Please use this identifier to cite or link to this item:
192.168.6.56/handle/123456789/13923
Title: | Climate, Fire and Human Evolution |
Other Titles: | The Deep Time Dimensions of the Anthropocene |
Authors: | Andrew Y., Glikson Colin, Groves |
Keywords: | The Deep Time Dimensions of the Anthropocene |
Issue Date: | 2016 |
Publisher: | Springer |
Description: | The development of isotopic age determination methods and stable isotopic tracers to paleo-climate investigations, including oxygen (δ18O), sulphur (δ33S) and carbon (δ13C), integrated with Sedimentological records and organic and biological proxies studies, allows vital insights into the composition of early atmosphere–ocean-biosphere system, suggesting low atmospheric oxygen, high levels of greenhouse gases (CO2, CO, CH4 and likely H2S), oceanic anoxia and high acidity, limiting habitats to single-cell methanogenic and photosynthesizing autotrophs. Increases in atmospheric oxygen have been related to proliferation of phytoplankton in the oceans, likely about ~2.4 Ga (billion years-ago) and 0.7–0.6 Ga. |
URI: | http://10.6.20.12:80/handle/123456789/13923 |
ISBN: | 978-3-319-22512-8 |
Appears in Collections: | Archeology and Heritage Management |
Files in This Item:
File | Description | Size | Format | |
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46.pdf.pdf | 17.78 MB | Adobe PDF | View/Open |
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