Reconstruction of Middle to Late Quaternary sea level using submerged speleothems from the northeastern Yucatán Peninsula-Reference-Cited by-同舟云学术

Reconstruction of Middle to Late Quaternary sea level using submerged speleothems from the northeastern Yucatán Peninsula

Published:2021-08-31 Issue:7 Volume:36 Page:1190-1200
ISSN:0267-8179
Container-title:Journal of Quaternary Science
language:en
Short-container-title:J. Quaternary Sci

Author:

Steidle Simon D.¹²^ORCID,Warken Sophie F.¹³^ORCID,Schorndorf Nils¹³^ORCID,Förstel Julius¹,Schröder‐Ritzrau Andrea¹^ORCID,Moseley Gina E.²^ORCID,Spötl Christoph²^ORCID,Aviles Jeronimo⁴⁵,Stinnesbeck Wolfgang³⁶^ORCID,Frank Norbert¹³^ORCID

Affiliation:

1. Institute of Environmental Physics Heidelberg University Heidelberg Germany

2. Institute of Geology University of Innsbruck Innsbruck Austria

3. Institute of Earth Science Heidelberg University Heidelberg Germany

4. Instituto de la Prehistoria de América Solidaridad Mexico

5. Museo del Desierto Saltillo Mexico

6. Universidad Autónoma de Coahuila, Centro en Geociencias Aplicadas Nueva Rosita Mexico

Funder

Deutsche Forschungsgemeinschaft

Bundesministerium für Bildung und Forschung

Publisher

Wiley

Subject

Paleontology,Earth and Planetary Sciences (miscellaneous),Arts and Humanities (miscellaneous)

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3365

Reference66 articles.

1. 215-ka History of sea-level oscillations from marine and continental layers in Argentarola Cave speleothems (Italy)

2. ArpsJ.2017. Towards epsilon‐Precision of U‐series Age Determinations of Secondary Carbonates.University of Heidelberg Germany PhD thesis.

3. Differential dissolution of a Pleistocene reef in the ground-water mixing zone of coastal Yucatan, Mexico

4. Review: The Yucatán Peninsula karst aquifer, Mexico

5. Decoupled fresh–saline groundwater circulation of a coastal carbonate aquifer: Spatial patterns of temperature and specific electrical conductivity

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