Uplift rate of Kitadaito Jima Island on the lithospheric forebulge of the Philippine Sea Plate

Abstract Estimates of uplift rates for lithospheric forebulges are needed to understand exact plate motions at plate convergence zones and to delineate the fate of coral reefs atop the forebulges. A carbonate island on a lithospheric forebulge can provide excellent materials for estimating uplift ra...

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Main Authors: Yasufumi Iryu, Hideko Takayanagi, Tsuyoshi Ishikawa, Akimasa Ishigaki, Takuji Asanuma, Rin Teruya, David A. Budd
Format: Article
Language:English
Published: SpringerOpen 2023-01-01
Series:Progress in Earth and Planetary Science
Subjects:
Online Access:https://doi.org/10.1186/s40645-023-00535-5
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author Yasufumi Iryu
Hideko Takayanagi
Tsuyoshi Ishikawa
Akimasa Ishigaki
Takuji Asanuma
Rin Teruya
David A. Budd
author_facet Yasufumi Iryu
Hideko Takayanagi
Tsuyoshi Ishikawa
Akimasa Ishigaki
Takuji Asanuma
Rin Teruya
David A. Budd
author_sort Yasufumi Iryu
collection DOAJ
description Abstract Estimates of uplift rates for lithospheric forebulges are needed to understand exact plate motions at plate convergence zones and to delineate the fate of coral reefs atop the forebulges. A carbonate island on a lithospheric forebulge can provide excellent materials for estimating uplift rate because carbonate sediments can be dated and their paleo-water depth determined. We estimated the uplift rate of Kitadaito Jima Island, a carbonate island on the lithospheric forebulge of the Philippine Sea Plate that is subducting beneath the Eurasian Plate. Marine skeletal sands containing pebble-sized bioclasts and filling the concavity of an intertidal erosional notch at an elevation of ~ 71 m were found near the top of this island. Strontium isotope ages ranging from 1.78 to 2.01 Ma with an average of 1.89 Ma (standard deviation = 0.07 Ma) were obtained from these deposits. As global sea level at 1.89 Ma was ~ 21 m lower than the present, the mean uplift rate was estimated at ~ 49 m/million years (Myr) with a compounded uncertainty of ± 2.6 m/Myr. This rate is comparable to, or up to ~ 140 m/Myr less than, rates reported from other Indo-Pacific carbonate islands in similar tectonic settings. This study illustrates how contemporary Sr isotope age models and careful considerations of limestone sample depositional depths can yield more accurate and precise uplift rates of modern forearc bulges than possible in many older studies.
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spelling doaj.art-58b6659c3f2c4c7fb2d1e8e977cb60162023-01-22T12:28:28ZengSpringerOpenProgress in Earth and Planetary Science2197-42842023-01-0110111410.1186/s40645-023-00535-5Uplift rate of Kitadaito Jima Island on the lithospheric forebulge of the Philippine Sea PlateYasufumi Iryu0Hideko Takayanagi1Tsuyoshi Ishikawa2Akimasa Ishigaki3Takuji Asanuma4Rin Teruya5David A. Budd6Institute of Geology and Paleontology, Graduate School of Science, Tohoku UniversityInstitute of Geology and Paleontology, Graduate School of Science, Tohoku UniversityKochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)Institute of Geology and Paleontology, Graduate School of Science, Tohoku UniversityKitadaito Village Board of EducationKitadaito Village Board of EducationDepartment of Geological Sciences, University of ColoradoAbstract Estimates of uplift rates for lithospheric forebulges are needed to understand exact plate motions at plate convergence zones and to delineate the fate of coral reefs atop the forebulges. A carbonate island on a lithospheric forebulge can provide excellent materials for estimating uplift rate because carbonate sediments can be dated and their paleo-water depth determined. We estimated the uplift rate of Kitadaito Jima Island, a carbonate island on the lithospheric forebulge of the Philippine Sea Plate that is subducting beneath the Eurasian Plate. Marine skeletal sands containing pebble-sized bioclasts and filling the concavity of an intertidal erosional notch at an elevation of ~ 71 m were found near the top of this island. Strontium isotope ages ranging from 1.78 to 2.01 Ma with an average of 1.89 Ma (standard deviation = 0.07 Ma) were obtained from these deposits. As global sea level at 1.89 Ma was ~ 21 m lower than the present, the mean uplift rate was estimated at ~ 49 m/million years (Myr) with a compounded uncertainty of ± 2.6 m/Myr. This rate is comparable to, or up to ~ 140 m/Myr less than, rates reported from other Indo-Pacific carbonate islands in similar tectonic settings. This study illustrates how contemporary Sr isotope age models and careful considerations of limestone sample depositional depths can yield more accurate and precise uplift rates of modern forearc bulges than possible in many older studies.https://doi.org/10.1186/s40645-023-00535-5Kitadaito JimaLithospheric forebulgePhilippine Sea PlateUplift rateSr isotope stratigraphy
spellingShingle Yasufumi Iryu
Hideko Takayanagi
Tsuyoshi Ishikawa
Akimasa Ishigaki
Takuji Asanuma
Rin Teruya
David A. Budd
Uplift rate of Kitadaito Jima Island on the lithospheric forebulge of the Philippine Sea Plate
Progress in Earth and Planetary Science
Kitadaito Jima
Lithospheric forebulge
Philippine Sea Plate
Uplift rate
Sr isotope stratigraphy
title Uplift rate of Kitadaito Jima Island on the lithospheric forebulge of the Philippine Sea Plate
title_full Uplift rate of Kitadaito Jima Island on the lithospheric forebulge of the Philippine Sea Plate
title_fullStr Uplift rate of Kitadaito Jima Island on the lithospheric forebulge of the Philippine Sea Plate
title_full_unstemmed Uplift rate of Kitadaito Jima Island on the lithospheric forebulge of the Philippine Sea Plate
title_short Uplift rate of Kitadaito Jima Island on the lithospheric forebulge of the Philippine Sea Plate
title_sort uplift rate of kitadaito jima island on the lithospheric forebulge of the philippine sea plate
topic Kitadaito Jima
Lithospheric forebulge
Philippine Sea Plate
Uplift rate
Sr isotope stratigraphy
url https://doi.org/10.1186/s40645-023-00535-5
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