FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2916106331> ?p ?o ?g. }

• W2916106331 endingPage "1392" @default.
• W2916106331 startingPage "1373" @default.
• W2916106331 abstract "Abstract Tsunami deposits preserved in the geological record provide a more comprehensive understanding of their patterns of frequency and intensity over longer timescales; but recognizing tsunami deposits can prove challenging due to post‐depositional changes, lack of contrast between the deposits and surrounding sedimentary layers, and differentiating between tsunami and storm deposition. Modern baseline studies address these challenges by providing insight into modern spatial distributions that can be compared with palaeotsunami deposits. This study documents the spatial fingerprint of grain size and foraminifera from Hasunuma Beach and the Kujukuri shelf to provide a basis from which tsunami deposits can be interpreted. At Hasunuma Beach, approximately 50 km east of Tokyo, the spatial distribution of three common proxies (foraminiferal taxonomy, foraminiferal taphonomy and sediment grain size) for tsunami identification were mapped and clustered using Partitioning Around Medoids cluster analysis. Partitioning Around Medoids cluster analysis objectively discriminated two coastal zones corresponding to onshore and offshore sample locations. Results show that onshore samples are characterized by coarser grain sizes (medium to coarse sand) and higher abundances of Pararotalia nipponica (27 to 63%) than offshore samples, which are characterized by finer grain sizes (fine to medium sand), lower abundances of Pararotalia nipponica (2 to 19%) and Ammonia parkinsoniana (0 to 10%), higher abundances of planktonics (15 to 58%) and species with fragile tests including Uvigerinella glabra . When compared to grain‐size and foraminiferal taxonomy, foraminiferal taphonomy; i.e. surface condition of foraminifera, a proxy not commonly used to identify tsunami deposits, was most effective in discriminating modern coastal zones (identified supratidal, intertidal and offshore environments) and determining sediment provenance for tsunami deposits at Kujukuri. This modern baseline study assists the interpretation of tsunami deposits in the geological record because it provides a basis for sediment provenance to be determined." @default.
• W2916106331 created "2019-03-02" @default.
• W2916106331 creator A5019737450 @default.
• W2916106331 creator A5026586431 @default.
• W2916106331 creator A5031572966 @default.
• W2916106331 creator A5051542070 @default.
• W2916106331 creator A5060646080 @default.
• W2916106331 creator A5067412557 @default.
• W2916106331 creator A5077248254 @default.
• W2916106331 creator A5084053928 @default.
• W2916106331 creator A5084918743 @default.
• W2916106331 creator A5089444914 @default.
• W2916106331 date "2019-04-30" @default.
• W2916106331 modified "2023-10-01" @default.
• W2916106331 title "Constraining sediment provenance for tsunami deposits using distributions of grain size and foraminifera from the Kujukuri coastline and shelf, Japan" @default.
• W2916106331 cites W1481622287 @default.
• W2916106331 cites W1493454437 @default.
• W2916106331 cites W1512247913 @default.
• W2916106331 cites W1531316914 @default.
• W2916106331 cites W1534682587 @default.
• W2916106331 cites W1823167647 @default.
• W2916106331 cites W1964577047 @default.
• W2916106331 cites W1967072856 @default.
• W2916106331 cites W1969905542 @default.
• W2916106331 cites W1975444579 @default.
• W2916106331 cites W1977844210 @default.
• W2916106331 cites W1982086088 @default.
• W2916106331 cites W1985094595 @default.
• W2916106331 cites W1990127547 @default.
• W2916106331 cites W2002506179 @default.
• W2916106331 cites W2003561999 @default.
• W2916106331 cites W2004712931 @default.
• W2916106331 cites W2007673724 @default.
• W2916106331 cites W2007782885 @default.
• W2916106331 cites W2010681628 @default.
• W2916106331 cites W2010883462 @default.
• W2916106331 cites W2012644643 @default.
• W2916106331 cites W2020653750 @default.
• W2916106331 cites W2023317688 @default.
• W2916106331 cites W2027826665 @default.
• W2916106331 cites W2028719423 @default.
• W2916106331 cites W2040423036 @default.
• W2916106331 cites W2046809970 @default.
• W2916106331 cites W2050765201 @default.
• W2916106331 cites W2051448467 @default.
• W2916106331 cites W2055702267 @default.
• W2916106331 cites W2058275453 @default.
• W2916106331 cites W2071781238 @default.
• W2916106331 cites W2077267127 @default.
• W2916106331 cites W2080071812 @default.
• W2916106331 cites W2089382933 @default.
• W2916106331 cites W2089623642 @default.
• W2916106331 cites W2089660532 @default.
• W2916106331 cites W2093443145 @default.
• W2916106331 cites W2096549615 @default.
• W2916106331 cites W2104045754 @default.
• W2916106331 cites W2104377612 @default.
• W2916106331 cites W2115333736 @default.
• W2916106331 cites W2123925869 @default.
• W2916106331 cites W2124334795 @default.
• W2916106331 cites W2135859728 @default.
• W2916106331 cites W2137384232 @default.
• W2916106331 cites W2141949079 @default.
• W2916106331 cites W2143087931 @default.
• W2916106331 cites W2143370091 @default.
• W2916106331 cites W2155175103 @default.
• W2916106331 cites W2157505241 @default.
• W2916106331 cites W2158686645 @default.
• W2916106331 cites W2185624931 @default.
• W2916106331 cites W2203764990 @default.
• W2916106331 cites W2269341987 @default.
• W2916106331 cites W2281842549 @default.
• W2916106331 cites W2314022116 @default.
• W2916106331 cites W2324530999 @default.
• W2916106331 cites W2330191137 @default.
• W2916106331 cites W2527097712 @default.
• W2916106331 cites W2582922089 @default.
• W2916106331 cites W2625900549 @default.
• W2916106331 cites W2765660414 @default.
• W2916106331 cites W2901193697 @default.
• W2916106331 cites W4234700805 @default.
• W2916106331 cites W4234712688 @default.
• W2916106331 cites W4367590708 @default.
• W2916106331 doi "https://doi.org/10.1111/sed.12591" @default.
• W2916106331 hasPublicationYear "2019" @default.
• W2916106331 type Work @default.
• W2916106331 sameAs 2916106331 @default.
• W2916106331 citedByCount "13" @default.
• W2916106331 countsByYear W29161063312019 @default.
• W2916106331 countsByYear W29161063312020 @default.
• W2916106331 countsByYear W29161063312021 @default.
• W2916106331 countsByYear W29161063312022 @default.
• W2916106331 countsByYear W29161063312023 @default.
• W2916106331 crossrefType "journal-article" @default.
• W2916106331 hasAuthorship W2916106331A5019737450 @default.
• W2916106331 hasAuthorship W2916106331A5026586431 @default.
• W2916106331 hasAuthorship W2916106331A5031572966 @default.
• W2916106331 hasAuthorship W2916106331A5051542070 @default.

• next