Reconstruction of Mesozoic Ocean Plate Stratigraphy and biogenic silica history in the high-latitude southern Panthalassa Ocean
Project/Area Number |
23540528
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Research Category |
Grant-in-Aid for Scientific Research (C)
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Allocation Type | Multi-year Fund |
Section | 一般 |
Research Field |
Geology
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Research Institution | Utsunomiya University |
Principal Investigator |
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Research Collaborator |
BERNHARD Spörli K. University of Auckland, 博士
GRANT-MACKIE J. A. University of Auckland, 博士
CAMPBELL H. J. GNS Science, Campbell
|
Project Period (FY) |
2011 – 2013
|
Project Status |
Completed (Fiscal Year 2013)
|
Budget Amount *help |
¥4,940,000 (Direct Cost: ¥3,800,000、Indirect Cost: ¥1,140,000)
Fiscal Year 2013: ¥910,000 (Direct Cost: ¥700,000、Indirect Cost: ¥210,000)
Fiscal Year 2012: ¥1,430,000 (Direct Cost: ¥1,100,000、Indirect Cost: ¥330,000)
Fiscal Year 2011: ¥2,600,000 (Direct Cost: ¥2,000,000、Indirect Cost: ¥600,000)
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Keywords | 海洋プレート層序 / パンサラサ海 / 高緯度帯 / 三畳紀 / 層状チャート / 生物源シリカ / 堆積相 / 放散虫化石 / ニュージーランド / 三畳紀中期 / 赤色層状チャート / モツタプ島 / 堆積相区分 / 海綿骨針や放散虫殻の密集相(G1相) / 高珪質粘土相(G2相) / 低珪質粘土相(E1/E2相) / 海綿骨針 / 放散虫 / 高精細SEM / 堆積環境 / 三畳紀中期放散虫化石 / 高緯度海域 / コノドント化石 / 海洋底プレート層序 / チャート / 海綿骨針チャート / 炭酸マンガンノジュール |
Research Abstract |
The bedded chert section on Motutapu Island, near Auckland is comprised of black laminated chert and red chert. Based on conodont biostratigraphy, the black chert is Spathian and the red chert is early to middle Anisian in age. In order to unravel the sedimentary facies and microstructure of the bedded chert, high-resolution SEM observations were carried out on HF-treated chert slabs that were collected through the section. Three microfacies have been recognized: ordinary pelagic chert facies (G2), pelagic siliceous clay facies (E1/E2) and biogenic siliceous constituent facies (G1) comprising abundant sponge spicules and radiolarian shells. Facies G2 has a high biosiliceous component (10-30%) which appears as mostly dissolved and/or poorly preserved microfossils. Facies E1/E2 has a siliceous clay matrix with a low content (1-10%) of biosiliceous shells and spicules. Facies G1 is characterized by densely packed, non-cemented sponge spicules and spherical radiolarian shells.
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Report
(4 results)
Research Products
(62 results)
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[Journal Article] A probable shark dorsal fin fragment from the Early Triassic of the Arrow Rocks sequence, Whangaroa, northern New Zealand2014
Author(s)
Grant-Mackie, J.A., Yamakita, S., Matsumoto, T., Hori, R.S., Takemura, A., Aita, Y., Takahashi, S., and Campbell, H.J
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Journal Title
New Zealand Journal of Geology and Geophysics
Volume: 1
Issue: 3
Pages: 1-5
DOI
Related Report
Peer Reviewed
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[Journal Article] Sulphur isotope profiles in the pelagic Panthalassic deep sea during the Permian-Triassic transition2013
Author(s)
Takahashi, S., Kaiho, K., Hori, R. S., Gorjan, P., Watanabe, T., Yamakita, S., Aita, Y., Takemura, A., Spörli, K.B., Kakegawa, T., and Oba, M
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Journal Title
Global and Planetary Change
Volume: 105
Pages: 68-78
DOI
Related Report
Peer Reviewed
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[Journal Article] Phylum Radiozoa radiolarian. Gordon, D.P. (Ed.) New Zealand Inventory of Biodiversity2012
Author(s)
Hollis, C.J., Lüer, V., Aita, Y., Boltovskoy, D., Hori, R.S., O'Connor, B.M., and Takemura, A
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Journal Title
Kingdoms Bacteria, Protozoa, Chromista, Plantae, Fungi. Canterbury University Press
Volume: Volume 3
Pages: 288-305
Related Report
Peer Reviewed
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[Journal Article] Early Triassic (Induan) Radiolaria and carbon-isotope ratios of a deep-sea sequence from Waiheke Island, North Island, New Zealand2011
Author(s)
Hori, R. S., Yamakita, S., Ikehara, M., Kodama, K., Aita, Y., Sakai, T., Takemura, A., Kamata, Y., Suzuki, N., Takahashi, S., Spörli, K.B., and Grant-Mackie, J.A
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Journal Title
Palaeoworld
Volume: 20
Pages: 166-178
Related Report
Peer Reviewed
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[Presentation] Biogenic silica sedimentation process of Middle Triassic bedded chert from Panthalassa ocean2014
Author(s)
Aita, Y., Tamura, H., Yamakita, S., Takemura, A., Hori, R.S., Takahashi, S., Sporli, K.B., Campbell, H.J.
Organizer
AOGS 2014
Place of Presentation
札幌
Related Report
Invited
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