Analysis of the ichnogenus herradurichnus in quartzites of the balcarce formation (lower silurian) from the tandilia system of Argentina

Herradurichnus Poiré and del Valle, 1996 from the Balcarce Formation (lower Paleozoic of the Tandilia System, Argentina) is an enigmatic ichnogenus previously considered as problematic. In this paper, Herradurichnus is revised and key material from collections is redescribed together with other spec...

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Autores principales: Gutiérrez, C., Pazos, P.J., Fernández, D.E.
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_03757633_v56_n2_p_Gutierrez
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spelling todo:paper_03757633_v56_n2_p_Gutierrez2023-10-03T15:30:35Z Analysis of the ichnogenus herradurichnus in quartzites of the balcarce formation (lower silurian) from the tandilia system of Argentina Gutiérrez, C. Pazos, P.J. Fernández, D.E. Balcarce formation Gondwana Herradurichnus Ichnology Ichnotaxonomy Silurian bedding plane Cambrian fine grained sediment Gondwana ichnology morphology outcrop paleocurrent quartzite sandstone Silurian taxonomy trilobite Argentina Balcarce Buenos Aires [Argentina] Tandilia Range Herradurichnus Poiré and del Valle, 1996 from the Balcarce Formation (lower Paleozoic of the Tandilia System, Argentina) is an enigmatic ichnogenus previously considered as problematic. In this paper, Herradurichnus is revised and key material from collections is redescribed together with other specimens documented in situ from outcrops and quarries. The diagnosis is emended to include its morphological variability. The revised Herradurichnus includes negative, epichnial, U-shaped, V-shaped and parabolic depressions. The specimens are horizontal, subhorizontal or oblique with respect to the bedding plane, and are recorded in fine-grained to very coarse-grained sandstones. Other characteristics are also described in detail. The holotype of Herradurichnus scagliai (Borrello, 1967) has been recovered. Material previously included in Crescentichnus Romano and Whyte, 2015 is now reassigned to Herradurichnus. Xiphosurans and trilobites are disregarded as possible tracemakers of Herradurichnus. The producers were able to construct structures oriented with the convex side of the arch in an opposite sense to the main paleocurrents. This ichnogenus is now reappraised and found to range from the Cambrian to the lower Silurian of Gondwana. © 2017, Mucchi Editori s.r.l. All rights reserved. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_03757633_v56_n2_p_Gutierrez
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Balcarce formation
Gondwana
Herradurichnus
Ichnology
Ichnotaxonomy
Silurian
bedding plane
Cambrian
fine grained sediment
Gondwana
ichnology
morphology
outcrop
paleocurrent
quartzite
sandstone
Silurian
taxonomy
trilobite
Argentina
Balcarce
Buenos Aires [Argentina]
Tandilia Range
spellingShingle Balcarce formation
Gondwana
Herradurichnus
Ichnology
Ichnotaxonomy
Silurian
bedding plane
Cambrian
fine grained sediment
Gondwana
ichnology
morphology
outcrop
paleocurrent
quartzite
sandstone
Silurian
taxonomy
trilobite
Argentina
Balcarce
Buenos Aires [Argentina]
Tandilia Range
Gutiérrez, C.
Pazos, P.J.
Fernández, D.E.
Analysis of the ichnogenus herradurichnus in quartzites of the balcarce formation (lower silurian) from the tandilia system of Argentina
topic_facet Balcarce formation
Gondwana
Herradurichnus
Ichnology
Ichnotaxonomy
Silurian
bedding plane
Cambrian
fine grained sediment
Gondwana
ichnology
morphology
outcrop
paleocurrent
quartzite
sandstone
Silurian
taxonomy
trilobite
Argentina
Balcarce
Buenos Aires [Argentina]
Tandilia Range
description Herradurichnus Poiré and del Valle, 1996 from the Balcarce Formation (lower Paleozoic of the Tandilia System, Argentina) is an enigmatic ichnogenus previously considered as problematic. In this paper, Herradurichnus is revised and key material from collections is redescribed together with other specimens documented in situ from outcrops and quarries. The diagnosis is emended to include its morphological variability. The revised Herradurichnus includes negative, epichnial, U-shaped, V-shaped and parabolic depressions. The specimens are horizontal, subhorizontal or oblique with respect to the bedding plane, and are recorded in fine-grained to very coarse-grained sandstones. Other characteristics are also described in detail. The holotype of Herradurichnus scagliai (Borrello, 1967) has been recovered. Material previously included in Crescentichnus Romano and Whyte, 2015 is now reassigned to Herradurichnus. Xiphosurans and trilobites are disregarded as possible tracemakers of Herradurichnus. The producers were able to construct structures oriented with the convex side of the arch in an opposite sense to the main paleocurrents. This ichnogenus is now reappraised and found to range from the Cambrian to the lower Silurian of Gondwana. © 2017, Mucchi Editori s.r.l. All rights reserved.
format JOUR
author Gutiérrez, C.
Pazos, P.J.
Fernández, D.E.
author_facet Gutiérrez, C.
Pazos, P.J.
Fernández, D.E.
author_sort Gutiérrez, C.
title Analysis of the ichnogenus herradurichnus in quartzites of the balcarce formation (lower silurian) from the tandilia system of Argentina
title_short Analysis of the ichnogenus herradurichnus in quartzites of the balcarce formation (lower silurian) from the tandilia system of Argentina
title_full Analysis of the ichnogenus herradurichnus in quartzites of the balcarce formation (lower silurian) from the tandilia system of Argentina
title_fullStr Analysis of the ichnogenus herradurichnus in quartzites of the balcarce formation (lower silurian) from the tandilia system of Argentina
title_full_unstemmed Analysis of the ichnogenus herradurichnus in quartzites of the balcarce formation (lower silurian) from the tandilia system of Argentina
title_sort analysis of the ichnogenus herradurichnus in quartzites of the balcarce formation (lower silurian) from the tandilia system of argentina
url http://hdl.handle.net/20.500.12110/paper_03757633_v56_n2_p_Gutierrez
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AT pazospj analysisoftheichnogenusherradurichnusinquartzitesofthebalcarceformationlowersilurianfromthetandiliasystemofargentina
AT fernandezde analysisoftheichnogenusherradurichnusinquartzitesofthebalcarceformationlowersilurianfromthetandiliasystemofargentina
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