A review of crural types, their relationships to shell microstructure, and significance among post-Palaeozoic Rhynchonellida

Autores
Manceñido, Miguel Oscar; Motchurova Dekova, Neda
Año de publicación
2010
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
This overview deals with a few key morphological features that appear crucial to the advancement of knowledge about relationships between macromorphology and micromorphology of the rhynchonellide brachiopod shell. Relevant aspects that may hinder description, comparison and ⁄ or interpretation of morphological skeletal structures of rhynchonellides when studied by means of serial grinding techniques are briefly reviewed. First, the types of crura, traditionally regarded of paramount taxonomic importance, are currently placed into four main cognate groups: septifal, arcual, raducal and ensimergal. Constituent types are characterized, and likely transformation series among them are also outlined. The value of crural types and their groupings within the systematic and evolutionary framework currently applied to post-Palaeozoic Rhynchonellida is corroborated, as is the significant role of heterochronic processes in the development of evolutionary novelties or in the recovery from a severe biotic crisis. Therefore, further studies of ontogenetic development of crura should be encouraged. Second, the main kinds of microstructural patterns of the secondary shell layer as seen in cross section are summarized and illustrated. The leptinoid pattern, typically displaying finer, anisometric fibres with anvil-like or halberd-like outline is contrasted with the eurinoid type, characteristically having coarser, isometric fibres with predominantly diamond-shaped cross section. A close correspondence established between leptinoid shell microstructure and superfamilies with crura of the raducal and ensimergal groups (such as hemithiridoids, rhynchonelloids, rhynchotrematoids, dimerelloids) on the one hand, and between eurinoid shell pattern and superfamilies with crura of the septifal and arcual groups (e.g. pugnacoids, wellerelloids, norelloids) on the other vindicates the prevailing classificatory scheme. Finally, some broad variations of the basic configurations in mantle canal patterns are outlined, confirming the merit of jointly analysing multiple morphological characters and of applying a variety of techniques. All these may lead towards a stronger, more stable and predictive classification of Rhynchonellida in which there is potential for reconsidering the suitability of proper subordinal divisions.
Fil: Manceñido, Miguel Oscar. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Departamento de Paleontología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Motchurova Dekova, Neda. National Museum of Natural History; Bulgaria. University of Mining and Geology; Bulgaria
Materia
Brachiopoda
Rhynchonellida
Crura
Shell microstructure
Mantle canals
Systematics
Heterochrony
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/241551

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network_name_str CONICET Digital (CONICET)
spelling A review of crural types, their relationships to shell microstructure, and significance among post-Palaeozoic RhynchonellidaManceñido, Miguel OscarMotchurova Dekova, NedaBrachiopodaRhynchonellidaCruraShell microstructureMantle canalsSystematicsHeterochronyhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1This overview deals with a few key morphological features that appear crucial to the advancement of knowledge about relationships between macromorphology and micromorphology of the rhynchonellide brachiopod shell. Relevant aspects that may hinder description, comparison and ⁄ or interpretation of morphological skeletal structures of rhynchonellides when studied by means of serial grinding techniques are briefly reviewed. First, the types of crura, traditionally regarded of paramount taxonomic importance, are currently placed into four main cognate groups: septifal, arcual, raducal and ensimergal. Constituent types are characterized, and likely transformation series among them are also outlined. The value of crural types and their groupings within the systematic and evolutionary framework currently applied to post-Palaeozoic Rhynchonellida is corroborated, as is the significant role of heterochronic processes in the development of evolutionary novelties or in the recovery from a severe biotic crisis. Therefore, further studies of ontogenetic development of crura should be encouraged. Second, the main kinds of microstructural patterns of the secondary shell layer as seen in cross section are summarized and illustrated. The leptinoid pattern, typically displaying finer, anisometric fibres with anvil-like or halberd-like outline is contrasted with the eurinoid type, characteristically having coarser, isometric fibres with predominantly diamond-shaped cross section. A close correspondence established between leptinoid shell microstructure and superfamilies with crura of the raducal and ensimergal groups (such as hemithiridoids, rhynchonelloids, rhynchotrematoids, dimerelloids) on the one hand, and between eurinoid shell pattern and superfamilies with crura of the septifal and arcual groups (e.g. pugnacoids, wellerelloids, norelloids) on the other vindicates the prevailing classificatory scheme. Finally, some broad variations of the basic configurations in mantle canal patterns are outlined, confirming the merit of jointly analysing multiple morphological characters and of applying a variety of techniques. All these may lead towards a stronger, more stable and predictive classification of Rhynchonellida in which there is potential for reconsidering the suitability of proper subordinal divisions.Fil: Manceñido, Miguel Oscar. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Departamento de Paleontología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Motchurova Dekova, Neda. National Museum of Natural History; Bulgaria. University of Mining and Geology; BulgariaPalaeontological Association2010-11info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/241551Manceñido, Miguel Oscar; Motchurova Dekova, Neda; A review of crural types, their relationships to shell microstructure, and significance among post-Palaeozoic Rhynchonellida; Palaeontological Association; Special Papers In Palaeontology Series; 84; 11-2010; 203-2240038-6804CONICET DigitalCONICETenginfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:36:36Zoai:ri.conicet.gov.ar:11336/241551instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:36:36.745CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv A review of crural types, their relationships to shell microstructure, and significance among post-Palaeozoic Rhynchonellida
title A review of crural types, their relationships to shell microstructure, and significance among post-Palaeozoic Rhynchonellida
spellingShingle A review of crural types, their relationships to shell microstructure, and significance among post-Palaeozoic Rhynchonellida
Manceñido, Miguel Oscar
Brachiopoda
Rhynchonellida
Crura
Shell microstructure
Mantle canals
Systematics
Heterochrony
title_short A review of crural types, their relationships to shell microstructure, and significance among post-Palaeozoic Rhynchonellida
title_full A review of crural types, their relationships to shell microstructure, and significance among post-Palaeozoic Rhynchonellida
title_fullStr A review of crural types, their relationships to shell microstructure, and significance among post-Palaeozoic Rhynchonellida
title_full_unstemmed A review of crural types, their relationships to shell microstructure, and significance among post-Palaeozoic Rhynchonellida
title_sort A review of crural types, their relationships to shell microstructure, and significance among post-Palaeozoic Rhynchonellida
dc.creator.none.fl_str_mv Manceñido, Miguel Oscar
Motchurova Dekova, Neda
author Manceñido, Miguel Oscar
author_facet Manceñido, Miguel Oscar
Motchurova Dekova, Neda
author_role author
author2 Motchurova Dekova, Neda
author2_role author
dc.subject.none.fl_str_mv Brachiopoda
Rhynchonellida
Crura
Shell microstructure
Mantle canals
Systematics
Heterochrony
topic Brachiopoda
Rhynchonellida
Crura
Shell microstructure
Mantle canals
Systematics
Heterochrony
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv This overview deals with a few key morphological features that appear crucial to the advancement of knowledge about relationships between macromorphology and micromorphology of the rhynchonellide brachiopod shell. Relevant aspects that may hinder description, comparison and ⁄ or interpretation of morphological skeletal structures of rhynchonellides when studied by means of serial grinding techniques are briefly reviewed. First, the types of crura, traditionally regarded of paramount taxonomic importance, are currently placed into four main cognate groups: septifal, arcual, raducal and ensimergal. Constituent types are characterized, and likely transformation series among them are also outlined. The value of crural types and their groupings within the systematic and evolutionary framework currently applied to post-Palaeozoic Rhynchonellida is corroborated, as is the significant role of heterochronic processes in the development of evolutionary novelties or in the recovery from a severe biotic crisis. Therefore, further studies of ontogenetic development of crura should be encouraged. Second, the main kinds of microstructural patterns of the secondary shell layer as seen in cross section are summarized and illustrated. The leptinoid pattern, typically displaying finer, anisometric fibres with anvil-like or halberd-like outline is contrasted with the eurinoid type, characteristically having coarser, isometric fibres with predominantly diamond-shaped cross section. A close correspondence established between leptinoid shell microstructure and superfamilies with crura of the raducal and ensimergal groups (such as hemithiridoids, rhynchonelloids, rhynchotrematoids, dimerelloids) on the one hand, and between eurinoid shell pattern and superfamilies with crura of the septifal and arcual groups (e.g. pugnacoids, wellerelloids, norelloids) on the other vindicates the prevailing classificatory scheme. Finally, some broad variations of the basic configurations in mantle canal patterns are outlined, confirming the merit of jointly analysing multiple morphological characters and of applying a variety of techniques. All these may lead towards a stronger, more stable and predictive classification of Rhynchonellida in which there is potential for reconsidering the suitability of proper subordinal divisions.
Fil: Manceñido, Miguel Oscar. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Departamento de Paleontología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Motchurova Dekova, Neda. National Museum of Natural History; Bulgaria. University of Mining and Geology; Bulgaria
description This overview deals with a few key morphological features that appear crucial to the advancement of knowledge about relationships between macromorphology and micromorphology of the rhynchonellide brachiopod shell. Relevant aspects that may hinder description, comparison and ⁄ or interpretation of morphological skeletal structures of rhynchonellides when studied by means of serial grinding techniques are briefly reviewed. First, the types of crura, traditionally regarded of paramount taxonomic importance, are currently placed into four main cognate groups: septifal, arcual, raducal and ensimergal. Constituent types are characterized, and likely transformation series among them are also outlined. The value of crural types and their groupings within the systematic and evolutionary framework currently applied to post-Palaeozoic Rhynchonellida is corroborated, as is the significant role of heterochronic processes in the development of evolutionary novelties or in the recovery from a severe biotic crisis. Therefore, further studies of ontogenetic development of crura should be encouraged. Second, the main kinds of microstructural patterns of the secondary shell layer as seen in cross section are summarized and illustrated. The leptinoid pattern, typically displaying finer, anisometric fibres with anvil-like or halberd-like outline is contrasted with the eurinoid type, characteristically having coarser, isometric fibres with predominantly diamond-shaped cross section. A close correspondence established between leptinoid shell microstructure and superfamilies with crura of the raducal and ensimergal groups (such as hemithiridoids, rhynchonelloids, rhynchotrematoids, dimerelloids) on the one hand, and between eurinoid shell pattern and superfamilies with crura of the septifal and arcual groups (e.g. pugnacoids, wellerelloids, norelloids) on the other vindicates the prevailing classificatory scheme. Finally, some broad variations of the basic configurations in mantle canal patterns are outlined, confirming the merit of jointly analysing multiple morphological characters and of applying a variety of techniques. All these may lead towards a stronger, more stable and predictive classification of Rhynchonellida in which there is potential for reconsidering the suitability of proper subordinal divisions.
publishDate 2010
dc.date.none.fl_str_mv 2010-11
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/241551
Manceñido, Miguel Oscar; Motchurova Dekova, Neda; A review of crural types, their relationships to shell microstructure, and significance among post-Palaeozoic Rhynchonellida; Palaeontological Association; Special Papers In Palaeontology Series; 84; 11-2010; 203-224
0038-6804
CONICET Digital
CONICET
url http://hdl.handle.net/11336/241551
identifier_str_mv Manceñido, Miguel Oscar; Motchurova Dekova, Neda; A review of crural types, their relationships to shell microstructure, and significance among post-Palaeozoic Rhynchonellida; Palaeontological Association; Special Papers In Palaeontology Series; 84; 11-2010; 203-224
0038-6804
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Palaeontological Association
publisher.none.fl_str_mv Palaeontological Association
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.070432