The paleocene of iodpsite u1511, tasman sea: Alagerstätte deposit for deep-water agglutinated foraminifera

  • Michael A. Kaminski*
  • , Laia Alegret
  • , Syouma Hikmahtiar
  • , Anna Waskowska
  • *Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

16 Scopus citations

Abstract

Deep-water agglutinated Foraminifera (DWAF) are investigated from Paleocene sediments recovered from IODP Hole U1511B in the northeastern Tasman Sea. The recovered foraminifera display exceptional three-dimensional preservation: They are relatively unaltered by sediment diagenesis and compaction.We examined 27 samples fromCores U1511B-45R to -47R, and recovered over 70 species of DWAF. The assemblage consists entirely of "cosmopolitan" forms originally described from the Carpathians, Caucasus, Trinidad, and the western Tethys, implying that there is no provinciality among DWAF faunas in the world ocean.

Original languageEnglish
Pages (from-to)341-364
Number of pages24
JournalMicropaleontology
Volume67
Issue number4
DOIs
StatePublished - 2021

Bibliographical note

Publisher Copyright:
© 2021 Micropaleontology Press. All rights reserved.

Keywords

  • Foraminifera
  • Lagerstätte
  • Paleocene
  • Tasman Sea

ASJC Scopus subject areas

  • Paleontology

Fingerprint

Dive into the research topics of 'The paleocene of iodpsite u1511, tasman sea: Alagerstätte deposit for deep-water agglutinated foraminifera'. Together they form a unique fingerprint.

Cite this