World subterranean ostracod biogeography: dispersal or vicariance
Identifieur interne : 00D722 ( Main/Exploration ); précédent : 00D721; suivant : 00D723World subterranean ostracod biogeography: dispersal or vicariance
Auteurs : D. L. Danielopol [Autriche] ; P. Marmonier [France] ; A. J. Boulton [Australie] ; G. Bonaduce [Italie]Source :
- Hydrobiologia [ 0018-8158 ] ; 1994-07-01.
Descripteurs français
English descriptors
- KwdEn :
- Active dispersal, Active migration, Ancestral species, Arcturi, Atlantic ocean, Biogeography, Bonaduce, Boulton, Candoninae namibcypridini, Carapace, Carapace shape, Cavernocypris, Central america, Colonisation, Colonised, Common ancestor, Continental drift, Costata, Crustacea, Danielopol, Danielopol bonaduce, Danielopol hart, Danielopol hartmann, Danube river, Defaunated hyporheic sediments, Desert stream, Dispersal, Dispersionist model, Ecological, Ecological flexibility, Ecological processes, Ecological requirements, Ecological tolerance, Ecology, Epigean, Fabaeformiscandona wegelini, Freshwater, Galapagos, Galapagos islands, Genus, Genus cavernocypris, Genus hobsiella, Genus sphaeromicola, Geographic distribution, Geological events, Hobsiella species, Hyporheic zone, Interstitial, Interstitial animals, Interstitial fauna, Interstitial habitats, Interstitial ostracods, Interstitial spaces, Interstitial species, Interstitial xestoleberis species, Karstic, Karstic areas, Laboratory observations, Lobau wetland, Long history, Main channel, Many species, Marine ancestor, Marine ostracods, Marmonier, Marmonier ward, Marten, Namibcypridini, Oceanic islands, Ostracod, Ostracod case histories, Ostracod groups, Ostracoda, Passive dispersal, Passive transport, Phylogenetic lineage, Phytophilous species, Platte river, Rhbne river, Roca danielopol, Sandy sediments, Sediment, Sonoran desert stream, Southern texas, Spatial distribution, Spatial scales, Sphaeromicola, Sphaeromicolinae, Subsurface, Subsurface environment, Subsurface habitats, Subsurface ostracods, Subterranean, Subterranean crustaceans, Subterranean freshwaters, Subterranean habitats, Subterranean taxa, Surface sediments, Surface waters, Sycamore creek, Taxon, Taxonomic position, Tuberoloxoconcha, Upper messinian, Various times, Vicariance, Vicariance biogeography, Vicariance model, Water column, Wegelini, West indies, Western coast, Wide range, World distribution, Worldwide distribution, Xestoleberis, Xestoleberis arcturi group, Xestoleberis arcturi species group.
- Teeft :
- Active dispersal, Active migration, Ancestral species, Arcturi, Atlantic ocean, Biogeography, Bonaduce, Boulton, Candoninae namibcypridini, Carapace, Carapace shape, Cavernocypris, Central america, Colonisation, Colonised, Common ancestor, Continental drift, Costata, Crustacea, Danielopol, Danielopol bonaduce, Danielopol hart, Danielopol hartmann, Danube river, Defaunated hyporheic sediments, Desert stream, Dispersal, Dispersionist model, Ecological, Ecological flexibility, Ecological processes, Ecological requirements, Ecological tolerance, Ecology, Epigean, Fabaeformiscandona wegelini, Freshwater, Galapagos, Galapagos islands, Genus, Genus cavernocypris, Genus hobsiella, Genus sphaeromicola, Geographic distribution, Geological events, Hobsiella species, Hyporheic zone, Interstitial, Interstitial animals, Interstitial fauna, Interstitial habitats, Interstitial ostracods, Interstitial spaces, Interstitial species, Interstitial xestoleberis species, Karstic, Karstic areas, Laboratory observations, Lobau wetland, Long history, Main channel, Many species, Marine ancestor, Marine ostracods, Marmonier, Marmonier ward, Marten, Namibcypridini, Oceanic islands, Ostracod, Ostracod case histories, Ostracod groups, Ostracoda, Passive dispersal, Passive transport, Phylogenetic lineage, Phytophilous species, Platte river, Rhbne river, Roca danielopol, Sandy sediments, Sediment, Sonoran desert stream, Southern texas, Spatial distribution, Spatial scales, Sphaeromicola, Sphaeromicolinae, Subsurface, Subsurface environment, Subsurface habitats, Subsurface ostracods, Subterranean, Subterranean crustaceans, Subterranean freshwaters, Subterranean habitats, Subterranean taxa, Surface sediments, Surface waters, Sycamore creek, Taxon, Taxonomic position, Tuberoloxoconcha, Upper messinian, Various times, Vicariance, Vicariance biogeography, Vicariance model, Water column, Wegelini, West indies, Western coast, Wide range, World distribution, Worldwide distribution, Xestoleberis, Xestoleberis arcturi group, Xestoleberis arcturi species group.
Abstract
Abstract: Origins of the present day distribution of several freshwater and marine phyletic groups of ostracods are described using both Recent and fossil data. Six examples of subterranean ostracods distributed world-wide are discussed. The first two examples (i.e. the Candoninae Namibcypridini and the Sphaeromicolinae) seemed, in a first approach, to fit well with the ‘vicariance model’ but a detailed study demonstrate that their present day distribution can not be seen as a consequence of any geological events. The four other examples (the Xestoleberis arcturi species group, the Tuberoloxoconcha, the Cavernocypris and Fabaeformiscandona wegelini) fit well with the ‘dispersionist model’. We propose a biogeographical model similar to the dispersal one which foccus on the ecological processes occurring at local and/or regional scales. Some present day species or their epigean ancestors may originally have been more widely dispersed. These species were predisposed to colonize subsurface habitats; a process that could occur polytopically and at various times. It is the degree of ecological flexibility, the width of ecological tolerance, the type of preadaptations, and the capacity to perceive and successfully invade new environments that allow subsurface ostracods to migrate actively or be dispersed passively through both subterranean and epigean aquatic systems and to settle in new places. But no centers of origin and direction of dispersal can be identified in our data. There is little known about the autecology of subterranean ostracod taxa with broad geographical ranges. Samples should be collected at fine (habitat) and broad scales (regional surveys) so that we can better understand the modes of ostracod dispersal across a range of spatial scales.
Url:
DOI: 10.1007/BF00006901
Affiliations:
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type="ISSN">0018-8158</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Active dispersal</term><term>Active migration</term><term>Ancestral species</term><term>Arcturi</term><term>Atlantic ocean</term><term>Biogeography</term><term>Bonaduce</term><term>Boulton</term><term>Candoninae namibcypridini</term><term>Carapace</term><term>Carapace shape</term><term>Cavernocypris</term><term>Central america</term><term>Colonisation</term><term>Colonised</term><term>Common ancestor</term><term>Continental drift</term><term>Costata</term><term>Crustacea</term><term>Danielopol</term><term>Danielopol bonaduce</term><term>Danielopol hart</term><term>Danielopol hartmann</term><term>Danube river</term><term>Defaunated hyporheic sediments</term><term>Desert stream</term><term>Dispersal</term><term>Dispersionist model</term><term>Ecological</term><term>Ecological flexibility</term><term>Ecological processes</term><term>Ecological requirements</term><term>Ecological tolerance</term><term>Ecology</term><term>Epigean</term><term>Fabaeformiscandona wegelini</term><term>Freshwater</term><term>Galapagos</term><term>Galapagos islands</term><term>Genus</term><term>Genus cavernocypris</term><term>Genus hobsiella</term><term>Genus sphaeromicola</term><term>Geographic distribution</term><term>Geological events</term><term>Hobsiella species</term><term>Hyporheic zone</term><term>Interstitial</term><term>Interstitial animals</term><term>Interstitial fauna</term><term>Interstitial habitats</term><term>Interstitial ostracods</term><term>Interstitial spaces</term><term>Interstitial species</term><term>Interstitial xestoleberis species</term><term>Karstic</term><term>Karstic areas</term><term>Laboratory observations</term><term>Lobau wetland</term><term>Long history</term><term>Main channel</term><term>Many species</term><term>Marine ancestor</term><term>Marine ostracods</term><term>Marmonier</term><term>Marmonier ward</term><term>Marten</term><term>Namibcypridini</term><term>Oceanic islands</term><term>Ostracod</term><term>Ostracod case histories</term><term>Ostracod groups</term><term>Ostracoda</term><term>Passive dispersal</term><term>Passive transport</term><term>Phylogenetic lineage</term><term>Phytophilous species</term><term>Platte river</term><term>Rhbne river</term><term>Roca danielopol</term><term>Sandy sediments</term><term>Sediment</term><term>Sonoran desert stream</term><term>Southern texas</term><term>Spatial distribution</term><term>Spatial scales</term><term>Sphaeromicola</term><term>Sphaeromicolinae</term><term>Subsurface</term><term>Subsurface environment</term><term>Subsurface habitats</term><term>Subsurface ostracods</term><term>Subterranean</term><term>Subterranean crustaceans</term><term>Subterranean freshwaters</term><term>Subterranean habitats</term><term>Subterranean taxa</term><term>Surface sediments</term><term>Surface waters</term><term>Sycamore creek</term><term>Taxon</term><term>Taxonomic position</term><term>Tuberoloxoconcha</term><term>Upper messinian</term><term>Various times</term><term>Vicariance</term><term>Vicariance biogeography</term><term>Vicariance model</term><term>Water column</term><term>Wegelini</term><term>West indies</term><term>Western coast</term><term>Wide range</term><term>World distribution</term><term>Worldwide distribution</term><term>Xestoleberis</term><term>Xestoleberis arcturi group</term><term>Xestoleberis arcturi species group</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Active dispersal</term><term>Active migration</term><term>Ancestral species</term><term>Arcturi</term><term>Atlantic ocean</term><term>Biogeography</term><term>Bonaduce</term><term>Boulton</term><term>Candoninae namibcypridini</term><term>Carapace</term><term>Carapace shape</term><term>Cavernocypris</term><term>Central america</term><term>Colonisation</term><term>Colonised</term><term>Common ancestor</term><term>Continental drift</term><term>Costata</term><term>Crustacea</term><term>Danielopol</term><term>Danielopol bonaduce</term><term>Danielopol hart</term><term>Danielopol hartmann</term><term>Danube river</term><term>Defaunated hyporheic sediments</term><term>Desert stream</term><term>Dispersal</term><term>Dispersionist model</term><term>Ecological</term><term>Ecological flexibility</term><term>Ecological processes</term><term>Ecological requirements</term><term>Ecological tolerance</term><term>Ecology</term><term>Epigean</term><term>Fabaeformiscandona wegelini</term><term>Freshwater</term><term>Galapagos</term><term>Galapagos islands</term><term>Genus</term><term>Genus cavernocypris</term><term>Genus hobsiella</term><term>Genus sphaeromicola</term><term>Geographic distribution</term><term>Geological events</term><term>Hobsiella species</term><term>Hyporheic zone</term><term>Interstitial</term><term>Interstitial animals</term><term>Interstitial fauna</term><term>Interstitial habitats</term><term>Interstitial ostracods</term><term>Interstitial spaces</term><term>Interstitial species</term><term>Interstitial xestoleberis species</term><term>Karstic</term><term>Karstic areas</term><term>Laboratory observations</term><term>Lobau wetland</term><term>Long history</term><term>Main channel</term><term>Many species</term><term>Marine ancestor</term><term>Marine ostracods</term><term>Marmonier</term><term>Marmonier ward</term><term>Marten</term><term>Namibcypridini</term><term>Oceanic islands</term><term>Ostracod</term><term>Ostracod case histories</term><term>Ostracod groups</term><term>Ostracoda</term><term>Passive dispersal</term><term>Passive transport</term><term>Phylogenetic lineage</term><term>Phytophilous species</term><term>Platte river</term><term>Rhbne river</term><term>Roca danielopol</term><term>Sandy sediments</term><term>Sediment</term><term>Sonoran desert stream</term><term>Southern texas</term><term>Spatial distribution</term><term>Spatial scales</term><term>Sphaeromicola</term><term>Sphaeromicolinae</term><term>Subsurface</term><term>Subsurface environment</term><term>Subsurface habitats</term><term>Subsurface ostracods</term><term>Subterranean</term><term>Subterranean crustaceans</term><term>Subterranean freshwaters</term><term>Subterranean habitats</term><term>Subterranean taxa</term><term>Surface sediments</term><term>Surface waters</term><term>Sycamore creek</term><term>Taxon</term><term>Taxonomic position</term><term>Tuberoloxoconcha</term><term>Upper messinian</term><term>Various times</term><term>Vicariance</term><term>Vicariance biogeography</term><term>Vicariance model</term><term>Water column</term><term>Wegelini</term><term>West indies</term><term>Western coast</term><term>Wide range</term><term>World distribution</term><term>Worldwide distribution</term><term>Xestoleberis</term><term>Xestoleberis arcturi group</term><term>Xestoleberis arcturi species group</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>écologie</term><term>Eau douce</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Origins of the present day distribution of several freshwater and marine phyletic groups of ostracods are described using both Recent and fossil data. Six examples of subterranean ostracods distributed world-wide are discussed. The first two examples (i.e. the Candoninae Namibcypridini and the Sphaeromicolinae) seemed, in a first approach, to fit well with the ‘vicariance model’ but a detailed study demonstrate that their present day distribution can not be seen as a consequence of any geological events. The four other examples (the Xestoleberis arcturi species group, the Tuberoloxoconcha, the Cavernocypris and Fabaeformiscandona wegelini) fit well with the ‘dispersionist model’. We propose a biogeographical model similar to the dispersal one which foccus on the ecological processes occurring at local and/or regional scales. Some present day species or their epigean ancestors may originally have been more widely dispersed. These species were predisposed to colonize subsurface habitats; a process that could occur polytopically and at various times. It is the degree of ecological flexibility, the width of ecological tolerance, the type of preadaptations, and the capacity to perceive and successfully invade new environments that allow subsurface ostracods to migrate actively or be dispersed passively through both subterranean and epigean aquatic systems and to settle in new places. But no centers of origin and direction of dispersal can be identified in our data. There is little known about the autecology of subterranean ostracod taxa with broad geographical ranges. Samples should be collected at fine (habitat) and broad scales (regional surveys) so that we can better understand the modes of ostracod dispersal across a range of spatial scales.</div></front></TEI><affiliations><list><country><li>Australie</li><li>Autriche</li><li>France</li><li>Italie</li></country><region><li>Auvergne-Rhône-Alpes</li><li>Rhône-Alpes</li></region><settlement><li>Le Bourget du Lac</li></settlement></list><tree><country name="Autriche"><noRegion><name sortKey="Danielopol, D L" sort="Danielopol, D L" uniqKey="Danielopol D" first="D. L." last="Danielopol">D. L. Danielopol</name></noRegion></country><country name="France"><region name="Auvergne-Rhône-Alpes"><name sortKey="Marmonier, P" sort="Marmonier, P" uniqKey="Marmonier P" first="P." last="Marmonier">P. Marmonier</name></region></country><country name="Australie"><noRegion><name sortKey="Boulton, A J" sort="Boulton, A J" uniqKey="Boulton A" first="A. J." last="Boulton">A. J. Boulton</name></noRegion></country><country name="Italie"><noRegion><name sortKey="Bonaduce, G" sort="Bonaduce, G" uniqKey="Bonaduce G" first="G." last="Bonaduce">G. Bonaduce</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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