Sedimentological Effect of Noto Tsunami in the Conditions of Ice Cover on the Coast of the Japan Sea

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Аннотация

The Noto tsunami inundation zone was surveyed in the field in Preobrazheniye Bay (Eastern Primorye) in late January and April 2024. Before the tsunami, the inner part of the bay began to freeze, forming fast ice and drift ice. Despite the low wave height and run-up (20–60 cm according to the results of tacheometric survey), an extensive silt-pelitic mud sheet was formed in the bay on unbroken fast ice and strongly consolidated ice, and covered the shore in the head of the bay (from 1.5 to 26 m). The total length of the silt sheet was 325 m. The tsunami penetrated along the frozen stream up to 680 m from the mouth, and the mud sheet and patches were encountered up to 250 m. Features of wave propagation were recorded by the position of grass blades, Zostera rollers and algal scraps. The grain size composition of mud and biofossils (diatoms and benthic foraminifera) were studied. Changes in grain size and ecological groups of biofossils along the profiles were analyzed. Epiphytes predominate among the diatoms. Benthic foraminifera are mainly represented by agglutinating forms. The source of the material was the littoral and sublittoral, where active erosion of bottom sediments by water saturated with ice floes took place. The implications of the results for paleotsunami searches are discussed.

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Авторлар туралы

N. Razzhigaeva

Pacific Geographical Institute of the Far Eastern Branch of the Russian Academy of Sciences

Хат алмасуға жауапты Автор.
Email: nadyar@tigdvo.ru
Ресей, Vladivostok

D. Tyunyatkin

Pacific Geographical Institute of the Far Eastern Branch of the Russian Academy of Sciences

Email: nadyar@tigdvo.ru
Ресей, Vladivostok

L. Ganzey

Pacific Geographical Institute of the Far Eastern Branch of the Russian Academy of Sciences

Email: nadyar@tigdvo.ru
Ресей, Vladivostok

T. Grebennikova

Pacific Geographical Institute of the Far Eastern Branch of the Russian Academy of Sciences

Email: nadyar@tigdvo.ru
Ресей, Vladivostok

E. Ivanova

Pacific Geographical Institute of the Far Eastern Branch of the Russian Academy of Sciences

Email: nadyar@tigdvo.ru
Ресей, Vladivostok

Yu. Putintsev

Pacific Geographical Institute of the Far Eastern Branch of the Russian Academy of Sciences

Email: nadyar@tigdvo.ru
Ресей, Vladivostok

Yu. Zhabyko

Primorsky Administration for Hydrometeorology and Environmental Monitoring

Email: nadyar@tigdvo.ru
Ресей, Vladivostok

D. Shpachuk

Pacific Geographical Institute of the Far Eastern Branch of the Russian Academy of Sciences; Far East Regional Hydrometeorological Research Institute

Email: nadyar@tigdvo.ru
Ресей, Vladivostok; Vladivostok

E. Stasyuk

Far East Regional Hydrometeorological Research Institute

Email: nadyar@tigdvo.ru
Ресей, Vladivostok

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1. JATS XML
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2. Fig. 1. Research area: a - position of the work area in the Japanese Sea region with the foci of historical tsunamis; b - Sokolovskaya and Preobrazheniya bays with the area where the Noto tsunami inundation zone was surveyed; c - kut part of the Preobrazheniya bay with observation points (ts. d - northern side of the bay and bottom with linear traces of erosion; e - tsunami inundation zone along the watercourse, arrows show the boundaries of the sedimentation zone and maximum splash.

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3. Fig. 2. Change of ice conditions: a - before (01.01.2024, 02:01 UTC) and b - after the Noto tsunami (6.01.2024, 02:01 UTC). Ice situation - according to data of the Far Eastern Centre of FNBU ‘SIC Planeta’.

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4. Fig. 3. Noto tsunami inundation zone in the Bay of Transfiguration. Transformations (a-e - in January, g-m - in April 2024. ): a - kut part of the bay, silt cover and ice floes on landfast ice; b - sediment cover and overlying ice in the inundation zone; c - inverted ice floe with frozen sediment; d - ice floe with abundance of frozen zostera in the foreground; e - ice floes transported by the tsunami to the mouth of the watercourse; f - inundation zone with ice floes and silt patches along the watercourse channel; g - inundation area on the northern side of the bay with a cover and silt stains, the lying grass shows the direction of forward and reverse flows; h - silt cover on the grass near the cut-off; i - silt stain at the place of melted ice floe; j - traces of a counterclockwise whirlpool; e - inundation area on the southern side of the bay; m - boundary of the maximum splash near the bridge over the watercourse (t. n. 436).

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5. Fig. 4. Granulometric characteristics of tsunamigenic sediments in Preobrazheniya Bay. a-e - typical particle size distribution curves and cumulative curves; a-c - tsunamigenic mud, cover on the landfast ice and shore of the bay; d - tsunamigenic mud at the boundary of the sedimentation zone on the watercourse ice; e-e - littoral sediments; g - variation of the mean particle size (Ma), pelite and fine sand fraction content along the profile on the landfast ice (ts. nos. 364-350, inundation zone on the shore (ts. nos. 349-346 and on the watercourse ice). n. 364-350), flood zone on the shore (t. n. 349-346) and on the watercourse ice (t. n. 375-377). Fractional contents: 1 - < 10 µm, 2 - 100-250 µm; h - Passeg diagram for tsunamigenic muds of the bay. Transformation (Noto tsunami, 2024) and closed bays of Shikotan Island (Tohoku tsunami, 2024). Shikotan Island (Tohoku tsunami, 2011).

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6. Fig. 5. Predominant species of diatom algae in the sediments of the Noto Tsunami in Preobrazheniya Bay. Preobrazheniya: a - 1 - profile across the inundation zone to the shore, 2 - profile from the estuary zone along the watercourse ice, 3 - profile on the northern side of the bay, 4 - in sediments transported by ice floes from the littoral. Photos of individual diatom species: b - Cocconeis scutellum Ehrenberg (27 × 18 µm); c - Diploneis interrupta (Kützing) Cleve (42 × 18 µm); d - Gomphonemopsis exigua (Kützing) Medlin (48 × 5.8 µm); e - Gomphonema exiguum var. minutissimum Grunow (11 × 2 µm); f - Petroneis granulata D.G. Mann (50 × 26 µm); g - Hyalodiscus subtilis Bailey (132 × 132 µm); h - Odontella aurita (Lyngbye) Agardh (32 × 12 µm); i - Tryblionella acuminata W. Smith (72 × 12 µm); j - Tryblionella punctata W. Smith (40 × 20 µm); k - Pseudogomphonema kamtchaticum (Grunow) Medlin (48 × 5.8 µm); l - Trigonium caelatum (Janisch) Mann (118 µm); m - Rhoicosphenia marina (Kützing) M. Schmidt (26 × 7. 5 µm); n - Paralia sulcata (Ehrenberg) Kützing (13 × 24 µm, colony); o - Halamphora coffeiformis (Agardh) Levkov (42 × 14 µm); p - Tryblionella plana (Smith) Pelletan (119 × 30 µm); q - Pinnularia quadratarea var. constricta (Østrup) Heiden (45 × 14 μm); r - Coscinodiscus oculus-iridis (Ehrenberg) Ehrenberg (14 × 10 μm, fragment); s - Cymbella angusta (Gregory) Gusliakov (49 × 9 μm); t - Tryblionella coarctata (Grunow) D.G. Mann (32 × 12 µm); u - Ardissonea formosa (Hantzsch) Grunow (50 × 13 µm, fragment); v - Planothidium delicatulum (Kützing) Round & Bukhtiyarova (Kützing) Round & Bukhtiyarova (22 × 8 µm).

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7. Fig. 6. Ratio of total and relative content of benthic foraminifera species (a) and percentage of secreted and agglutinating forms (b) in tsunamigenic muds and sediments of the bay drainage of Bay Preobrazheniye

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