Late Holocene higher sea-level indicators from the South China coast
Dating of a relict shell horizon ( Saccostrea cucullata) on Hong Kong Island located approximately 1.7 m above present day high tide level constrains the timing of a late Holocene higher sea-level. At 5140±50 yr BP sea-level in the South China area was 4–5 m higher with respect to the Principal Datu...
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Veröffentlicht in: | Marine geology 2000-12, Vol.171 (1), p.1-5 |
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creator | Davis, A.M Aitchison, J.C Flood, P.G Morton, B.S Baker, R.G.V Haworth, R.J |
description | Dating of a relict shell horizon (
Saccostrea cucullata) on Hong Kong Island located approximately 1.7
m above present day high tide level constrains the timing of a late Holocene higher sea-level. At 5140±50
yr BP sea-level in the South China area was 4–5
m higher with respect to the Principal Datum (2.7
m below high tide mark) than at present. |
doi_str_mv | 10.1016/S0025-3227(00)00113-4 |
format | Article |
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Saccostrea cucullata) on Hong Kong Island located approximately 1.7
m above present day high tide level constrains the timing of a late Holocene higher sea-level. At 5140±50
yr BP sea-level in the South China area was 4–5
m higher with respect to the Principal Datum (2.7
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Saccostrea cucullata) on Hong Kong Island located approximately 1.7
m above present day high tide level constrains the timing of a late Holocene higher sea-level. At 5140±50
yr BP sea-level in the South China area was 4–5
m higher with respect to the Principal Datum (2.7
m below high tide mark) than at present.</description><subject>Biological markers</subject><subject>Holocene</subject><subject>Hong Kong</subject><subject>Marine</subject><subject>Saccostrea cucullata</subject><subject>Sea-level</subject><subject>South China</subject><issn>0025-3227</issn><issn>1872-6151</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2000</creationdate><recordtype>article</recordtype><recordid>eNqFkM1KAzEYRYMoWKuPIGQluhjN32SmK5H6CwUX1XX4mvniRKaTmqQF395pK25d3c25F-4h5Jyza864vpkzJspCClFdMnbFGOeyUAdkxOtKFJqX_JCM_pBjcpLSJxsoycWI3M8gI30OXbDYI239R4uRJoSiww121PeNt5BDTNTFsKS5RToP69zSaet7oDZAyqfkyEGX8Ow3x-T98eFt-lzMXp9epnezAqTmucBaonYCZKlALCrNFLMTlDW3yqGYMN1UIAEaqWXDOUqnJZQlLIRoXK0mCzkmF_vdVQxfa0zZLH2y2HXQY1gnw6tK6VLpASz3oI0hpYjOrKJfQvw2nJmtM7NzZrZCDGNm58yooXe77-HwYuMxmmQ99hYbH9Fm0wT_z8IP8qFyiw</recordid><startdate>20001215</startdate><enddate>20001215</enddate><creator>Davis, A.M</creator><creator>Aitchison, J.C</creator><creator>Flood, P.G</creator><creator>Morton, B.S</creator><creator>Baker, R.G.V</creator><creator>Haworth, R.J</creator><general>Elsevier B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20001215</creationdate><title>Late Holocene higher sea-level indicators from the South China coast</title><author>Davis, A.M ; Aitchison, J.C ; Flood, P.G ; Morton, B.S ; Baker, R.G.V ; Haworth, R.J</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a361t-e83e6f2a354a2b76040c9e381c4fe2906d7a3aad363d11e3f63a55ab22df849b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2000</creationdate><topic>Biological markers</topic><topic>Holocene</topic><topic>Hong Kong</topic><topic>Marine</topic><topic>Saccostrea cucullata</topic><topic>Sea-level</topic><topic>South China</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Davis, A.M</creatorcontrib><creatorcontrib>Aitchison, J.C</creatorcontrib><creatorcontrib>Flood, P.G</creatorcontrib><creatorcontrib>Morton, B.S</creatorcontrib><creatorcontrib>Baker, R.G.V</creatorcontrib><creatorcontrib>Haworth, R.J</creatorcontrib><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Marine geology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Davis, A.M</au><au>Aitchison, J.C</au><au>Flood, P.G</au><au>Morton, B.S</au><au>Baker, R.G.V</au><au>Haworth, R.J</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Late Holocene higher sea-level indicators from the South China coast</atitle><jtitle>Marine geology</jtitle><date>2000-12-15</date><risdate>2000</risdate><volume>171</volume><issue>1</issue><spage>1</spage><epage>5</epage><pages>1-5</pages><issn>0025-3227</issn><eissn>1872-6151</eissn><abstract>Dating of a relict shell horizon (
Saccostrea cucullata) on Hong Kong Island located approximately 1.7
m above present day high tide level constrains the timing of a late Holocene higher sea-level. At 5140±50
yr BP sea-level in the South China area was 4–5
m higher with respect to the Principal Datum (2.7
m below high tide mark) than at present.</abstract><pub>Elsevier B.V</pub><doi>10.1016/S0025-3227(00)00113-4</doi><tpages>5</tpages></addata></record> |
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source | Elsevier ScienceDirect Journals |
subjects | Biological markers Holocene Hong Kong Marine Saccostrea cucullata Sea-level South China |
title | Late Holocene higher sea-level indicators from the South China coast |
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