Facies and faunal assemblage changes in response to the Holocene transgression in the Lagoon of Mayotte (Comoro Archipelago, SW Indian Ocean)

Autor: Wolf-Christian Dullo, Jens Zinke, John J. G. Reijmer, Marco Taviani, B. A. Thomassin
Přispěvatelé: Petrology
Rok vydání: 2005
Předmět:
Zdroj: Facies, 50 (3-4). pp. 391-408.
Zinke, J, Reijmer, J J G, Taviani, M, Dullo, W-C & Thomassin, B A 2005, ' Facies and faunal assemblage changes in response to the Holocene transgression in the lagoon of Mayotte (Comoro Archipelago, SW Indian Ocean) ', Facies, vol. 50, no. (3-4), pp. 391-408 . https://doi.org/10.1007/s10347-004-0040-7
Facies, 50((3-4)), 391-408. Springer Verlag
Facies 50 (2005): 391–408.
info:cnr-pdr/source/autori:Zinke J. (1) (4), Reijmer J.J.G. (5), Taviani M. (2), Dullo W.C. (1), Thomassin B. (3)/titolo:Facies and faunal assemblage changes in response to the Holocene transgression in the Lagoon of Mayotte (Comoro Archipelago, SW Indian Ocean)/doi:/rivista:Facies/anno:2005/pagina_da:391/pagina_a:408/intervallo_pagine:391–408/volume:50
ISSN: 0172-9179
DOI: 10.1007/s10347-004-0040-7
Popis: This paper documents the facies change in response to the Holocene transgression within five sediment cores taken in the lagoon of Mayotte, which contain a Type-1 depositional sequence (lowstand, transgressive and highstand deposits underlain by an erosive sequence boundary). Quantitative compositional analysis and visual examination of the bioclasts were used to document the facies changes. The distribution of the skeletal and non-skeletal grains in the lagoon of Mayotte is clearly controlled by (1) the rate and amplitude of the Holocene sea-level rise, (2) the pre-Holocene basement topography and (3) the growth-potential of the barrier reef during sea-level rise, and the changes in bathymetry and continuity during this period. The sequence boundary consists of the glacial karst surface. The change-over from the glacial lowstand is marked by the occurrence of mangrove deposits. Terrigenous and/or mixed terrigenous-carbonate muds to sandy muds with a mollusc or mollusc-ostracod assemblage dominate the transgressive deposits. Mixed carbonate-siliciclastic or carbonate sand to gravel with a mollusc-foraminifer or mollusc-coral-foraminifer assemblage characterize the early highstand deposits on the inner lagoonal plains. The early highstand deposits in the outer lagoonal plains consist of carbonate muds with a mollusc-foraminifer assemblage. Late highstand deposits consist of terrigenous muds in the nearshore bays, mixed terrigenous-carbonate sandy muds to sands with a mollusc-foraminifer assemblage on the inner lagoonal plains and mixed muds with a mollusc-foraminifer assemblage on the outer deep lagoonal plains. The present development stage of the individual lagoons comprises semi-enclosed to open lagoons with fair or good water exchange with the open ocean. © Springer-Verlag 2005.
Databáze: OpenAIRE
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