eprintid: 19427
rev_number: 2
eprint_status: archive
userid: 1
dir: disk0/00/01/94/27
datestamp: 2024-06-04 14:11:53
lastmod: 2024-06-04 14:11:53
status_changed: 2024-06-04 14:05:42
type: article
metadata_visibility: show
creators_name: Lunt, P.
title: BIOLOGICAL EVOLUTION OF SOUTHEAST ASIAN CARBONATES, BASED ON THEIR MICROFOSSIL CONTENT
ispublished: pub
note: cited By 6
abstract: A new compilation of data suggests aragonitic coral reefs were already common in Southeast Asia by the mid-Oligocene. A gradual change from calcite to aragonite seas through the Oligocene and early Miocene appears to be related to a gradual expansion of the importance of scleractinia, along with green algae and mollusks, and an associated decline in the abundance of calcitic larger foraminifera. The larger foraminifera had been important rock-forming bioclasts in the early part of the early Miocene, but were a minor component of carbonate faunas by the end of the middle Miocene. This gradual decline in abundance included a few extinction events that reduced diversity, and these extinctions appear to correlate with periods of tectonic change. The K-selection evolutionary pressure impacted carbonate facies, but foraminifera maintained their taxonomic diversity until the abrupt faunal extinctions. Changes in sea-surface temperature, or the regional change from seasonal to ever-wet climate, do not appear to have impacted larger foraminiferal diversity or caused extinctions, only modified their latitudinal range. Some extinction events can be recognized across the whole Tethys Ocean, as can some of the times of tectonic activity and possible climate change. These correlations tentatively point to a link between large-scale changes in plate motion, oceanography, and foraminiferal extinctions. In contrast, the change from seasonal to ever-wet conditions around the Oligo�Miocene boundary around the South China Sea does not appear to have been caused by a wider tectonic event, and this event does not impact larger foraminifera diversity. A combined tectonic unconformity and mass extinction of larger foraminifera in middle middle Miocene times might have been due to the plate tectonic constriction of a throughflow between the Pacific and Indian Oceans. © 2023 SEPM Society for Sedimentary Geology. All rights reserved.
date: 2023
publisher: SEPM Society for Sedimentary Geology
official_url: https://www.scopus.com/inward/record.uri?eid=2-s2.0-85143727053&doi=10.2110%2fsepmsp.114.07&partnerID=40&md5=fe1bf1ec17f120f1b8ff79cd9792c5f1
id_number: 10.2110/sepmsp.114.07
full_text_status: none
publication: SEPM Special Publications
volume: 2023
number: 114
pagerange: 70-84
refereed: TRUE
issn: 1060071X
citation:   Lunt, P.  (2023) BIOLOGICAL EVOLUTION OF SOUTHEAST ASIAN CARBONATES, BASED ON THEIR MICROFOSSIL CONTENT.  SEPM Special Publications, 2023 (114).  pp. 70-84.  ISSN 1060071X