(Table T4) Ages of the magnetic reversals for ODP Site 202-1237


Note that the age models according to Lourens et al. (2004), Shackleton et al. (1995) and Cande and Kent (1995) do not differentiate between top, mean and base of reversal boundary. Sediment depth in mcd. The reversals were determined at sections that did not belong to the mcd splice. Using core logging data, these sections were more precisely matched to the mcd splice.

DOI https://doi.org/10.1594/PANGAEA.773998
Related Identifier IsPartOf https://doi.org/10.1594/PANGAEA.774009
Related Identifier References https://doi.org/10.2973/odp.proc.ir.202.2003
Related Identifier References https://doi.org/10.1029/95PA01454
Related Identifier References https://doi.org/10.2973/odp.proc.sr.202.210.2007
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.773998
Creator Tiedemann, Ralf ORCID logo; Sturm, Arne; Steph, Silke; Lund, Steven P; Stoner, Joseph S ORCID logo
Publisher PANGAEA
Publication Year 2007
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Resource Type Dataset
Format text/tab-separated-values
Size 222 data points
Discipline Earth System Research
Spatial Coverage (-76.378 LON, -16.007 LAT); South Pacific Ocean