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Holocene evolution of the granite based Lizard Island and MacGillivray Reef systems, Northern Great Barrier Reef
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The current ocean level is generally considered to be reached around 6000 BP; Rees et al. estimate it was established around 4000 BP.
“Si se considera generalmente que el nivel actual de los océanos se alcanza alrededor de 6000 BP (4000 a. C), Rees et al. (2006) estiman que el nivel actual se establece hacia 4000 BP (2050 a. C).”
From Geodinámica y ocupación humana del litoral pacífico en el sur de colombia y en el ecuador desde el holoceno (últimos 10 000 años) (2010) · cites this paper as Rees et al. (2006)
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Research works printed but not linked: 46
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Usselmann, P. (2010) · Bulletin de l’Institut français d’études andines · doi:10.4000/bifea.1798 · Cited by 1
Metadata
- Authors
- Rees, S. A., Opdyke, B. N., Wilson, P. A., Keith Fifield, L., & Levchenko, V.
- Venue
- Coral Reefs
- Published
- 2006-08-12
- Volume
- 25
- Issue
- 4
- Pages
- 555-565
- ISSN
- 0722-4028
- 1432-0975
- Cited by
- 26
- References
- 0
- Language
- en
- Licence
- www.springer.com/tdm (tdm)
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