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Please use this identifier to cite or link to this item: https://lib.hpu.edu.vn/handle/123456789/23657
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dc.contributor.authorVanWoesik, R.en_US
dc.contributor.authorGolbuu, Y.en_US
dc.contributor.authorRoff, G.en_US
dc.date.accessioned2016-10-11T05:37:44Z
dc.date.available2016-10-11T05:37:44Z
dc.date.issued2015en_US
dc.identifier.otherHPU4160577en_US
dc.identifier.urihttps://lib.hpu.edu.vn/handle/123456789/23657en_US
dc.description.abstractSince the Mid-Holocene, some 5000 years ago, coral reefs in the Pacific Ocean have been vertically constrained by sea level. Contemporary sea-level rise is releasing these constraints, providing accommodation space for vertical reef expansion. Here, we show that Porites microatolls, from reef-flat environments in Palau (western Pacific Ocean), are ‘keeping up’ with contemporary sea-level rise.en_US
dc.format.extent8 p.en_US
dc.format.mimetypeapplication/pdfen_US
dc.language.isoenen_US
dc.subjectBiologyen_US
dc.subjectEcologyen_US
dc.subjectEnvironmental scienceen_US
dc.subjectPalaeontologyen_US
dc.subjectSea-level riseen_US
dc.subjectPacificen_US
dc.subjectCoral reefsen_US
dc.typeArticleen_US
dc.size1.25MBen_US
dc.departmentEducationen_US
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