IODP Expedition 378 Magnetic susceptibility (point or contact system) ...

Magnetic susceptibility was measured on section halves on the Section Half Multisensor Logger (SHMSL) using a Bartington MS2 meter and either a MS2E or MS2K probe. Because all JRSO cores meet minimum size requirements for these two probes, MSPOINT data are corrected for volume and recorded in SI sus...

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Bibliographic Details
Main Authors: Röhl, Ursula, Thomas, Deborah J., Childress, Laurel B., Anagnostou, Eleni, Ausín, Blanca, Boscolo Galazzo, Flavia, Dias, Bruna Borba, Brzelinski, Swaantje, Dunlea, Ann G., George, Simon C., Haynes, Laura L., Hendy, Ingrid L., Jones, Heather L., Khanolkar, Sonal S., Kitch, Gabriella D., Lee, Hojun, Raffi, Isabella, Reis, Alex J., Sheward, Rosie M., Sibert, Elizabeth, Tanaka, Erika, Wilkens, Roy H., Yasukawa, Kazutaka, Yuan, Wei, Zhang, Qiang, Zhang, Yang, Drury, Anna J., Hollis, Christopher J.
Format: Dataset
Language:unknown
Published: International Ocean Discovery Program 2022
Subjects:
International Ocean Discovery Program
IODP
JOIDES Resolution
Expedition 378
Site U1553
South Pacific Paleogene Climate
climate and ocean change
Campbell Plateau
high southern latitude
carbon system dynamics
Cenozoic climate history
high CO2 world
chronostratigraphy
ocean circulation
intermediate water formation
hydrologic cycling
biological productivity
ice sheet dynamics
Ice Sheet
Online Access:https://dx.doi.org/10.5281/zenodo.10809984
https://zenodo.org/doi/10.5281/zenodo.10809984
Description
Summary:Magnetic susceptibility was measured on section halves on the Section Half Multisensor Logger (SHMSL) using a Bartington MS2 meter and either a MS2E or MS2K probe. Because all JRSO cores meet minimum size requirements for these two probes, MSPOINT data are corrected for volume and recorded in SI susceptibility units (x10-5). ...

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