Abstract
Shallow 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.
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Acknowledgements
This study was initially undertaken by D.F.M.G. as a partial fulfilment of the requirements for Ph.D. at Royal Holloway University of London (UK). We wish to thank Christine Perrin, and John B. Wilson at RHUL for useful comments on the first stages of this work, José B. Neto and Marcio L. Vianna (INPE/SP) in Brazil for helping with fieldwork. Collecting permits and logistical support were provided by the Reserva Biológica do Atol das Rocas (IBAMA/RN-Brazil) and the Brazilian Navy. This work was supported by CNPq (Brazil) grant no. 260073/92-0 (RHAE-TOPSUB/INPE to D.F.M.G.) and NERC (UK) grants no. GR9/1266 and BFM 550/0993.
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Gherardi, D.F.M., Bosence, D.W.J. Late Holocene reef growth and relative sea-level changes in Atol das Rocas, equatorial South Atlantic. Coral Reefs 24, 264–272 (2005). https://doi.org/10.1007/s00338-005-0475-5
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DOI: https://doi.org/10.1007/s00338-005-0475-5