File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

Article: Holocene relative sea-level change in Hiroshima Bay, Japan: A semi-quantitative reconstruction based on ostracodes

TitleHolocene relative sea-level change in Hiroshima Bay, Japan: A semi-quantitative reconstruction based on ostracodes
Authors
Yasuhara, MSeto, K
KeywordsHolocene
Japan
Ostracoda
Relative sea-level change
Semi-quantitative reconstruction
Seto Inland Sea
Issue Date2006
Citation
Paleontological Research, 2006, v. 10 n. 2, p. 99-116 How to Cite?
DOI: http://dx.doi.org/10.2517/prpsj.10.99
AbstractHolocene relative sea-level changes in Hiroshima Bay were reconstructed from fossil ostracodes from a core, using a semi-quantitative method. In Hiroshima Bay, relative sea level rose rapidly (about 25 m) between ca. 9000 cal yr BP and ca. 5800 cal yr BP, after which it gradually fell (about 5 m) to its present level. The peak in relative sea level occurred at ca. 5800 cal yr BP. The sea-level curve for Hiroshima Bay is similar to curves for tectonically stable areas of Japan (e.g., Osaka Bay). © by the Palaeontological Society of Japan.
Persistent Identifierhttp://hdl.handle.net/10722/132797
ISSN
1342-8144
2023 Impact Factor: 1.3
2023 SCImago Journal Rankings: 0.533
References
References in Scopus

 

DC FieldValueLanguage
dc.contributor.authorYasuhara, Men_HK
dc.contributor.authorSeto, Ken_HK
dc.date.accessioned2011-03-28T09:29:09Z-
dc.date.available2011-03-28T09:29:09Z-
dc.date.issued2006en_HK
dc.identifier.citationPaleontological Research, 2006, v. 10 n. 2, p. 99-116en_HK
dc.identifier.issn1342-8144en_HK
dc.identifier.urihttp://hdl.handle.net/10722/132797-
dc.description.abstractHolocene relative sea-level changes in Hiroshima Bay were reconstructed from fossil ostracodes from a core, using a semi-quantitative method. In Hiroshima Bay, relative sea level rose rapidly (about 25 m) between ca. 9000 cal yr BP and ca. 5800 cal yr BP, after which it gradually fell (about 5 m) to its present level. The peak in relative sea level occurred at ca. 5800 cal yr BP. The sea-level curve for Hiroshima Bay is similar to curves for tectonically stable areas of Japan (e.g., Osaka Bay). © by the Palaeontological Society of Japan.en_HK
dc.languageengen_US
dc.relation.ispartofPaleontological Researchen_HK
dc.subjectHoloceneen_HK
dc.subjectJapanen_HK
dc.subjectOstracodaen_HK
dc.subjectRelative sea-level changeen_HK
dc.subjectSemi-quantitative reconstructionen_HK
dc.subjectSeto Inland Seaen_HK
dc.titleHolocene relative sea-level change in Hiroshima Bay, Japan: A semi-quantitative reconstruction based on ostracodesen_HK
dc.typeArticleen_HK
dc.identifier.emailYasuhara, M: yasuhara@hku.hken_HK
dc.identifier.authorityYasuhara, M=rp01474en_HK
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.doi10.2517/prpsj.10.99en_HK
dc.identifier.scopuseid_2-s2.0-33748531274en_HK
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-33748531274&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume10en_HK
dc.identifier.issue2en_HK
dc.identifier.spage99en_HK
dc.identifier.epage116en_HK
dc.identifier.scopusauthoridYasuhara, M=7102069020en_HK
dc.identifier.scopusauthoridSeto, K=7202201396en_HK
dc.identifier.issnl1342-8144-

Export via OAI-PMH Interface in XML Formats

OR

Export to Other Non-XML Formats