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...
Published in: | Journal of Marine Systems |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier Science
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Online Access: | http://hdl.handle.net/11336/39848 |
_version_ | 1821720173803995136 |
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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 |
id | ftconicet:oai:ri.conicet.gov.ar:11336/39848 |
institution | Open Polar |
language | English |
op_collection_id | ftconicet |
op_container_end_page | 53 |
op_doi | https://doi.org/10.1016/j.jmarsys.2017.07.010 |
op_relation | 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 |
op_rights | info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
publisher | Elsevier Science |
record_format | openpolar |
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 |