Palaeoenvironmental analysis of the Miocene barnacle facies: case studies from Europe and South America
Autor: | Giovanni Coletti, Alberto Collareta, Sirio Consani, Akram El Kateb, Giulia Bosio, John S. Buckeridge |
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Přispěvatelé: | Coletti, G, Bosio, G, Collareta, A, Buckeridge, J, Consani, S, El Kateb, A |
Jazyk: | angličtina |
Rok vydání: | 2018 |
Předmět: |
010506 paleontology
Carbonate Factories Heterozoan Barnamol Barnalgal Tertiary Piedmont Basin Sommières Basin Pisco Basin 010502 geochemistry & geophysics Geologic record Barnalgal 01 natural sciences Paleontology Barnacle Barnamol Algae Assemblage (archaeology) 0105 earth and related environmental sciences biology lcsh:QE1-996.5 Heterozoan Tertiary Piedmont Basin Pisco Basin Geology Biota biology.organism_classification Crustacean Northern italy Carbonate Factories lcsh:Geology Facies Sommières Basin |
Zdroj: | Geologica Carpathica, Vol 69, Iss 6, Pp 573-592 (2018) |
ISSN: | 1336-8052 |
Popis: | Acorn barnacles are sessile crustaceans common in shallow-water settings, both in modern oceans and in the Miocene geological record. Barnacle-rich facies occur from polar to equatorial latitudes, generally associated with shallow-water, high-energy, hard substrates. The aim of this work is to investigate this type of facies by analysing, from the palaeontological, sedimentological and petrographical points of view, early Miocene examples from Northern Italy, Southern France and South-western Peru. Our results are then compared with the existing information on both modern and fossil barnacle-rich deposits. The studied facies can be divided into two groups. The first one consists of very shallow, nearshore assemblages where barnacles are associated with an abundant hard-substrate biota (e.g., barnamol). The second one includes a barnacle-coralline algae association, here named “barnalgal” (= barnacle / red algal dominated), related to a deeper setting. The same pattern occurs in the distribution of both fossil and recent barnacle facies. The majority of them are related to very shallow, high-energy, hard-substrate, a setting that represents the environmental optimum for the development of barnacle facies, but exceptions do occur. These atypical facies can be identified through a complete analysis of both the skeletal assemblage and the barnacle association, showing that barnacle palaeontology can be a powerful tool for palaeoenvironmental reconstruction. |
Databáze: | OpenAIRE |
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