Global paleoclimate indicators are the proxies sensitive to global paleoclimatic environment changes. They are mostly derived from marine sediments. Paleoclimate indicators derived from terrestrial sediments, on the other hand, are commonly influenced by local tectonic movements and paleogeographic variations. Factors governing the earth climate system include plate tectonics, which controls the configuration of continents, the interplay between the atmosphere and the ocean, and the earth's orbital characteristics (Milankovitch cycles). Global paleoclimate indicators are established based on the information extracted from the analyses of geologic materials, including biological, geochemical and mineralogical data preserved in marine sediments. Indicators are generally grouped into three ca
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| - Global Paleoclimate Indicators (en)
- 全球性古氣候指標 (zh)
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| - 全球性古氣候指標(英語:Global Paleoclimate Indicators)是指能反映全球古氣候環境變化的指標,大多來自。而源自陸地沉積物的古氣候指標容易受到板塊運動與古地理變化的影響。主要控制地球氣候系統的因素包括控制大陸分佈的板塊構造、大氣和海洋之間的相互作用以及地球軌道的特性(米蘭科維奇循環)。全球性古氣候指標是根據地質材料分析所得到的資訊而建立的,這些資訊包含保存在海洋沉積物中的生物學、地球化學和礦物學的資料。指標一般分為三類:古生物學、地球化學和岩性。 (zh)
- Global paleoclimate indicators are the proxies sensitive to global paleoclimatic environment changes. They are mostly derived from marine sediments. Paleoclimate indicators derived from terrestrial sediments, on the other hand, are commonly influenced by local tectonic movements and paleogeographic variations. Factors governing the earth climate system include plate tectonics, which controls the configuration of continents, the interplay between the atmosphere and the ocean, and the earth's orbital characteristics (Milankovitch cycles). Global paleoclimate indicators are established based on the information extracted from the analyses of geologic materials, including biological, geochemical and mineralogical data preserved in marine sediments. Indicators are generally grouped into three ca (en)
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| - Global paleoclimate indicators are the proxies sensitive to global paleoclimatic environment changes. They are mostly derived from marine sediments. Paleoclimate indicators derived from terrestrial sediments, on the other hand, are commonly influenced by local tectonic movements and paleogeographic variations. Factors governing the earth climate system include plate tectonics, which controls the configuration of continents, the interplay between the atmosphere and the ocean, and the earth's orbital characteristics (Milankovitch cycles). Global paleoclimate indicators are established based on the information extracted from the analyses of geologic materials, including biological, geochemical and mineralogical data preserved in marine sediments. Indicators are generally grouped into three categories; paleontological, geochemical and lithological. (en)
- 全球性古氣候指標(英語:Global Paleoclimate Indicators)是指能反映全球古氣候環境變化的指標,大多來自。而源自陸地沉積物的古氣候指標容易受到板塊運動與古地理變化的影響。主要控制地球氣候系統的因素包括控制大陸分佈的板塊構造、大氣和海洋之間的相互作用以及地球軌道的特性(米蘭科維奇循環)。全球性古氣候指標是根據地質材料分析所得到的資訊而建立的,這些資訊包含保存在海洋沉積物中的生物學、地球化學和礦物學的資料。指標一般分為三類:古生物學、地球化學和岩性。 (zh)
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