Pleistocene radiolarian biostratigraphy of the submarine Vityaz Ridge, Northwest Pacific

This study presents new data on radiolarian fauna from the Pliocene–Quaternary sediments of the submarine Vityaz Ridge (SVR) and the paraxial zone of the Kuril– Kamchatka Trench (KKT): 60 taxa from 32 genera of Spumellaria, 50 taxa from 34 genera of Nassellaria, and 6 taxa from 2 genera of Collodari...

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Veröffentlicht in:Marine micropaleontology 2021-12, Vol.169, p.102040, Article 102040
Hauptverfasser: Vasilenko, Lidiya Nikolaevna, Vasilenko, Yuriy Pavlovich
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Sprache:eng
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Zusammenfassung:This study presents new data on radiolarian fauna from the Pliocene–Quaternary sediments of the submarine Vityaz Ridge (SVR) and the paraxial zone of the Kuril– Kamchatka Trench (KKT): 60 taxa from 32 genera of Spumellaria, 50 taxa from 34 genera of Nassellaria, and 6 taxa from 2 genera of Collodaria were observed. An analysis of taxonomic compositional of the radiolarians revealed the Pleistocene radiolarian zone assemblages Cycladophora sphaeris, Eucyrtidium matuyamai, Stylatractus universus, and Lychnocanoma sakaii on the SVR and in the paraxial zone of the KKT. We also determined geographical distributions of these zones in the North Pacific. In addition, based on our and other previously published data, we inferred that two hiatuses occurred (during the Late Pliocene and the Middle–Late Pleistocene) in the study area. We established that the southern and northern plateaus of the SVR developed in different tectonic and sedimentation regimes at the end of the Early–beginning of the Middle Pleistocene. •Three orders, 68 genera, and 116 radiolarian taxa were identified from submarine Vityaz Ridge.•Regional zonal radiolarian scheme for the Quaternary period of the submarine Vityaz Ridge was designed.•Hiatuses recognized in the Late Pliocene and Middle-Late Pleistocene.•The geographical distributions of Pleistocene radiolarian zones in the North Pacific are determined.•The southern and northern plateaus of the submarine Vityaz Ridge developed in different tectonic and sedimentation regimes at the end of the Early–beginning of the Middle Pleistocene.
ISSN:0377-8398
1872-6186
DOI:10.1016/j.marmicro.2021.102040