Project Details
Projekt Print View

Atypische tropische Karbonate als Klima-Archive

Subject Area Palaeontology
Term from 2005 to 2010
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 5452403
 
Final Report Year 2011

Final Report Abstract

The present study has strongly changed the understanding of carbonate production controls under eutrophic conditions. These findings have implications for the paleotemperature and paleodimatic interpretations of heterozoan carbonates. The main conclusions are: - The complex sediment distribution of the Golfe d'Arguin (N Mauritania) results from an important sediment reworking and transport that are primarily controlled by hydrological patterns such as the swell and wind-driven currents. - The modem sedimentation of the northern Mauritanian shelf shows that heterozoan carbonates not only form in cool and cold waters but are produced under eutrophic tropical marine environments. This outcome differs from classical carbonate grain association models based on water temperature. - Taxonomy and ecology are the keys to interpret the paleoenvironments of heterozoan carbonate production. Heterozoan carbonate associations yield a wealth of multiparameter environmental information that needs to be included into meaningful paleoenvironmental interpretation. While this finding is far from being new, it has gained new significance on the background of the common practice of focusing on temperature interpretations.

Publications

 
 

Additional Information

Textvergrößerung und Kontrastanpassung