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1)  paleoenvironmental contrast
古气候对比
2)  climatic event correlation
气候事件对比
3)  paleoclimate ['pæliəu,klaimit]
古气候
1.
Compostion of Carbon Isotopes in Soil Carbonates and Paleoclimate Recoreds of The Late Holocene in the West of Jilin,China;
吉林西部全新世晚期土壤碳酸盐中碳稳定同位素记录的古气候信息
2.
Evolutional characteristics and their paleoclimate significance of elements in the Qianjiang formation, Qianjiang depression;
潜江凹陷潜江组元素演化特征及其古气候意义
3.
Numerical modeling in paleoclimate study:Progress and problems;
古气候数值模拟:进展评述
4)  palaeo-climate
古气候
1.
We have researched the forming condition of gas hydrate in the South China Sea according to the physical oceanography,palaeo-climate,sedimentary environment,and tectonic environment.
从物理海洋、古气候、沉积环境和构造环境分析入手,研究了南海天然气水合物的形成条件。
2.
Distribution patterns of phytolith percentage,warmth index and grass cover index demonstrate that there occur 3 assemblage zones in response to palaeo-vegetation and palaeo-climate changes in mid-late Pleistocene,respectively.
在温暖指数和草本覆盖指数计算基础上,获得了中—晚更新世以来的3个古植被、古气候演化组合带;运用植硅体和分子化石的相关指标(C21-/C22+、C23/C30)揭示了洪积扇红土沉积时期的植被与气候信息,即间冰期气候暖湿,风化作用强,降水较多,高等草本植物繁盛;而冰期时气候干凉,风化作用弱,降水减少和地下水位降低等则有利于洪积扇体上木本类植被发育。
5)  palaeoclimate
古气候
1.
Effect of palaeoclimate change at the late Cretaceous period on lithologic sequences in Songliao basin;
松辽盆地晚白垩世古气候变化对层序发育的影响
2.
Palynological Assemblages of Pleistocence from Shanghai Region and Its Palaeovegetation and Palaeoclimate;
上海地区更新世孢粉组合及其古植被、古气候
3.
A δ~(13)C record of the organic matter in lacustrine sediments of the core ZHJfrom Lake Caohai and its palaeoclimate implications;
草海ZHJ柱样沉积物有机质的δ~(13)C记录及其古气候信息
6)  paleo-climate
古气候
1.
Predicting Paleo-climate Since 140 Ma B.P. by Experiment of Carbon Isotope in Loess;
用洛川黄土中碳同位素重建140万年以来古气候
2.
Using the function, paleo-climate parameters of Yunshu peat profile were calculated and the paleo-climate evolution is then divided into 7 stages: warm-cold-warm-clod-warm-cold-warm.
根据泥炭表土植硅体分析和气候气象资料,运用因子分析和逐步回归分析方法建立了东北地区泥炭表土植硅体—气候因子转换函数;并将之用于榆树泥炭剖面的古气候参数重建中,得出近3000a来的古气候参数值,并将之暖—冷—暖—冷—暖—冷—暖7个阶段。
3.
The authors introduce and summarize some important progress made in paleo-vegetation and paleo-climate researches,especially the recognition of biological origin,reconstruction of paleo-vegetation, paleo-temperature and climatic change.
与古植被、古气候变化密切相关的正构烷烃分子化石及其单体碳同位素的研究是近年来最为引人注目和关切的环境科学问题之一,这一研究在国际上已取得了一定的成果。
补充资料:东北平原农业气候资源利用(见农业气候资源利用)


东北平原农业气候资源利用(见农业气候资源利用)


  默军爵攫戳猛罚胃植和l用2 iyuanl心yong 见农业气候资
  
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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