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1. Identity statement
Reference TypeJournal Article
Sitemtc-m12.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositorysid.inpe.br/iris@1912/2005/07.12.11.49   (restricted access)
Last Update2005:07.12.03.00.00 (UTC) administrator
Metadata Repositorysid.inpe.br/iris@1912/2005/07.12.11.49.44
Metadata Last Update2019:02.04.13.03.17 (UTC) administrator
Secondary KeyINPE-12879-PRE/8169
ISSN0722-4028
Citation KeyGherardiBose:2005:LaHoRe
TitleLate Holocene reef growth and relative sea-level changes in Atol das Rocas, equatorial South Atlantic
ProjectPrograma HIDRO
Year2005
MonthJune
Access Date2024, Apr. 28
Secondary TypePRE PI
Number of Files1
Size481 KiB
2. Context
Author1 Gherardi, Douglas Francisco Marcolino
2 Bosence, D. W. J.
Resume Identifier1 8JMKD3MGP5W/3C9JGU3
Group1 DSR-INPE-MCT-BR
Affiliation1 Royal Holloway Univ London, Dept Geol, Egham, Surrey TW20 0EX England
2 Instituto Nacional de Pesquisas Espaciais, Divisão de Sensoriamento Remoto(INPE, DSR)
JournalCoral Reefs
Volume24
Number2
Pages264-272
History (UTC)2005-07-12 11:49:44 :: sergio -> administrator ::
2005-07-18 18:06:13 :: administrator -> sergio ::
2006-03-17 14:48:00 :: sergio -> administrator ::
2006-09-03 21:42:17 :: administrator -> sergio ::
2007-04-23 21:07:03 :: sergio -> administrator ::
2008-06-09 19:18:47 :: administrator -> marciana ::
2011-12-02 13:12:45 :: marciana -> administrator ::
2019-02-04 13:03:17 :: administrator -> simone :: 2005
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsOCEANOGRAFIA
coralline algae
reef growth
radiocarbon dating
Atol das Rocas
AbstractShallow drilling provided the first detailed record of vertical reef accretion rates for the last 4,000 years from the oceanic atoll Atol das Rocas. Six cores up to1-m long from windward, leeward, and intertidal hardground environments were radiocarbon dated. Frameworks are dominated by the coralline alga Porolithon cf. pachydermum with minor contributions of Lithophyllum sp. Coralline bindstone and framestone facies were identified. Vertical accretion rates (VAR) form three groups: group A frameworks were formed between 3,490 +/- 45 years BP and 2,770 +/- 45 years BP, and VAR are 0.85, 1.4, and 1.6 mm/year; group B frameworks were formed between 2,510 +/- 45 year BP and 490 +/- 45 year BP, and VAR are 0.25, 0.46, and 0.42 mm/year; group C frameworks were formed between 900 +/- 50 year BP and 655 +/- 45 year BP, and VAR are 3.2, 9.75, and 18.4 mm/year. Results indicate that coralline-algal reefs may display a catch-down response to a falling sea level similar to the way corals respond to a rising sea level. In this case, present day reef topography may be the result of late Holocene SW Atlantic sea-level changes. The calculated VAR of 18.4 mm/year is the highest rate known to date for a coralline-algal reef and close to the maximum rates recorded for corals.
AreaSRE
Arrangementurlib.net > Fonds > Produção anterior à 2021 > DIDSR > Late Holocene reef...
doc Directory Contentaccess
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4. Conditions of access and use
Languageen
Target FileJ2816W186363K471.pdf
User Groupadministrator
marciana
sergio
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher denyfinaldraft12
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ER446E
DisseminationWEBSCI
Host Collectionsid.inpe.br/banon/2001/04.06.10.52
6. Notes
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