English
 
Help Privacy Policy Disclaimer
  Advanced SearchBrowse

Item

ITEM ACTIONSEXPORT
  Ostracod shell chemistry as proxy for paleoenvironmental change

Börner, N., De Baere, B., Yang, Q. C., Jochum, K. P., Frenzel, P., Andreae, M. O., et al. (2013). Ostracod shell chemistry as proxy for paleoenvironmental change. Quaternary International, 313, 17-37.

Item is

Files

show Files

Locators

show

Creators

show
hide
 Creators:
Börner, N., Author
De Baere, B., Author
Yang, Q. C., Author
Jochum, K. P.1, Author           
Frenzel, P., Author
Andreae, M. O.1, Author           
Schwalb, A., Author
Affiliations:
1Biogeochemistry, Max Planck Institute for Chemistry, Max Planck Society, ou_1826286              

Content

show
hide
Free keywords: -
 Abstract: The application of ostracod shell chemistry as a paleoenvironmental tool has grown within the past decades. Most studies have investigated Mg and Sr in ostracod shells as proxies for temperature and salinity, and the use of a wide range of trace elements as prospective paleoenvironmental indicators has yet to be developed for lacustrine systems. Only a few preliminary studies have used trace metals in paleolimnological studies such as Cd, Ba and Zn as paleonutrient indicators, or Mn, Fe and U as redox and oxygenation indicators. This paper reviews the state of the art of geochemical analyses in microfossils such as ostracods, foraminifera, and corals, and provides insights in new trace element proxies with the goal to promote the use of trace elements in ostracod shells as paleoenvironmental proxies. In paleoceanography, foraminifera and corals are most prominently used to reconstruct past climate conditions. Well-established proxies such as delta O-18, Mg/Ca and Sr/Ca provide information about changes in sea surface temperatures. In addition, a great number of new proxies have been developed recently, such as radiogenic isotopes and redox sensitive trace elements. In paleolimnology, ostracod shell chemistry is widely used to assess paleohydrological changes. Reconstruction of temperature and salinity changes in lake environments is often achieved by oxygen isotopes as well as Mg/Ca and Sr/Ca ratios, but depending on the hydrological and geological settings of the lake system, local calibrations are needed to assess which proxy is suited to reflect which processes. New proxies need to be tested by novel techniques that recently have become available. Compared to conventional instrumentation used in ostracod shell chemistry, methods such as Laser Ablation ICP-MS and NanoSIMS allow single shell analysis and provide high-resolution data. The potential of ostracods in paleolimnology is not yet fully assessed, but can be developed by learning from paleoceanographic studies. (C) 2013 Elsevier Ltd and INQUA. All rights reserved.

Details

show
hide
Language(s): eng - English
 Dates: 2013-11-05
 Publication Status: Issued
 Pages: -
 Publishing info: -
 Table of Contents: -
 Rev. Type: Internal
 Identifiers: eDoc: 675631
ISI: 000327171200003
 Degree: -

Event

show

Legal Case

show

Project information

show

Source 1

show
hide
Title: Quaternary International
Source Genre: Journal
 Creator(s):
Affiliations:
Publ. Info: -
Pages: - Volume / Issue: 313 Sequence Number: - Start / End Page: 17 - 37 Identifier: ISSN: 1040-6182