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Postglacial stratigraphic evolution of a current‐influenced sandy shelf: offshore Kujukuri strandplain, central Japan
Author(s) -
Nishida Naohisa,
Ajioka Taku,
Ikehara Ken,
Nakashima Rei,
Katayama Hajime,
Sato Tomoyuki,
Furuyama Seishiro,
Tamura Toru
Publication year - 2020
Publication title -
sedimentology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.494
H-Index - 108
eISSN - 1365-3091
pISSN - 0037-0746
DOI - 10.1111/sed.12654
Subject(s) - geology , sedimentary depositional environment , sedimentary rock , continental shelf , current (fluid) , lamination , oceanography , sediment , submarine pipeline , storm , paleontology , clastic rock , sediment transport , sedimentary structures , geomorphology , structural basin , chemistry , organic chemistry , layer (electronics)
Sandy shelf sediments are important elements of clastic sedimentary systems because of their wide distribution in the geological record and their significance as hydrocarbon reservoirs. Although many studies have investigated shelf sediments influenced by waves or tidal currents, little is known about shelf sediments influenced by oceanic currents, particularly their lithofacies characteristics and stratigraphic evolution. This study investigated the stratigraphic evolution of shelf sediments off the Kujukuri strandplain facing the Pacific Ocean, which is influenced by the strong Kuroshio Current. Sediment cores were obtained from six locations on the Kujukuri shelf (34 to 124 m water depth) using a vibrocorer. The dominant lithofacies is mud‐free sand with low‐angle cross‐lamination associated with alternating beds of finer and coarser sand with cross‐lamination. These display depositional processes influenced by storm waves and the Kuroshio Current, respectively. This finding is consistent with the previously presented modern and historical observations of the Kuroshio Current and estimates of the storm‐wave base. Radiocarbon dates show that the sediment succession formed during the last transgressive and highstand stages after 13·1 ka. The depositional processes during the stages represent a transition from storm waves with abundant sediment supply to both storm waves and the Kuroshio Current with sediment starvation mainly due to its trapping in the strandplain. Comparison to other Holocene–Modern shelf systems suggests that the sandy shelf successions are strongly influenced by oceanic currents under conditions of limited riverine input and open coastal geometry. The resultant sand‐dominated succession is characterized by reversal of the proximal to distal grain‐size trend compared to the fining for most other recognized wave/storm‐dominated shelf successions. This is because of seaward increase in the influence of the Kuroshio Current. Thus, shelf deposits are naturally complex, and these may be further complicated by the additional influence of oceanic currents above the usual wave‐dominated and tide‐dominated end members.