All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

Chemical Characteristics of Sediments and Seawater

The result's identifiers

  • Result code in 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>

  • Result on the web

    <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>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Chemical Characteristics of Sediments and Seawater

  • Original language description

    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

  • Czech name

  • Czech description

Classification

  • Type

    C - Chapter in a specialist book

  • CEP classification

    DD - Geochemistry

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GPP210%2F12%2FP631" target="_blank" >GPP210/12/P631: Magnesium isotope record of Phanerozoic marine carbonates: Implications for chemical evolution of seawater and the formation of massive dolomites</a><br>

  • Continuities

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

Others

  • Publication year

    2013

  • Confidentiality

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

Data specific for result type

  • Book/collection name

    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

  • Number of pages of the result

    57

  • Pages from-to

    1457-1514

  • Number of pages of the book

    528

  • Publisher name

    Springer

  • Place of publication

    Berlin

  • UT code for WoS chapter