Autors de l'ICTA

Projectes relationats

Últims articles publicats

2015 What explains public support for climate policies? A review of empirical and experimental studies[disponible en anglès]

2015 Socially sustainable degrowth as a social–ecological transformation: repoliticizing sustainability[disponible en anglès]

2015 Bolivia set to violate its protected areas[disponible en anglès]

2015 What if solar energy becomes really cheap? A thought experiment on environmental problem shifting[disponible en anglès]

Field-based validation of a diagenetic effect on G. ruber Mg/Ca paleothermometry: Core top results from the Aegean Sea (eastern Mediterranean)

2011, GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS - número/volum 12 - DOI 10.1029/2011GC003692

Autors de l'ICTA:
Miguel Ángel Martínez Botí, P. Graham Mortyn

Tots els autors:
George Kontakiotis; P. Graham Mortyn; Assimina Antonarakou; Miguel A. Martínez-Botí; Maria V. Triantaphyllou

Referència:
www.agu.org/pubs/crossref/2011/2011GC003692.shtml

Abstract
Recent work across the Mediterranean Sea has illustrated the salinity and overgrowth effects on planktonic foraminiferal Mg/Ca, which potentially confound the use of this as a temperature proxy for paleoceanographic reconstructions. To test and verify these effects, we present new Aegean Sea results which reveal Mg/Ca values that were unreasonably high to be explained by temperature or salinity variations alone, confirming that foraminiferal Mg/Ca is affected by diagenesis. We have specifically targeted Globigerinoides ruber (w, sensu stricto), from a series of modern core tops spanning a strong sea surface salinity gradient and a minor sea surface temperature range, along a north-south Aegean Sea transect. Scanning Electron Microscopy analyses show that G. ruber specimens were covered by microscale euhedral crystallites of inorganic precipitates. This secondary calcite phase seems to be responsible for the anomalously high Mg/Ca ratios and likely formed near the sediment/water interface from CaCO3 supersaturated interstitial seawater. We also have clear evidence of diagenetic alteration in a north-south direction along the Aegean Sea, possibly depending on salinity and calcite saturation state gradients. These observations illustrate the necessity of alternative techniques (e.g., flow-through time resolved analysis or laser ablation inductively coupled plasma mass spectrometry) to potentially overcome these diagenetic issues and develop a more reliable and sensitive temperature proxy in similar subtropical settings characterized by high salinity, excessive evaporation, and restricted circulation.

Article

© 2008 ICTA - Universitat Autònoma de Barcelona - Tots els drets reservats