Please use this identifier to cite or link to this item: 192.168.6.56/handle/123456789/13923
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dc.contributor.authorAndrew Y., Glikson-
dc.contributor.authorColin, Groves-
dc.date.accessioned2018-10-24T06:42:46Z-
dc.date.available2018-10-24T06:42:46Z-
dc.date.issued2016-
dc.identifier.isbn978-3-319-22512-8-
dc.identifier.urihttp://10.6.20.12:80/handle/123456789/13923-
dc.descriptionThe 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.en_US
dc.languageenen_US
dc.language.isoenen_US
dc.publisherSpringeren_US
dc.subjectThe Deep Time Dimensions of the Anthropoceneen_US
dc.titleClimate, Fire and Human Evolutionen_US
dc.title.alternativeThe Deep Time Dimensions of the Anthropoceneen_US
dc.typeBooken_US
Appears in Collections:Archeology and Heritage Management

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