Data report: X-ray fluorescence scanning of sediment cores, IODP Expedition 390/393 Site U1583, South Atlantic Transect

  • Adriane R. Lam*
  • , Chiara Amadori
  • , Chiara Borrelli
  • , Gail Christeson
  • , Emily Estes
  • , Laura Guertin
  • , Jennifer Hertzberg
  • , Michael R. Kaplan
  • , Ravi Kiran Koorapati
  • , Christopher M. Lowery
  • , Andrew McIntyre
  • , Julia S. Reece
  • , Claudio Robustelli Test
  • , Claire M. Routledge
  • , Patricia Standring
  • , Jason B. Sylvan
  • , Mary Thompson
  • , Alexandra Villa
  • , Yi Wang
  • , Shu Ying Wee
  • Trevor Williams, Jesse Yeon, Damon A.H. Teagle, Rosalind M. Coggon
*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

Abstract

The western South Atlantic Ocean has not been drilled since the end of the Deep Sea Drilling Program, leading to a dearth of sedimentary sequences available from this sector of the Atlantic Ocean. In 2020–2022, a transect of new sites was drilled during International Ocean Discovery Program Expeditions 390C, 395E, 390, and 393 at 31°S and spanning from 28.8°W to 15.2°W. Here, we use X-ray fluorescence data, combined with shipboard magnetic susceptibility and natural gamma radiation, to characterize the sediments below the oligotrophic South Atlantic Gyre at Site U1583. These geochemical data add to the otherwise understudied southwest Atlantic Ocean.

Original languageEnglish
JournalInternational Ocean Discovery Program: Preliminary Reports
Volume390-393
DOIs
Publication statusPublished - 5 Apr 2024
Externally publishedYes

ASJC Scopus subject areas

  • Oceanography

Keywords

  • Expedition 393
  • International Ocean Discovery Program
  • JOIDES Resolution
  • Miocene
  • Neogene
  • Oligocene
  • Pleistocene
  • Pliocene
  • Site U1583
  • South Atlantic Transect

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