Late Maastrichtian-early Paleocene iron (Fe) intensity data from ODP Site 208-1262, South Atlantic

DOI

Iron (Fe) intensity records measured by X-Ray Fluorescence (XRF) from ODP Site 1262 (Walvis Ridge, South Atlantic) covering the late Maastrichtian to early Paleocene (65.6 to 67.1 Ma). These data were measured between 2004 and 2007 and compiled to assess the magnitude of calcium carbonate dissolution at ODP Site 1262 during the Late Maastrichtian warming event and K/Pg boundary interval, since Fe is a proxy for clay content in the sediment.

Identifier
DOI https://doi.pangaea.de/10.1594/PANGAEA.973511
Related Identifier References https://doi.org/10.1130/G39771.1
Related Identifier References https://doi.org/10.2973/odp.proc.sr.165.009.2000
Related Identifier References https://doi.org/10.1016/j.palaeo.2007.09.016
Related Identifier References https://doi.org/10.1594/PANGAEA.666119
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.973511
Provenance
Creator Barnet, James S K ORCID logo; Littler, Kate; Kroon, Dick; Leng, Melanie J ORCID logo; Westerhold, Thomas ORCID logo; Röhl, Ursula ORCID logo; Zachos, James C ORCID logo
Publisher PANGAEA
Publication Year 2024
Funding Reference NERC Isotope Geosciences Laboratory, Keyworth https://doi.org/10.13039/501100000270 Crossref Funder ID IP-1581–1115 Late Maastrichtian warming event
Rights Creative Commons Attribution 4.0 International; Data access is restricted (moratorium, sensitive data, license constraints); https://creativecommons.org/licenses/by/4.0/
OpenAccess false
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 3069 data points
Discipline Earth System Research
Spatial Coverage (1.577 LON, -27.186 LAT); Walvis Ridge, Southeast Atlantic Ocean
Temporal Coverage Begin 2003-03-24T00:00:00Z
Temporal Coverage End 2003-03-29T00:00:00Z