Aulotortus friedli from the Upper Triassic gravitational flow deposits of the Kumagawa River (Kyushu, Southwest Japan)

Jerome Chablais, Rossana Martini, Tetsuji Onoue

Research output: Contribution to journalArticle

9 Citations (Scopus)

Abstract

The benthic foraminifer Aulotortus friedli is reported from the Upper Triassic carbonates (capped seamount) of the Sambosan Accretionary Complex in Kyushu, Southwest Japan. Specimens were collected from shallow-water limestone clasts in a debris flow sequence near the Ose locality along the Kumagawa River. The limestone clasts mainly represent shoal facies where the benthic foraminifer is extremely abundant. Because of the remarkable preservation of the Japanese specimens, they allow further description of the involutinid A. friedli. In addition, a detailed sedimentary and environmental analysis of the gravitational deposits where A. friedli occurs is given. Using microfacies analysis together with the biostratigraphic range of A. friedli and associated foraminifers, a new interpretation is proposed of a seamount collapse process that occurred during the Norian-Rhaetian and preceded the major collapse event of the Sambosan seamount, which has been placed in the Middle to Late Jurassic.

Original languageEnglish
Pages (from-to)151-160
Number of pages10
JournalPaleontological Research
Volume14
Issue number2
DOIs
Publication statusPublished - Jan 1 2010

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seamount
Triassic
Japan
benthic foraminifera
limestone
clast
rivers
river
Rhaetian
Norian
microfacies
environmental assessment
debris flow
foraminifera
carbonates
shallow water
Jurassic
carbonate
Retaria
water

All Science Journal Classification (ASJC) codes

  • Ecology, Evolution, Behavior and Systematics
  • Palaeontology

Cite this

Aulotortus friedli from the Upper Triassic gravitational flow deposits of the Kumagawa River (Kyushu, Southwest Japan). / Chablais, Jerome; Martini, Rossana; Onoue, Tetsuji.

In: Paleontological Research, Vol. 14, No. 2, 01.01.2010, p. 151-160.

Research output: Contribution to journalArticle

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