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Calcitic sclerites at base of malacostracan pleopods (Crustacea) – part of a coxa

BACKGROUND: Cuticular specialisations such as joints and membranes play an important role in the function of arthropod limbs. This includes sclerotisations and mineral incrustations of cuticular areas to achieve either more rigidity or flexibility. The anterior eight thoracopods of Malacostraca have...

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Autores principales: Kutschera, Verena, Maas, Andreas, Mayer, Gerd, Waloszek, Dieter
Formato: Online Artículo Texto
Lenguaje:English
Publicado: BioMed Central 2015
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4474572/
https://www.ncbi.nlm.nih.gov/pubmed/26087942
http://dx.doi.org/10.1186/s12862-015-0357-6
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author Kutschera, Verena
Maas, Andreas
Mayer, Gerd
Waloszek, Dieter
author_facet Kutschera, Verena
Maas, Andreas
Mayer, Gerd
Waloszek, Dieter
author_sort Kutschera, Verena
collection PubMed
description BACKGROUND: Cuticular specialisations such as joints and membranes play an important role in the function of arthropod limbs. This includes sclerotisations and mineral incrustations of cuticular areas to achieve either more rigidity or flexibility. The anterior eight thoracopods of Malacostraca have limb stems comprising a coxa and a basipod, which carries the two rami. Their pleopods, the limbs of the posterior trunk part, have for long been regarded to lack a coxa. Several calcitic sclerites occur in the area between ventral body and limb stem. This raises the questions: do these elements represent specialisations of the membrane due to functional requirements, and do they originate from an originally larger limb portion, i.e., the coxa, or in fact represent it. RESULTS: We investigated 16 species of selected malacostracan taxa from all major in-groups. Calcitic sclerites occur in constant numbers and position within a species (no individual variation, and independent of specific modification such as in genital appendages). These are even constant within a supra-specific taxon, which facilitates comparisons. In general the sclerites connect via two pivot joints to the sternite medially and the tergopleura laterally, and two more to the limb stem. Based on this, we reconstructed putative ground-pattern conditions for the sclerites of the examined taxa of Malacostraca. CONCLUSIONS: The pattern of sclerites is characteristic for each monophyletic malacostracan taxon. The highest number of sclerites most likely represents the plesiomorphic state. Reduction of sclerite numbers occurs in Caridoida and its in-groups. Sclerite arrangement in these taxa provides an important character complex for phylogenetic studies. The presence of pivot joints to the body proximally and basipod distally demonstrates the existence of a coxa, which is just slightly less sclerotised, particularly on its posterior side. This can be explained by enhanced flexibility of the pleopods evolved in the course to their major role as swimming devices. Both the pivot joints and the proximal and distal extension of the calcitic sclerites demarcate the minimum area of the coxa. With this, sclerites appear as very valuable also in shedding more light on the putative relationships between Malacostraca, Myriapoda, Insecta, and Remipedia.
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spelling pubmed-44745722015-06-20 Calcitic sclerites at base of malacostracan pleopods (Crustacea) – part of a coxa Kutschera, Verena Maas, Andreas Mayer, Gerd Waloszek, Dieter BMC Evol Biol Research Article BACKGROUND: Cuticular specialisations such as joints and membranes play an important role in the function of arthropod limbs. This includes sclerotisations and mineral incrustations of cuticular areas to achieve either more rigidity or flexibility. The anterior eight thoracopods of Malacostraca have limb stems comprising a coxa and a basipod, which carries the two rami. Their pleopods, the limbs of the posterior trunk part, have for long been regarded to lack a coxa. Several calcitic sclerites occur in the area between ventral body and limb stem. This raises the questions: do these elements represent specialisations of the membrane due to functional requirements, and do they originate from an originally larger limb portion, i.e., the coxa, or in fact represent it. RESULTS: We investigated 16 species of selected malacostracan taxa from all major in-groups. Calcitic sclerites occur in constant numbers and position within a species (no individual variation, and independent of specific modification such as in genital appendages). These are even constant within a supra-specific taxon, which facilitates comparisons. In general the sclerites connect via two pivot joints to the sternite medially and the tergopleura laterally, and two more to the limb stem. Based on this, we reconstructed putative ground-pattern conditions for the sclerites of the examined taxa of Malacostraca. CONCLUSIONS: The pattern of sclerites is characteristic for each monophyletic malacostracan taxon. The highest number of sclerites most likely represents the plesiomorphic state. Reduction of sclerite numbers occurs in Caridoida and its in-groups. Sclerite arrangement in these taxa provides an important character complex for phylogenetic studies. The presence of pivot joints to the body proximally and basipod distally demonstrates the existence of a coxa, which is just slightly less sclerotised, particularly on its posterior side. This can be explained by enhanced flexibility of the pleopods evolved in the course to their major role as swimming devices. Both the pivot joints and the proximal and distal extension of the calcitic sclerites demarcate the minimum area of the coxa. With this, sclerites appear as very valuable also in shedding more light on the putative relationships between Malacostraca, Myriapoda, Insecta, and Remipedia. BioMed Central 2015-06-19 /pmc/articles/PMC4474572/ /pubmed/26087942 http://dx.doi.org/10.1186/s12862-015-0357-6 Text en © Kutschera et al. 2015 This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated.
spellingShingle Research Article
Kutschera, Verena
Maas, Andreas
Mayer, Gerd
Waloszek, Dieter
Calcitic sclerites at base of malacostracan pleopods (Crustacea) – part of a coxa
title Calcitic sclerites at base of malacostracan pleopods (Crustacea) – part of a coxa
title_full Calcitic sclerites at base of malacostracan pleopods (Crustacea) – part of a coxa
title_fullStr Calcitic sclerites at base of malacostracan pleopods (Crustacea) – part of a coxa
title_full_unstemmed Calcitic sclerites at base of malacostracan pleopods (Crustacea) – part of a coxa
title_short Calcitic sclerites at base of malacostracan pleopods (Crustacea) – part of a coxa
title_sort calcitic sclerites at base of malacostracan pleopods (crustacea) – part of a coxa
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4474572/
https://www.ncbi.nlm.nih.gov/pubmed/26087942
http://dx.doi.org/10.1186/s12862-015-0357-6
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