IMIS

Publications | Institutes | Persons | Datasets | Projects | Maps
[ report an error in this record ]basket (0): add | show Print this page

A global transition to ferruginous conditions in the early Neoproterozoic oceans
Guilbaud, R.; Poulton, S.W.; Butterfield, N.J.; Zhu, M.; Shields-Zhou, G. (2015). A global transition to ferruginous conditions in the early Neoproterozoic oceans. Nature Geoscience 8(6): 466–470. http://dx.doi.org/10.1038/ngeo2434
In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894; e-ISSN 1752-0908, more
Peer reviewed article  

Available in  Authors 

Keyword
    Marine/Coastal

Authors  Top 
  • Guilbaud, R.
  • Poulton, S.W.
  • Butterfield, N.J.
  • Zhu, M.
  • Shields-Zhou, G.

Abstract
    Deeper ocean waters were anoxic during the Neoproterozoic. Geochemical data suggest a transition from sulphidic to iron-rich mid-depth waters about one billion years ago, coincident with increased iron influx from the supercontinent Rodinia.

All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy Top | Authors