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Accession Number:
AD0412368
Title:
Recent Carbonate Sedimentation on Alacran Beef, Yucatan, Mexico.
Descriptive Note:
Corporate Author:
NATIONAL ACADEMY OF SCIENCES-NATIONAL RESEARCH COUNCIL WASHINGTON DC
Report Date:
1963-01-01
Pagination or Media Count:
160.0
Abstract:
Hard parts from marine organisms composed or aragonite and calcite, and a trace of siliceous particles from Recent surface sediments on Alacran Reef, a living coral continental shelf atoll in the Gulf of Mexico. These surface sediments are sands and silts which contain minor amounts of gravel and clay-size particles. Within the three major environments of the reef, the windward reef, the leeward reef, and the lagoon, the proportion of each size grade in the sediments is a reflection of the depositional environment coarse sediments accumulate in shallow, wave-washed areas, and fine sediments in deeper water. These three major environments have been subdivided into 19 biotopes, most of which are recognized by criteria of grain size and grain-type composition. Nearly all sub merged sediments are poorly sorted, and most are coarse-skewed andkurtic. The averaged sand fraction of Alacran Reef sediment is com posed of 35 Halimeda, 29 coral, 8 coralline algae, 8 mollusks, 6 foraminifers, 1 miscel laneous skeletal grains, 9 fecal pellets, and 4 aggregates, by volume. Coral grains are most abundant in sediment on the tops of lagoon pin nacle reefs. Author
Distribution Statement:
APPROVED FOR PUBLIC RELEASE