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古海洋研究中的地球化学新指标 被引量:64
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作者 陈建芳 《地球科学进展》 CAS CSCD 2002年第3期402-410,共9页
有机地球化学与微量元素地球化学古环境指标及其相关的同位素指标已成为追溯古全球变化与古海洋生物地球化学演化的有力工具。从古环境替代指标的示踪原理和应用的角度 ,综述了有孔虫碳同位素、有机地球化学整体指标、生物标志化合物、... 有机地球化学与微量元素地球化学古环境指标及其相关的同位素指标已成为追溯古全球变化与古海洋生物地球化学演化的有力工具。从古环境替代指标的示踪原理和应用的角度 ,综述了有孔虫碳同位素、有机地球化学整体指标、生物标志化合物、单体有机分子同位素、微量元素等在古海洋古环境研究中的应用及相关的研究动态与进展。指出古海洋研究正从以恢复古海洋的物理参数 (温度、盐度、古洋流等 )为主 ,向着揭示古水团演化、古生产力、古营养状况。 展开更多
关键词 古海洋学 有机地球化学 微量元素 同位素 古生物地球化学演化
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中国北方黄土区C-3草本植物碳同位素组成研究 被引量:64
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作者 王国安 韩家懋 刘东生 《中国科学(D辑)》 CSCD 北大核心 2003年第6期550-556,共7页
对生长在我国北方黄土区的367个C-3草本植物样品进行了碳同位素分析,结果表明我国北方黄土区C-3草本植物δ^(13)C值分布区间为-21.7%。~-30.0‰,平均值为-26.7‰;黄土高原中部半湿润区的C-3草本植物δ^(13)C值分布集中,在-24.4%。~-... 对生长在我国北方黄土区的367个C-3草本植物样品进行了碳同位素分析,结果表明我国北方黄土区C-3草本植物δ^(13)C值分布区间为-21.7%。~-30.0‰,平均值为-26.7‰;黄土高原中部半湿润区的C-3草本植物δ^(13)C值分布集中,在-24.4%。~-28.5‰之间,平均值为-27.5‰;而黄土高原西部边缘的半干旱-干旱气候区的C-3植物δ^(13)C值变化范围在-21.7‰~-30.0‰,平均值为-26.2‰;C-3植物的δ^(13)C值在黄土高原中部的半湿润气候区比黄土高原西部边缘半干旱-干旱气候区显著偏轻。年降雨量是造成这种显著偏轻的主要原因,C-3植物的碳同位素组成随着年降雨量的减少而变重,在我国北方黄土区年降雨量每增加100mm,C-3植被δ^(13)C平均值将偏负约0.49‰左右。 展开更多
关键词 中国北方黄土区 C-3草本植物 碳同位素 年降雨量 气候偏轻 古生物地球化学
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Progress and perspective on frontiers of geobiology 被引量:11
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作者 XIE ShuCheng YIN HongFu 《Science China Earth Sciences》 SCIE EI CAS 2014年第5期855-868,共14页
Geobiology is a new discipline on the crossing interface between earth science and life science, and aims to understand the in- teraction and co-evolution between organisms and environments. On the basis of the latest... Geobiology is a new discipline on the crossing interface between earth science and life science, and aims to understand the in- teraction and co-evolution between organisms and environments. On the basis of the latest international achievements, the new data presented in the Beijing geobiology forum sponsored by Chinese Academy of Sciences in 2013, and the papers in this special issue, here we present an overview of the progress and perspectives on three important frontiers, including geobiology of the critical periods in Earth history, geomicrobes and their responses and feedbacks to global environmental changes, and geobiology in extreme environments. Knowledge is greatly improved about the close relationship of some significant biotic events such as origin, radiation, extinction, and recovery of organisms with the deep Earth processes and the resultant envi- ronmental processes among oceans, land, and atmosphere in the critical periods, although the specific dynamics of the co-evolution between ancient life and paleoenvironments is still largely unknown. A variety of geomicrobial functional groups were found to respond sensitively to paleoenvironmental changes, which enable the establishment of proxies for paleoenvi- ronmental reconstruction, and to play active roles on the Earth environmental changes via elemental biogeochemical cycles and mineral bio-transforrnations, but to be deciphered are the mechanisms of these functional groups that change paleoenvi- ronmental conditions. Microbes of potential geobiology significance were found and isolated from some extreme environments with their biological properties partly understood, but little is known about their geobiological functions to change Earth envi- ronments. The biotic processes to alter or modify the environments are thus proposed to be the very issue geobiology aims to decipher in the future. Geobiology will greatly extend the temporal and spatial scope of biotic research on Earth and beyond. It has great potential of application in the domains of resource exploration and global change. To achieve these aims needs coor- dinative multidisciplinary studies concerning geomicrobiology and related themes, database and modeling of biogeochemical cycles, typical geological environments, and coupling of biological, physical, and chemical processes. 展开更多
关键词 microbial functional group extreme environment biotic crisis PALEOBIOLOGY
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