Recent foraminiferal assemblages near Ponza Island (Central Tyrrhenian Sea, Italy)

Ponza Island is located in the western sector of the Pontine volcanic Archipelago, on a structural high of the continental Tyrrhenian shelf. This preliminary study is comprised in a broad interdisciplinary project, aimed to know and describe the sea bottom of the Pontine Archipelago. On the whole, 2...

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Bibliographic Details
Main Authors: FREZZA, Virgilio, CARBONI, Maria Gabriella, MATTEUCCI, Ruggero
Other Authors: Frezza, Virgilio, Carboni, Maria Gabriella, Matteucci, Ruggero
Format: Article in Journal/Newspaper
Language:English
Published: 2005
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Online Access:http://hdl.handle.net/11573/360761
Description
Summary:Ponza Island is located in the western sector of the Pontine volcanic Archipelago, on a structural high of the continental Tyrrhenian shelf. This preliminary study is comprised in a broad interdisciplinary project, aimed to know and describe the sea bottom of the Pontine Archipelago. On the whole, 22 grab samples, collected for micropalaeontological analyses East to Ponza during the cruise of spring 2001, have been studied. Sampling stations range from 20 to 380 m water depth and are located on four transects, having the NW/SE direction. Among these, one transect comprises 12 stations, whereas the others are constituted by 2 to 4 stations. A total of 300 benthic foraminifera with well-preserved tests from each sample were separated and classified, from >125 micron size fraction. All benthic foraminifera with broken and old tests (tests with yellow/brown walls and filled by glauconite) were interpreted as reworked and/or displaced. These tests were collected and counted; planktonic foraminifera were contemporaneously counted and identified. Moreover, all the other bioclastic components of sediment (bivalves, bryozoans, coralline algae, gastropods, ostracods, pteropods, spines of echinoids and spicules of sponges) were counted in each aliquot of samples, in order to better describe the bioclastic facies. In absence of significant sources of terrestrial sediments, organic fraction is generally prevalent; benthic foraminifera always dominate bioclastic component, except in two samples. A total of 199 species, belonging to 91 genera, have been recognised. The data set, containing relative abundance of 16 common taxa of benthic foraminifera, was used to perform the multivariate analysis (Hierarchical Cluster Analysis and Principal Cluster Analysis). The output of Q-mode HCA singles out three main clusters, corresponding to three distinct foraminiferal assemblages: 1) Rosalina bradyi and Asterigerinata mamilla assemblage (depth: 20-87 m, inner continental shelf with Posidonia oceanica meadows), with Lobatula ...