Benthic foraminifera as environmental indicators in extreme environments: The marine cave of Bue Marino (Sardinia, Italy)

The coast of the Gulf of Orosei (Sardinia, Italy) consists of impressive cliffs set up on dolostones and limestones characterized by wide karst systems connected to the sea. Marine caves, which are part of these system flooded by seawater through marine entrances, may be considered as extreme enviro...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Elena Romano, Luisa Bergamin, Letizia Di Bella, Virgilio Frezza, Giancarlo Pierfranceschi, Andrea Marassich, Claudio Provenzani
Formato: article
Lenguaje:EN
Publicado: Elsevier 2021
Materias:
Acceso en línea:https://doaj.org/article/89c47a9ddf04446084f7ed43ae3f2226
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:89c47a9ddf04446084f7ed43ae3f2226
record_format dspace
spelling oai:doaj.org-article:89c47a9ddf04446084f7ed43ae3f22262021-12-01T04:31:29ZBenthic foraminifera as environmental indicators in extreme environments: The marine cave of Bue Marino (Sardinia, Italy)1470-160X10.1016/j.ecolind.2020.106977https://doaj.org/article/89c47a9ddf04446084f7ed43ae3f22262021-01-01T00:00:00Zhttp://www.sciencedirect.com/science/article/pii/S1470160X2030916Xhttps://doaj.org/toc/1470-160XThe coast of the Gulf of Orosei (Sardinia, Italy) consists of impressive cliffs set up on dolostones and limestones characterized by wide karst systems connected to the sea. Marine caves, which are part of these system flooded by seawater through marine entrances, may be considered as extreme environments because of wide spatial and temporal environmental variability due to changing marine and terrestrial contributions. This study presents the results of the third survey carried out in summer 2016 in the Bue Marino cave, as part of a research project started in 2014 aimed at the application of Benthic Foraminifera (BF) as ecological indicators in Mediterranean marine caves for the identification of different habitats and their environmental interpretation. Sediment and water samples were collected from a total of 25 stations from two distinct sectors of the cave (North Branch and Middle Branch); sediments were analysed for living and dead BF and grain size, while Temperature, Salinity, pH and Dissolved Oxygen were measured in water samples collected close to sediment water interface. Two main foraminiferal assemblages, with distinct characteristics with respect to the typical Mediterranean shallow-water ones, were recognized by means of Hierarchical Cluster Analysis and Non-metric Multidimensional Scaling, and a Canonical Correspondence Analysis deduced their environmental significance. A well oxygenated, less saline environment with coarse bottom sediment, correlated with a mixed calcareous-agglutinated assemblage (Gavelinopsis praegeri, Rosalina spp., Eggerelloides advenus and Reophax dentaliniformis) with high species diversity (H-index 2.32–3.57) and low foraminiferal density, was exclusive of the North Branch. A scarcely oxygenated, more saline environment with fine bottom sediment enriched in vegetal debris was related to a prevalently agglutinated assemblage characterized by low species diversity (H-index 1.60–2.68), with high dominance of E. advenus (up to 83.6%) associated to Ammonia tepida, and high foraminiferal density, recognized in the Middle Branch. These different environments were interpreted considering the different modes of feeding the karst systems of the two branches. They also corresponded to two distinct ecozones, Entrance and Confluence, already recognized in earlier studies. The environmental significance of the foraminiferal ecozones recognized in this study and their comparison with the ones identified in the previous years, helped to consider the ecological zonation as a tool for detecting seasonal and, possibly, long term annual environmental variability in the marine system.Elena RomanoLuisa BergaminLetizia Di BellaVirgilio FrezzaGiancarlo PierfranceschiAndrea MarassichClaudio ProvenzaniElsevierarticleMarine cavesBenthic foraminiferaEcological indicatorsCave sedimentSardiniaEcologyQH540-549.5ENEcological Indicators, Vol 120, Iss , Pp 106977- (2021)
institution DOAJ
collection DOAJ
language EN
topic Marine caves
Benthic foraminifera
Ecological indicators
Cave sediment
Sardinia
Ecology
QH540-549.5
spellingShingle Marine caves
Benthic foraminifera
Ecological indicators
Cave sediment
Sardinia
Ecology
QH540-549.5
Elena Romano
Luisa Bergamin
Letizia Di Bella
Virgilio Frezza
Giancarlo Pierfranceschi
Andrea Marassich
Claudio Provenzani
Benthic foraminifera as environmental indicators in extreme environments: The marine cave of Bue Marino (Sardinia, Italy)
description The coast of the Gulf of Orosei (Sardinia, Italy) consists of impressive cliffs set up on dolostones and limestones characterized by wide karst systems connected to the sea. Marine caves, which are part of these system flooded by seawater through marine entrances, may be considered as extreme environments because of wide spatial and temporal environmental variability due to changing marine and terrestrial contributions. This study presents the results of the third survey carried out in summer 2016 in the Bue Marino cave, as part of a research project started in 2014 aimed at the application of Benthic Foraminifera (BF) as ecological indicators in Mediterranean marine caves for the identification of different habitats and their environmental interpretation. Sediment and water samples were collected from a total of 25 stations from two distinct sectors of the cave (North Branch and Middle Branch); sediments were analysed for living and dead BF and grain size, while Temperature, Salinity, pH and Dissolved Oxygen were measured in water samples collected close to sediment water interface. Two main foraminiferal assemblages, with distinct characteristics with respect to the typical Mediterranean shallow-water ones, were recognized by means of Hierarchical Cluster Analysis and Non-metric Multidimensional Scaling, and a Canonical Correspondence Analysis deduced their environmental significance. A well oxygenated, less saline environment with coarse bottom sediment, correlated with a mixed calcareous-agglutinated assemblage (Gavelinopsis praegeri, Rosalina spp., Eggerelloides advenus and Reophax dentaliniformis) with high species diversity (H-index 2.32–3.57) and low foraminiferal density, was exclusive of the North Branch. A scarcely oxygenated, more saline environment with fine bottom sediment enriched in vegetal debris was related to a prevalently agglutinated assemblage characterized by low species diversity (H-index 1.60–2.68), with high dominance of E. advenus (up to 83.6%) associated to Ammonia tepida, and high foraminiferal density, recognized in the Middle Branch. These different environments were interpreted considering the different modes of feeding the karst systems of the two branches. They also corresponded to two distinct ecozones, Entrance and Confluence, already recognized in earlier studies. The environmental significance of the foraminiferal ecozones recognized in this study and their comparison with the ones identified in the previous years, helped to consider the ecological zonation as a tool for detecting seasonal and, possibly, long term annual environmental variability in the marine system.
format article
author Elena Romano
Luisa Bergamin
Letizia Di Bella
Virgilio Frezza
Giancarlo Pierfranceschi
Andrea Marassich
Claudio Provenzani
author_facet Elena Romano
Luisa Bergamin
Letizia Di Bella
Virgilio Frezza
Giancarlo Pierfranceschi
Andrea Marassich
Claudio Provenzani
author_sort Elena Romano
title Benthic foraminifera as environmental indicators in extreme environments: The marine cave of Bue Marino (Sardinia, Italy)
title_short Benthic foraminifera as environmental indicators in extreme environments: The marine cave of Bue Marino (Sardinia, Italy)
title_full Benthic foraminifera as environmental indicators in extreme environments: The marine cave of Bue Marino (Sardinia, Italy)
title_fullStr Benthic foraminifera as environmental indicators in extreme environments: The marine cave of Bue Marino (Sardinia, Italy)
title_full_unstemmed Benthic foraminifera as environmental indicators in extreme environments: The marine cave of Bue Marino (Sardinia, Italy)
title_sort benthic foraminifera as environmental indicators in extreme environments: the marine cave of bue marino (sardinia, italy)
publisher Elsevier
publishDate 2021
url https://doaj.org/article/89c47a9ddf04446084f7ed43ae3f2226
work_keys_str_mv AT elenaromano benthicforaminiferaasenvironmentalindicatorsinextremeenvironmentsthemarinecaveofbuemarinosardiniaitaly
AT luisabergamin benthicforaminiferaasenvironmentalindicatorsinextremeenvironmentsthemarinecaveofbuemarinosardiniaitaly
AT letiziadibella benthicforaminiferaasenvironmentalindicatorsinextremeenvironmentsthemarinecaveofbuemarinosardiniaitaly
AT virgiliofrezza benthicforaminiferaasenvironmentalindicatorsinextremeenvironmentsthemarinecaveofbuemarinosardiniaitaly
AT giancarlopierfranceschi benthicforaminiferaasenvironmentalindicatorsinextremeenvironmentsthemarinecaveofbuemarinosardiniaitaly
AT andreamarassich benthicforaminiferaasenvironmentalindicatorsinextremeenvironmentsthemarinecaveofbuemarinosardiniaitaly
AT claudioprovenzani benthicforaminiferaasenvironmentalindicatorsinextremeenvironmentsthemarinecaveofbuemarinosardiniaitaly
_version_ 1718405855453380608