Oxygen and carbon isotopic composition of Quaternary meteoric carbonates from western and southern Europe: their role in palaoenvironmental reconstruction

1.00
Hdl Handle:
http://hdl.handle.net/10545/292367
Title:
Oxygen and carbon isotopic composition of Quaternary meteoric carbonates from western and southern Europe: their role in palaoenvironmental reconstruction
Authors:
Candy, I.; Adamson, K.; Gallant, C.E.; Whitfield, E.; Pope, Richard J. J.
Abstract:
The relationship between environmental conditions and the δ18O and δ13C values of soil and groundwater carbonates in Europe is poorly understood. Consequently, the use of the isotopic composition of these carbonate palaeoclimatic indicators in European sedimentary sequences is restricted. In this study we examine the δ18O and δ13C values of soil and groundwater carbonates from western and southern Europe. In western Europe there is no relationship between carbonate δ18O values and carbonate δ13C values. The δ18O values of soil carbonate appears to be driven by temperature, whilst the δ13C value of soil and groundwater carbonate reflects the persistent dominance of C3 vegetation in this region during the Quaternary. The δ18O and δ13C values of soil carbonates from Spain and Crete show a strong degree of co-variance suggesting that they are being controlled by the same environmental factor. This is suggested to be aridity. δ18O values are controlled by soil moisture evaporation whilst δ13C value is controlled by soil moisture degassing, vegetation abundance and possible C3/C4 vegetation inputs. The paper concludes by highlighting the fact that, although currently under-utilised, the δ18O and δ13C values of soil and groundwater carbonates have a huge potential for providing important palaeoenvironmental information from sites across Europe.
Affiliation:
University of Manchester; University of London, Royal Holloway; Liverpool John Moores University; University of Derby
Journal:
Palaeogeography, Palaeoclimatology, Palaeoecology
Issue Date:
20-May-2013
URI:
http://hdl.handle.net/10545/292367
DOI:
10.1016/j.palaeo.2011.12.017
Additional Links:
http://linkinghub.elsevier.com/retrieve/pii/S0031018211006092
Type:
Article
Language:
en
Description:
Oxygen and carbon isotopic composition of Quaternary meteoric carbonates from western and southern Europe: Their role in palaoenvironmental reconstruction
ISSN:
00310182
Appears in Collections:
Human & Physical Environments Research Group

Full metadata record

DC FieldValue Language
dc.contributor.authorCandy, I.en_GB
dc.contributor.authorAdamson, K.en_GB
dc.contributor.authorGallant, C.E.en_GB
dc.contributor.authorWhitfield, E.en_GB
dc.contributor.authorPope, Richard J. J.en_GB
dc.date.accessioned2013-05-20T11:08:59Z-
dc.date.available2013-05-20T11:08:59Z-
dc.date.issued2013-05-20-
dc.identifier.issn00310182-
dc.identifier.doi10.1016/j.palaeo.2011.12.017-
dc.identifier.urihttp://hdl.handle.net/10545/292367-
dc.descriptionOxygen and carbon isotopic composition of Quaternary meteoric carbonates from western and southern Europe: Their role in palaoenvironmental reconstructionen_GB
dc.description.abstractThe relationship between environmental conditions and the δ18O and δ13C values of soil and groundwater carbonates in Europe is poorly understood. Consequently, the use of the isotopic composition of these carbonate palaeoclimatic indicators in European sedimentary sequences is restricted. In this study we examine the δ18O and δ13C values of soil and groundwater carbonates from western and southern Europe. In western Europe there is no relationship between carbonate δ18O values and carbonate δ13C values. The δ18O values of soil carbonate appears to be driven by temperature, whilst the δ13C value of soil and groundwater carbonate reflects the persistent dominance of C3 vegetation in this region during the Quaternary. The δ18O and δ13C values of soil carbonates from Spain and Crete show a strong degree of co-variance suggesting that they are being controlled by the same environmental factor. This is suggested to be aridity. δ18O values are controlled by soil moisture evaporation whilst δ13C value is controlled by soil moisture degassing, vegetation abundance and possible C3/C4 vegetation inputs. The paper concludes by highlighting the fact that, although currently under-utilised, the δ18O and δ13C values of soil and groundwater carbonates have a huge potential for providing important palaeoenvironmental information from sites across Europe.en_GB
dc.language.isoenen
dc.relation.urlhttp://linkinghub.elsevier.com/retrieve/pii/S0031018211006092en_GB
dc.rightsArchived with thanks to Palaeogeography, Palaeoclimatology, Palaeoecologyen_GB
dc.subjectOxygen isotopeen_GB
dc.subjectCarbon isotopeen_GB
dc.subjectQuaternary meteoric carbonatesen_GB
dc.subjectPalaoenvironmental reconstructionen_GB
dc.titleOxygen and carbon isotopic composition of Quaternary meteoric carbonates from western and southern Europe: their role in palaoenvironmental reconstructionen
dc.typeArticleen
dc.contributor.departmentUniversity of Manchesteren_GB
dc.contributor.departmentUniversity of London, Royal Hollowayen_GB
dc.contributor.departmentLiverpool John Moores Universityen_GB
dc.contributor.departmentUniversity of Derbyen_GB
dc.identifier.journalPalaeogeography, Palaeoclimatology, Palaeoecologyen_GB
This item is licensed under a Creative Commons License
Creative Commons
All Items in UDORA are protected by copyright, with all rights reserved, unless otherwise indicated.