Biogenic Sediments and Their Paleoceanographic Implication in West Pacific Warm Pool during the Pleistocene

作     者：王汝建 肖文申 

作者机构：State Key Laboratory of Marine GeologyTongji University Alfred Wegener Institute for Polar and Marine Research 

出 版 物：《Journal of Earth Science》 (地球科学学刊（英文版）)

年 卷 期：2010年第21卷第1期

页      面：42-54页

核心收录：

学科分类：070903[理学-古生物学与地层学(含：古人类学)] 0709[理学-地质学] 07[理学] 

基　　金：supported by the National Key Basic Research Programme (No. G2007CB815903) the National Natural Science Foundation of China (No. 40321603) the Foundation of National Excellent Doctoral Dissertation of China (No. 200126) 

主　　题：biogenic sediment paleoceanographic implication West Pacific Warming Pool Pleistocene. 

摘      要：Primary productivity has played an important role in the global carbon cycle during the Quaternary. The average Corg/N ratio was 7.0 from the core MD97-2140 in the West Pacific Warm Pool （WPWP） over the last 1 755 ka, which indicates a main contribution of marine organic carbon to the organic matter in the sediments. Large fluctuations in mass accumulation rates （MARs） of biogenics and lithogenics from this core since the marine isotope stage （MIS） 6 reflected the moderate variability in oceanographic condition, while tittle fluctuations in MAR-biogenics and -lithogenics from the MIS 59 to MIS 7 implied the relatively stable and uniform oceanographic condition, although the sea surface temperatures （SSTs） probably fluctuated by ca. 5 ℃. MAR-organic since the MIS 6 increased evidently during the glacial periods, which ascribed to terrestrial inputs, including lithogenic matter and dissolved nutrient, which also contribute to stimulating primary productivity. The results compared among the four cores in the WPWP since the MIS 9 indicate that in the western sector with the shallow thermocline, high primary productivity during the glacial periods was controlled by wind-induced surface water mixing, upwelling, and terrestrial inputs, while in the central and eastern sectors, the little different medium to low productivity might have been made by more intense upweil- ing driven by strong winds because the thicker warm surface water pool and the deeper thermocline prevented nutrient-bearing water from upwelling to upper water column even during the glacial times.