Alkenone sea-surface temperatures and carbon burial at site 846 (Eastern Equatorial Pacific Ocean) : the last 1.3 M.Y.
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A. Mix | K. Emeis | D. Schulz-Bull | H. Doose
[1] M. Sarnthein,et al. Molecular record of secular sea surface temperature changes on 100-year timescales for glacial terminations I, II and IV , 1992, Nature.
[2] F. Prahl,et al. Upwelling and productivity changes inferred from a temperature record in the central equatorial Pacific , 1992, Nature.
[3] S. Brassell,et al. Long-chain alkenones and alkyl alkenoates and the fossil coccolith record of marine sediments , 1990 .
[4] Francisco P. Chavez,et al. Phytoplankton taxa in relation to primary production in the equatorial Pacific , 1990 .
[5] Alan C. Mix,et al. Surface water response of the equatorial Atlantic Ocean to orbital forcing , 1989 .
[6] Laurel A Muehlhausen,et al. Further evaluation of long-chain alkenones as indicators of paleoceanographic conditions , 1988 .
[7] N. Pisias,et al. Late Pleistocene paleoclimatology of the central equatorial Pacific: Sea surface response to the southeast Trade Winds , 1988 .
[8] D. Murray,et al. The record of Late Pleistocene biogenic sedimentation in the eastern tropical Pacific Ocean , 1988 .
[9] F. Chavez,et al. An estimate of new production in the equatorial Pacific , 1987 .
[10] A. Kuijpers,et al. A Mid-Brunhes Climatic Event: Long-Term Changes in Global Atmosphere and Ocean Circulation , 1986, Science.
[11] G. Eglinton,et al. Molecular stratigraphy: a new tool for climatic assessment , 1986, Nature.
[12] H. Bryden,et al. Diagnostic Model of the Three-Dimensional Circulation in the Upper Equatorial Pacific Ocean , 1985 .
[13] C. Schramm. Implications of Radiolarian Assemblages for the Late Quaternary Paleoceanography of the Eastern Equatorial Pacific , 1985, Quaternary Research.
[14] E. Boyle. Chemical Accumulation Variations Under the Peru Current During the Past , 1983 .
[15] K. Wyrtki. An Estimate of Equatorial Upwelling in the Pacific , 1981 .
[16] E. Davidson,et al. What are the physical, chemical, and biological processes that control the formation and degradation of nonliving organic matter? , 1995 .
[17] M. Lyle. 8. COMPOSITION MAPS OF SURFACE SEDIMENTS OF THE EASTERN TROPICAL PACIFIC OCEAN1 , 1992 .
[18] V. Ittekkot,et al. Organic carbon removal in the sea: the continental connection , 1992, Geological Society, London, Special Publications.
[19] J. Imbrie,et al. Oceanic Response to Orbital Forcing in the Late Quaternary: Observational and Experimental Strategies , 1989 .
[20] G. Eldin,et al. Southwestward extent of chlorophyll-enriched waters from the Peruvian and equatorial upwellings between Tahiti and Panama , 1987 .
[21] T. Pedersen. Increased productivity in the eastern equatorial Pacific during the last glacial maximum (19,000 to 14,000 yr B.P) , 1983 .
[22] P. Müller,et al. Glacial-Interglacial Cycles in Oceanic Productivity Inferred from Organic Carbon Contents in Eastern North Atlantic Sediment Cores , 1983 .