Chemical Characteristics of Sediments and Seawater

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F13%3A00000002" target="_blank" >RIV/00025798:_____/13:00000002 - isvavai.cz</a>

Výsledek na webu

<a href="http://www.springerlink.com/content/tu470n7746262380/" target="_blank" >http://www.springerlink.com/content/tu470n7746262380/</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/978-3-642-29670-3_10" target="_blank" >10.1007/978-3-642-29670-3_10</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Chemical Characteristics of Sediments and Seawater

Popis výsledku v původním jazyce

The transition from an anoxic to oxygenated atmosphere was arguably the most dramatic change in the history of the Earth. This ?Great Oxidation Event? (Holland 2006) transformed the biogeochemical cycles of the elements by imposing an oxidative step in the cycles, creating strong redox gradients in the terrestrial and marine realms that energised microbial metabolism. Although much past research was focused on establishing when the rise of atmospheric oxygen took place, recognition that substantial mass-independent fraction (MIF) of the sulphur isotopes is restricted to the time interval before 2.45 Ga and requires an anoxic atmosphere (Farquhar et al. 2000, 2007; Mojzsis et al. 2003; Ono et al. 2003; Bekker et al. 2004) argues the atmosphere became permanently oxygenated at this time (Pavlov and Kasting 2002). A false-start to the modern aerobic biosphere and a ?whiff? of atmospheric oxygen (Anbar et al. 2007) may have occurred in the latest Archaean, as reflected in a transient enric

Název v anglickém jazyce

Chemical Characteristics of Sediments and Seawater

Popis výsledku anglicky

The transition from an anoxic to oxygenated atmosphere was arguably the most dramatic change in the history of the Earth. This ?Great Oxidation Event? (Holland 2006) transformed the biogeochemical cycles of the elements by imposing an oxidative step in the cycles, creating strong redox gradients in the terrestrial and marine realms that energised microbial metabolism. Although much past research was focused on establishing when the rise of atmospheric oxygen took place, recognition that substantial mass-independent fraction (MIF) of the sulphur isotopes is restricted to the time interval before 2.45 Ga and requires an anoxic atmosphere (Farquhar et al. 2000, 2007; Mojzsis et al. 2003; Ono et al. 2003; Bekker et al. 2004) argues the atmosphere became permanently oxygenated at this time (Pavlov and Kasting 2002). A false-start to the modern aerobic biosphere and a ?whiff? of atmospheric oxygen (Anbar et al. 2007) may have occurred in the latest Archaean, as reflected in a transient enric

Druh

C - Kapitola v odborné knize

CEP obor

DD - Geochemie

OECD FORD obor

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Projekt

<a href="/cs/project/GPP210%2F12%2FP631" target="_blank" >GPP210/12/P631: Izotopové složení hořčíku ve fanerozoických mořských karbonátech: Implikace pro chemickou evoluci mořské vody a vzniku masivních dolomitů</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2013

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název knihy nebo sborníku

Reading the Archive of Earth?s Oxygenation. Vol. 3 Global Events and the Fennoscandian Arctic Russia - Drilling Early Earth Project

ISBN

978-3-642-29669-7

Počet stran výsledku

57

Strana od-do

1457-1514

Počet stran knihy

528

Název nakladatele

Springer

Místo vydání

Berlin

Kód UT WoS kapitoly

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