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海陆气候变化记录相滞后:松山-布容极性转换约束 被引量:12
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作者 朱日祥 潘永信 +1 位作者 郭斌 刘青松 《科学通报》 EI CAS CSCD 北大核心 1998年第11期1131-1134,共4页
松山 布容极性转换位于中国黄土沉积层L8,即对应于冰期 .该沉积层具有记录地球磁场长期变化以及剩磁的Lock in深度小于深海沉积物的Lock in深度等特点 .结合大洋钻探研究成果 ,提出第四纪以来海洋与陆地气候记录一直存在着相滞后的观点 .
关键词 地磁极性转换 气候 黄土 海陆气候变化 相滞后
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Advances in GDGT research in Chinese Marginal Seas: A review 被引量:6
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作者 GE HuangMin ZHANG ChuanLun 《Science China Earth Sciences》 SCIE EI CAS CSCD 2016年第6期1173-1186,共14页
Archaeal and bacterial glycerol dialkyl glycerol tetraethers(GDGTs) play a unique role in discerning the biogeochemical processes and climate change in terrestrial(e.g. soil, peat, stalagmites, lakes, rivers, hot spri... Archaeal and bacterial glycerol dialkyl glycerol tetraethers(GDGTs) play a unique role in discerning the biogeochemical processes and climate change in terrestrial(e.g. soil, peat, stalagmites, lakes, rivers, hot springs) and marine environments. Organic proxies based on GDGTs(e.g. TEX_(86), MBT/CBT and BIT) have made impressive applications in the open ocean and terrestrial environments. However, the applicability of these proxies in marginal seas has not been thoroughly evaluated, which is necessary given the complexity and dynamics of these systems, such as organic matter(OM) flux, hydrodynamic conditions, and human impact. This review aims to summarize recent studies of GDGTs and GDGT-based proxies in the Chinese marginal seas(CMS), which are characterized by diverse gradient in terrigenous supplies and ocean productivity and hold rich information on climate and sea level changes, ocean current dynamics, sedimentary evolution and biogeochemical processes. 展开更多
关键词 GDGTs TEX86 MBT/CBT BIT Chinese marginal seas
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