(Table DR1) Abundance of benthonic foraminifera in sediments from ODP Hole 113-690

A mass extinction of deep-sea benthic foraminifera has been documented globally, coeval with the negative carbon isotope excursion (CIE) at the Paleocene-Eocene boundary, which was probably caused by dissociation of methane hydrate. A detailed record of benthic foraminiferal faunal change over ~30 k...

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Bibliographic Details
Main Author: Thomas, Ellen
Format: Dataset
Language:English
Published: PANGAEA 2003
Subjects:
113-690
Abyssamina poagi
Abyssamina quadrata
AGE
Alabamina creta
Anomalinoides cf. acutus
Anomalinoides rubiginosus
Anomalinoides spissiformis
Aragonia aragonensis
Aragonia sp.
Astacolus spp.
Bolivinita sp.
Bolivinoides cf. decoratus
Bolivinoides decoratus
Bolivinoides delicatulus
Bulimina kugleri
Bulimina midwayensis
Bulimina simplex
Bulimina thanetensis
Bulimina trinitatensis
Buliminella beaumonti
Calculated
Cibicides variabilis
Clinapertina subplanispira
COMPCORE
Composite Core
Coryphostoma sp.
Counting
Cyclammina sp.
DEPTH
sediment/rock
Dorothia oxycona
DSDP/ODP/IODP sample designation
Eilohedra weddellensis
Fishers alpha index of diversity
Foraminifera
benthic
uniserial
uniserial lagenids
Fursenkoina pauciloculata
Fursenkoina tegulata
Gaudryina pyramidata
Globobulimina sp.
Gravellina narivaensis
Gyroidinoides acutus
Gyroidinoides beisseli
Methane hydrate
Southern Ocean
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.724678
https://doi.org/10.1594/PANGAEA.724678

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