Middle to Late Pleistocene organic carbon and uranium content, nannofossil abundances and age model from IODP Site 356-U1460

Fuente: PANGAEA
Enregistré dans:
Détails bibliographiques
Auteurs principaux: Auer, Gerald, Petrick, Benjamin F, Yoshimura, Toshihiro, Mamo, Briony L, Reuning, Lars, Takayanagi, Hideko, De Vleeschouwer, David, Martínez-García, Alfredo
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2021
Sujets:
Accès en ligne:
Tags: Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
_version_ 1867171375350808576
author Auer, Gerald
Petrick, Benjamin F
Yoshimura, Toshihiro
Mamo, Briony L
Reuning, Lars
Takayanagi, Hideko
De Vleeschouwer, David
Martínez-García, Alfredo
author_facet Auer, Gerald
Petrick, Benjamin F
Yoshimura, Toshihiro
Mamo, Briony L
Reuning, Lars
Takayanagi, Hideko
De Vleeschouwer, David
Martínez-García, Alfredo
collection Datos científicos de ciencias marinas y ambientales
contents Here we present records of International Ocean Discovery Program (IODP) Site U1460 (eastern Indian Ocean, 27°22.49′S, 112°55.42′E), including surface water productivity (alkenone abundances, total nannofossil as well as alkenone producing nannofossil abundances and accumulation rates), as well as relative abundances of small Gephyrocapsa spp. and Reticulofenestra asanoi, which were used in age model generation. Furthermore, we provide organic matter flux (total organic carbon and Uranium content and mass accumulation rates), as well as biogenic silica and terrigenous flux records in combination with bulk calcite equivalent calcium carbonate content. Absolute and relative Nannofossil data was generated using the drop technique (c.f. Bordiga et al., 2015, doi: 10.1016/j.revmic.2015.05.002), with mass accumulation rates calculated based on the attached age model. Bulk total and organic carbon content measured in a LECO CS300 carbonate and sulfur analyzer and calculated mass accumulation rates of organic carbon and the calcite equivalent carbonate content. Alkenone abundances and calculated accumulation rates are derived from data originally measured for Petrick et al. (2019, doi: 10.1038/s41598-019-53382-0). Shipboard whole round multi-senor logger natural gamma radiation derived U content (see De Vleeschouwer et al., 2017, doi:10.1002/2016gc0067159) and calculated U mass accumulation rates. X-ray fluorescence (XRF) derived element counts originally published in Petrick et al. (2019, doi: 10.1038/s41598-019-53382-0) are used to calculate log normalized multi-element ratios ln((Al+K)/Ca) and ln(Si/(Al+Ca)). The gathered proxy data covers the interval between 61 and 163 m CSF-A, corresponding to an age of 1.1 – 0.6 Ma, based on the attached age model. The data records Pleistocene Leeuwin Current dynamics and sea level-driven environmental changes along the West Australian shelf over the MPT.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_928015
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Middle to Late Pleistocene organic carbon and uranium content, nannofossil abundances and age model from IODP Site 356-U1460
Auer, Gerald
Petrick, Benjamin F
Yoshimura, Toshihiro
Mamo, Briony L
Reuning, Lars
Takayanagi, Hideko
De Vleeschouwer, David
Martínez-García, Alfredo
Calcium carbonate; Indian Ocean; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Middle Pleistocene Transition; Organic carbon; U1460
Here we present records of International Ocean Discovery Program (IODP) Site U1460 (eastern Indian Ocean, 27°22.49′S, 112°55.42′E), including surface water productivity (alkenone abundances, total nannofossil as well as alkenone producing nannofossil abundances and accumulation rates), as well as relative abundances of small Gephyrocapsa spp. and Reticulofenestra asanoi, which were used in age model generation. Furthermore, we provide organic matter flux (total organic carbon and Uranium content and mass accumulation rates), as well as biogenic silica and terrigenous flux records in combination with bulk calcite equivalent calcium carbonate content. Absolute and relative Nannofossil data was generated using the drop technique (c.f. Bordiga et al., 2015, doi: 10.1016/j.revmic.2015.05.002), with mass accumulation rates calculated based on the attached age model. Bulk total and organic carbon content measured in a LECO CS300 carbonate and sulfur analyzer and calculated mass accumulation rates of organic carbon and the calcite equivalent carbonate content. Alkenone abundances and calculated accumulation rates are derived from data originally measured for Petrick et al. (2019, doi: 10.1038/s41598-019-53382-0). Shipboard whole round multi-senor logger natural gamma radiation derived U content (see De Vleeschouwer et al., 2017, doi:10.1002/2016gc0067159) and calculated U mass accumulation rates. X-ray fluorescence (XRF) derived element counts originally published in Petrick et al. (2019, doi: 10.1038/s41598-019-53382-0) are used to calculate log normalized multi-element ratios ln((Al+K)/Ca) and ln(Si/(Al+Ca)). The gathered proxy data covers the interval between 61 and 163 m CSF-A, corresponding to an age of 1.1 – 0.6 Ma, based on the attached age model. The data records Pleistocene Leeuwin Current dynamics and sea level-driven environmental changes along the West Australian shelf over the MPT.
title Middle to Late Pleistocene organic carbon and uranium content, nannofossil abundances and age model from IODP Site 356-U1460
topic Calcium carbonate; Indian Ocean; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Middle Pleistocene Transition; Organic carbon; U1460
url https://doi.org/10.1594/PANGAEA.928015