .

[12]  K. Kobayashi,et al.  The Cretaceous Okhotsk–Chukotka Volcanic Belt (NE Russia): Geology, geochronology, magma output rates, and implications on the genesis of silicic LIPs , 2012 .

[13]  Takashi T. Sakamoto,et al.  Characteristics and ages of tephra layers in the central Okhotsk Sea over the last 350 kyr , 2012 .

[14]  R. Tiedemann,et al.  Okhotsk Sea ice coverage and Kamchatka glaciation over the last 350ka — Evidence from ice-rafted debris and planktonic δ18O , 2011 .

[15]  K. Chen,et al.  Magnetostratigraphy of marine sediment core MD01-2414 from Okhotsk Sea and its paleoenvironmental implications , 2011 .

[16]  I. Zhabin,et al.  Influence of the Amur River runoff on the hydrological conditions of the Amur Liman and Sakhalin Bay (Sea of Okhotsk) during the spring-summer flood , 2010 .

[17]  G. Haug,et al.  Subpolar Link to the Emergence of the Modern Equatorial Pacific Cold Tongue , 2010, Science.

[18]  Y. Okazaki,et al.  Sea-ice distribution and atmospheric pressure patterns in southwestern Okhotsk Sea since the Last Glacial Maximum , 2010 .

[19]  N. Harada,et al.  Petromagnetic parameters of bottom sediments as indicators of the climatic and environmental changes in the central zone of the Sea of Okhotsk during the last 350 kyr , 2009 .

[20]  G. Haug,et al.  Subarctic Pacific evidence for a glacial deepening of the oceanic respired carbon pool , 2009 .

[21]  V. Gornitz,et al.  Encyclopedia of Paleoclimatology and Ancient Environments , 2008 .

[22]  N. Harada,et al.  Millennial-scale climatic and environmental oscillations in the Sea of Okhotsk in response to global changes during the last 190 Ka , 2008 .

[23]  N. Harada,et al.  Freshwater impacts recorded in tetraunsaturated alkenones and alkenone sea surface temperatures from the Okhotsk Sea across millennial-scale cycles , 2008 .

[24]  Wei-Lung Wang,et al.  Reconstruction of Oceanographic Changes Based on the Diatom Records of the Central Okhotsk Sea over the last 500000 Years , 2008 .

[25]  C. Clark,et al.  A last glacial ice sheet on the Pacific Russian coast and catastrophic change arising from coupled ice–volcanic interaction , 2008 .

[26]  N. A. Nikolaeva,et al.  Chapter 17 Multivariate Analysis of Heavy Mineral Assemblages of Sediments from the Marginal Seas of the Western Pacific , 2007 .

[27]  N. Harada,et al.  Millennial-scale variations of sea-ice expansion in the southwestern part of the Okhotsk Sea during the past 120 kyr: Age model and ice-rafted debris in IMAGES Core MD01-2412 , 2006 .

[28]  H. Chen,et al.  Mineralogical and geochemical changes in the sediments of the Okhotsk Sea during deglacial periods in the past 500 kyrs , 2006 .

[29]  N. Kimura,et al.  Ice-rafted debris (IRD)-based sea-ice expansion events during the past 100 kyrs in the Okhotsk Sea , 2005 .

[30]  Y. Okazaki,et al.  Late Quaternary paleoceanographic changes in the southwestern Okhotsk Sea: Evidence from geochemical, radiolarian, and diatom records , 2005 .

[31]  R. Tiedemann,et al.  Late quaternary environmental changes on the southeastern slope of the Sea of Okhotsk inferred from benthic foraminifera , 2005 .

[32]  M. Leppäranta.  The drift of sea ice , 2004 .

[33]  K. Ikehara,et al.  Middle to late Holocene changes of the Okhotsk Sea Intermediate Water and their relation to atmospheric circulation , 2004 .

[34]  Dirk Nürnberg,et al.  Environmental change in the Sea of Okhotsk during the last 1.1 million years , 2004 .

[35]  M. Wakatsuchi,et al.  Radiolarians under the seasonally sea-ice covered conditions in the Okhotsk Sea: flux and their implications for paleoceanography , 2003 .

[36]  Y. Okazaki,et al.  The production scheme of Cycladophora davisiana (Radiolaria) in the Okhotsk Sea and the northwestern North Pacific: implication for the paleoceanographic conditions during the glacials in the high latitude oceans , 2003 .

[37]  H. Neil,et al.  Late Quaternary ice-rafting events in the SW Pacific Ocean, off eastern New Zealand , 2002 .

[38]  J. Southon,et al.  Glacial Holocene environment of the southeastern Okhotsk Sea: evidence from geochemical and palaeontological data , 2002 .

[39]  T. Nakatsuka,et al.  A biomarker approach for assessing marine and terrigenous inputs to the sediments of Sea of Okhotsk for the last 27,000 years , 2001 .

[40]  Y. Tachibana,et al.  Does the fresh water supply from the amur river flowing into the sea of Okhotsk affect sea ice formation , 2001 .

[41]  Bo Qiu,et al.  Kuroshio And Oyashio Currents , 2001 .

[42]  K. S. John,et al.  Regional patterns of Pleistocene ice‐rafted debris flux in the North Pacific , 1999 .

[43]  N. Kimura,et al.  Processes controlling the advance and retreat of sea ice in the Sea of Okhotsk , 1999 .

[44]  I. Koizumi,et al.  Latest Quaternary oceanographic changes in the Okhotsk Sea based on diatom records , 1999 .

[45]  Seelye Martin,et al.  The production of ice and dense shelf water in the Okhotsk Sea polynyas , 1998 .

[46]  Kozo Takahashi.  The Bering and Okhotsk Seas: modern and past paleoceanographic changes and gateway impact , 1998 .

[47]  O. A. Braitseva,et al.  Holocene Key-Marker Tephra Layers in Kamchatka, Russia , 1997, Quaternary Research.

[48]  J. Bischof,et al.  Origin of ice-rafted debris: Pleistocene paleoceanography in the western Arctic Ocean , 1996 .

[49]  Jiayan Yang,et al.  Modeling the near‐freezing dichothermal layer in the Sea of Okhotsk and its interannual variations , 1996 .

[50]  M. Bennett,et al.  Testing the climatic significance of dropstones: an example from southeast Spain , 1994, Geological Magazine.

[51]  H. Kassens,et al.  Sediments in Arctic sea ice: Implications for entrainment, transport and release , 1994 .

[52]  D. Cavalieri,et al.  On the relationship between atmospheric circulation and the fluctuations in the sea ice extents of the Bering and Okhotsk Seas , 1987 .

[53]  N. Untersteiner.  The Geophysics of Sea Ice: Overview , 1986 .

[54]  Saburo Aoki,et al.  The distribution of clay minerals in recent sediments of the Okhotsk Sea , 1978 .