eprintid: 14271
rev_number: 2
eprint_status: archive
userid: 1
dir: disk0/00/01/42/71
datestamp: 2023-11-10 03:28:50
lastmod: 2023-11-10 03:28:50
status_changed: 2023-11-10 01:56:28
type: article
metadata_visibility: show
creators_name: Coxall, H.K.
creators_name: Jones, T.D.
creators_name: Jones, A.P.
creators_name: Lunt, P.
creators_name: Macmillan, I.
creators_name: Marliyani, G.I.
creators_name: Nicholas, C.J.
creators_name: O�halloran, A.
creators_name: Piga, E.
creators_name: Sanyoto, P.
creators_name: Rahardjo, W.
creators_name: Pearson, P.N.
title: The eocene�oligocene transition in nanggulan, java: Lithostratigraphy, biostratigraphy and foraminiferal stable isotopes
ispublished: pub
keywords: Boreholes; Isotopes; Stratigraphy; Submarine geology, Continental scale; Lithostratigraphy; Marine sediments; Microfossils; Oligocene; Sediment deposits; Stable isotopes; Sunda arc; Time interval; Volcanic deposits, Glacial geology, biostratigraphy; foraminifera; lithostratigraphy; marine sediment; microfossil; reconstruction; stable isotope; volcaniclastic deposit; volcanism, Greater Sunda Islands; Java; Sunda Isles, Foraminifera
note: cited By 2
abstract: The Nanggulan section in south central Java comprises open marine sediments and volcanic deposits of Eocene� Oligocene age that accumulated in a marginal basin within the young Sunda Arc complex. A new borehole captures the stratigraphy and showcases the exceptional preservation of calcareous microfossils across an apparently complete Eocene� Oligocene Transition (EOT), a time interval significant for the initiation of continental-scale glaciation on Antarctica. Low-resolution benthic and planktonic foraminifera oxygen and carbon stable isotopes (δ18O and δ13C) record increasing δ18O and δ13 C in the basal Oligocene, allowing correlation to global records. Isotopic values imply warm temperatures and relatively high nutrients along the SE Java margin. The Nanggulan EOT is a valuable archive for reconstructing ocean�climate behaviour and plankton evolution and extinction in the Indo-Pacific Warm Pool. The borehole also adds to understanding of the early stages of Sunda Arc volcanism. © 2021 The Author(s).
date: 2021
publisher: Geological Society of London
official_url: https://www.scopus.com/inward/record.uri?eid=2-s2.0-85120726445&doi=10.1144%2fjgs2021-006&partnerID=40&md5=1fb4b03246f1acd9e83fd91c39eb7626
id_number: 10.1144/jgs2021-006
full_text_status: none
publication: Journal of the Geological Society
volume: 178
number: 6
refereed: TRUE
issn: 00167649
citation:   Coxall, H.K. and Jones, T.D. and Jones, A.P. and Lunt, P. and Macmillan, I. and Marliyani, G.I. and Nicholas, C.J. and O�halloran, A. and Piga, E. and Sanyoto, P. and Rahardjo, W. and Pearson, P.N.  (2021) The eocene�oligocene transition in nanggulan, java: Lithostratigraphy, biostratigraphy and foraminiferal stable isotopes.  Journal of the Geological Society, 178 (6).   ISSN 00167649