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

Zinke, Jens, Reijmer, John, Taviani, Marco, Dullo, Wolf-Christian and Thomassin, Bernard (2005) Facies and faunal assemblage changes in response to the Holocene transgression in the Lagoon of Mayotte (Comoro Archipelago, SW Indian Ocean). Facies, 50 (3-4). pp. 391-408. DOI 10.1007/s10347-004-0040-7.

[img] Text
257_Taviani_2005_FaciesAndFaunalAssemblageChanges_Artzeit_pubid10077.pdf - Published Version
Restricted to Registered users only

Download (1015Kb) | Contact

Supplementary data:


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.

Document Type: Article
Keywords: Lagoonal communities, Quantitative compositional analysis, Systems tracts, Sea-level changes, Comoro Archipelago, Holocene
Research affiliation: OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-P-OZ Paleo-Oceanography
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1007/s10347-004-0040-7
ISSN: 0172-9179
Date Deposited: 27 Jul 2009 14:58
Last Modified: 19 Jan 2018 11:16
URI: http://oceanrep.geomar.de/id/eprint/6862

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...