Opal contents of sediment core GeoB16202-2

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Cite this as

Mulitza, Stefan, Chiessi, Cristiano Mazur, Schefuß, Enno, Lippold, Jörg, Wichmann, David, Antz, Benny, Mackensen, Andreas, Paul, André, Prange, Matthias, Rehfeld, Kira, Werner, Martin, Bickert, Torsten, Frank, Norbert, Kuhnert, Henning, Lynch-Stieglitz, Jean, Portilho-Ramos, Rodrigo Costa, Sawakuchi, André Oliveira, Schulz, Michael, Schwenk, Tilmann, Tiedemann, Ralf, Vahlenkamp, Maximilian, Zhang, Yancheng (2017). Dataset: Opal contents of sediment core GeoB16202-2. https://doi.org/10.1594/PANGAEA.877698

DOI retrieved: 2017

Additional Info

Field Value
Imported on November 30, 2024
Last update November 30, 2024
License CC-BY-3.0
Source https://doi.org/10.1594/PANGAEA.877698
Author Mulitza, Stefan
Given Name Stefan
Family Name Mulitza
More Authors
Chiessi, Cristiano Mazur
Schefuß, Enno
Lippold, Jörg
Wichmann, David
Antz, Benny
Mackensen, Andreas
Paul, André
Prange, Matthias
Rehfeld, Kira
Werner, Martin
Bickert, Torsten
Frank, Norbert
Kuhnert, Henning
Lynch-Stieglitz, Jean
Portilho-Ramos, Rodrigo Costa
Sawakuchi, André Oliveira
Schulz, Michael
Schwenk, Tilmann
Tiedemann, Ralf
Vahlenkamp, Maximilian
Zhang, Yancheng
Source Creation 2017
Publication Year 2017
Resource Type text/tab-separated-values - filename: GeoB16202-2_opal
Subject Areas
Name: Lithosphere

Name: Oceans

Name: Paleontology

Related Identifiers
Title: Synchronous and proportional deglacial changes in Atlantic meridional overturning and northeast Brazilian precipitation
Identifier: https://doi.org/10.1002/2017PA003084
Type: DOI
Relation: References
Year: 2017
Source: Paleoceanography
Authors: Mulitza Stefan , Schefuß Enno , Chiessi Cristiano Mazur , Lippold Jörg , Wichmann David , Antz Benny , Mackensen Andreas , Paul André , Prange Matthias , Rehfeld Kira , Werner Martin , Bickert Torsten , Frank Norbert , Kuhnert Henning , Lynch-Stieglitz Jean , Portilho-Ramos Rodrigo Costa , Sawakuchi André Oliveira , Schulz Michael , Schwenk Tilmann , Tiedemann Ralf , Vahlenkamp Maximilian , Zhang Yancheng .