Do coastal fronts influence bioerosion patterns along Patagonia? Late Quaternary ichnological tools from Golfo San Jorge

Late Quaternary marine molluscan skeletal concentrations from Argentina constitute a remarkable record of variations in palaeoceanographical conditions during interglacial times (mainly ca. 125 ka to present). Particularly, the Golfo San Jorge coastal area represents an extraordinary geographical zo...

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Published in:Journal of Marine Systems
Main Authors: Richiano, Sebastián Miguel, Aguirre, Marina Laura, Castellanos, Ignacio, Davies, Karen, Farinati, Ester Amanda
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier Science
Subjects:
Online Access:http://hdl.handle.net/11336/39848
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author Richiano, Sebastián Miguel
Aguirre, Marina Laura
Castellanos, Ignacio
Davies, Karen
Farinati, Ester Amanda
author_facet Richiano, Sebastián Miguel
Aguirre, Marina Laura
Castellanos, Ignacio
Davies, Karen
Farinati, Ester Amanda
author_sort Richiano, Sebastián Miguel
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_start_page 38
container_title Journal of Marine Systems
container_volume 176
description Late Quaternary marine molluscan skeletal concentrations from Argentina constitute a remarkable record of variations in palaeoceanographical conditions during interglacial times (mainly ca. 125 ka to present). Particularly, the Golfo San Jorge coastal area represents an extraordinary geographical zone to target from different points of view, mainly due to its linkage between northern and southern Patagonia, characterized by particular and contrasting physico-chemical conditions with direct consequences for littoral marine communities, determining their composition and structure. Among varied biological activities controlled by different environmental factors (i.e., substrate nature, sedimentation rates, water depth, sea surface temperature, salinity, nutrients-productivity), bioerosion traces can provide palaeoenvironmental evidence with important implications for palaeoclimate interpretations. In addition, the application of bioerosion patterns regionally and through time is a recent valuable worthy palaeoenvironmental tool not as yet developed for Patagonia. We attempted to characterize, qualitatively/semiquantitatively, the ichnotaxonomic composition of the coastal area of northern Golfo San Jorge since the Late Pleistocene; to compare results with those obtained for other geographical areas along Patagonia and the Bonaerensian coastal sectors; lastly, to evaluate its palaeoenvironmental/palaeoclimatic significance in a clue area in terms of circulation patterns near the Southern Ocean climatic pump. At Bustamante (Northern Patagonia Frontal System) Domichnia traces were dominant during the Late Pleistocene while Praedichnia in the mid-Holocene. Bustamante exhibits the highest ichnodiversity for the whole Argentinean coastal area. Ichnodiversity is not strongly different between Late Pleistocene and mid-Holocene interglacials and compared to present; however, the relative abundance of some ichnotaxa (e.g., Oichnus, Iramena, Pennatichnus, at Camarones; Oichnus, Iramena, Pinaceocladichnus, at Bustamante) ...
format Article in Journal/Newspaper
genre Southern Ocean
genre_facet Southern Ocean
geographic Argentina
Patagonia
Southern Ocean
geographic_facet Argentina
Patagonia
Southern Ocean
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op_doi https://doi.org/10.1016/j.jmarsys.2017.07.010
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http://hdl.handle.net/11336/39848
Richiano, Sebastián Miguel; Aguirre, Marina Laura; Castellanos, Ignacio; Davies, Karen; Farinati, Ester Amanda; Do coastal fronts influence bioerosion patterns along Patagonia? Late Quaternary ichnological tools from Golfo San Jorge; Elsevier Science; Journal Of Marine Systems; 176; 12-2017; 38-53
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CONICET Digital
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/39848 2025-01-17T00:56:57+00:00 Do coastal fronts influence bioerosion patterns along Patagonia? Late Quaternary ichnological tools from Golfo San Jorge Richiano, Sebastián Miguel Aguirre, Marina Laura Castellanos, Ignacio Davies, Karen Farinati, Ester Amanda application/pdf http://hdl.handle.net/11336/39848 eng eng Elsevier Science info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0924796317301082 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jmarsys.2017.07.010 http://hdl.handle.net/11336/39848 Richiano, Sebastián Miguel; Aguirre, Marina Laura; Castellanos, Ignacio; Davies, Karen; Farinati, Ester Amanda; Do coastal fronts influence bioerosion patterns along Patagonia? Late Quaternary ichnological tools from Golfo San Jorge; Elsevier Science; Journal Of Marine Systems; 176; 12-2017; 38-53 0924-7963 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ ICHNOLOGY GASTROPODS BIVALVES BRYOZOANS ACTIVITY PLEISTOCENE HOLOCENE https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1016/j.jmarsys.2017.07.010 2023-09-24T18:40:38Z Late Quaternary marine molluscan skeletal concentrations from Argentina constitute a remarkable record of variations in palaeoceanographical conditions during interglacial times (mainly ca. 125 ka to present). Particularly, the Golfo San Jorge coastal area represents an extraordinary geographical zone to target from different points of view, mainly due to its linkage between northern and southern Patagonia, characterized by particular and contrasting physico-chemical conditions with direct consequences for littoral marine communities, determining their composition and structure. Among varied biological activities controlled by different environmental factors (i.e., substrate nature, sedimentation rates, water depth, sea surface temperature, salinity, nutrients-productivity), bioerosion traces can provide palaeoenvironmental evidence with important implications for palaeoclimate interpretations. In addition, the application of bioerosion patterns regionally and through time is a recent valuable worthy palaeoenvironmental tool not as yet developed for Patagonia. We attempted to characterize, qualitatively/semiquantitatively, the ichnotaxonomic composition of the coastal area of northern Golfo San Jorge since the Late Pleistocene; to compare results with those obtained for other geographical areas along Patagonia and the Bonaerensian coastal sectors; lastly, to evaluate its palaeoenvironmental/palaeoclimatic significance in a clue area in terms of circulation patterns near the Southern Ocean climatic pump. At Bustamante (Northern Patagonia Frontal System) Domichnia traces were dominant during the Late Pleistocene while Praedichnia in the mid-Holocene. Bustamante exhibits the highest ichnodiversity for the whole Argentinean coastal area. Ichnodiversity is not strongly different between Late Pleistocene and mid-Holocene interglacials and compared to present; however, the relative abundance of some ichnotaxa (e.g., Oichnus, Iramena, Pennatichnus, at Camarones; Oichnus, Iramena, Pinaceocladichnus, at Bustamante) ... Article in Journal/Newspaper Southern Ocean CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Argentina Patagonia Southern Ocean Journal of Marine Systems 176 38 53
spellingShingle ICHNOLOGY
GASTROPODS
BIVALVES
BRYOZOANS ACTIVITY
PLEISTOCENE
HOLOCENE
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Richiano, Sebastián Miguel
Aguirre, Marina Laura
Castellanos, Ignacio
Davies, Karen
Farinati, Ester Amanda
Do coastal fronts influence bioerosion patterns along Patagonia? Late Quaternary ichnological tools from Golfo San Jorge
title Do coastal fronts influence bioerosion patterns along Patagonia? Late Quaternary ichnological tools from Golfo San Jorge
title_full Do coastal fronts influence bioerosion patterns along Patagonia? Late Quaternary ichnological tools from Golfo San Jorge
title_fullStr Do coastal fronts influence bioerosion patterns along Patagonia? Late Quaternary ichnological tools from Golfo San Jorge
title_full_unstemmed Do coastal fronts influence bioerosion patterns along Patagonia? Late Quaternary ichnological tools from Golfo San Jorge
title_short Do coastal fronts influence bioerosion patterns along Patagonia? Late Quaternary ichnological tools from Golfo San Jorge
title_sort do coastal fronts influence bioerosion patterns along patagonia? late quaternary ichnological tools from golfo san jorge
topic ICHNOLOGY
GASTROPODS
BIVALVES
BRYOZOANS ACTIVITY
PLEISTOCENE
HOLOCENE
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet ICHNOLOGY
GASTROPODS
BIVALVES
BRYOZOANS ACTIVITY
PLEISTOCENE
HOLOCENE
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/39848