Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots
Continental aquatic species richness hotspots are unevenly distributed across the planet. In present-day Europe, only two centers of biodiversity exist (Lake Ohrid on the Balkans and the Caspian Sea). During the Neogene, a wide variety of hotspots developed in a series of long-lived lakes. The mecha...
Ausführliche Beschreibung
Autor*in: |
Mathias Harzhauser [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
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2015 |
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Rechteinformationen: |
Nutzungsrecht: © COPYRIGHT 2015 National Academy of Sciences |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: Proceedings of the National Academy of Sciences of the United States of America - Washington, DC : NAS, 1877, 112(2015), 37, Seite 11478-11483 |
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Übergeordnetes Werk: |
volume:112 ; year:2015 ; number:37 ; pages:11478-11483 |
Links: |
Volltext |
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DOI / URN: |
10.1073/pnas.1503992112 |
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520 | |a Continental aquatic species richness hotspots are unevenly distributed across the planet. In present-day Europe, only two centers of biodiversity exist (Lake Ohrid on the Balkans and the Caspian Sea). During the Neogene, a wide variety of hotspots developed in a series of long-lived lakes. The mechanisms underlying the presence of richness hotspots in different geological periods have not been properly examined thus far. Based on Miocene to Recent gastropod distributions, we show that the existence and evolution of such hotspots in inland-water systems are tightly linked to the geodynamic history of the European continent. Both past and present hotspots are related to the formation and persistence of long-lived lake systems in geological basins or to isolation of existing inland basins and embayments from the marine realm. The faunal evolution within hotspots highly depends on warm climates and surface area. During the Quaternary icehouse climate and extensive glaciations, limnic biodiversity sustained a severe decline across the continent and most former hotspots disappeared. The Recent gastropod distribution is mainly a geologically young pattern formed after the Last Glacial Maximum (19 ky) and subsequent formation of postglacial lakes. The major hotspots today are related to long-lived lakes in preglacially formed, permanently subsiding geological basins. | ||
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650 | 4 | |a Gastropoda - physiology | |
650 | 4 | |a Volcanic hotspots | |
650 | 4 | |a Tectonics (Geology) | |
650 | 4 | |a Environmental aspects | |
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10.1073/pnas.1503992112 doi PQ20160211 (DE-627)OLC1970285095 (DE-599)GBVOLC1970285095 (PRQ)c3063-cbe97688187b523537c4f1ca22b6af09706b0da6339ed482e787f8fe5179a4360 (KEY)0583363920150000112003711478tectonicsclimateandtheriseanddemiseofcontinentalaq DE-627 ger DE-627 rakwb eng 500 DNB 570 AVZ LING fid BIODIV fid Mathias Harzhauser verfasserin aut Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Continental aquatic species richness hotspots are unevenly distributed across the planet. In present-day Europe, only two centers of biodiversity exist (Lake Ohrid on the Balkans and the Caspian Sea). During the Neogene, a wide variety of hotspots developed in a series of long-lived lakes. The mechanisms underlying the presence of richness hotspots in different geological periods have not been properly examined thus far. Based on Miocene to Recent gastropod distributions, we show that the existence and evolution of such hotspots in inland-water systems are tightly linked to the geodynamic history of the European continent. Both past and present hotspots are related to the formation and persistence of long-lived lake systems in geological basins or to isolation of existing inland basins and embayments from the marine realm. The faunal evolution within hotspots highly depends on warm climates and surface area. During the Quaternary icehouse climate and extensive glaciations, limnic biodiversity sustained a severe decline across the continent and most former hotspots disappeared. The Recent gastropod distribution is mainly a geologically young pattern formed after the Last Glacial Maximum (19 ky) and subsequent formation of postglacial lakes. The major hotspots today are related to long-lived lakes in preglacially formed, permanently subsiding geological basins. Nutzungsrecht: © COPYRIGHT 2015 National Academy of Sciences Gastropoda - physiology Volcanic hotspots Tectonics (Geology) Environmental aspects Analysis Basins Biological diversity Lakes Aquatic life Cenozoic species-area relationship biogeography Physical Sciences hotspot evolution freshwater gastropods Thomas A. Neubauer oth Andreas Kroh oth Elisavet Georgopoulou oth Oleg Mandic oth Enthalten in Proceedings of the National Academy of Sciences of the United States of America Washington, DC : NAS, 1877 112(2015), 37, Seite 11478-11483 (DE-627)129505269 (DE-600)209104-5 (DE-576)014909189 0027-8424 nnns volume:112 year:2015 number:37 pages:11478-11483 http://dx.doi.org/10.1073/pnas.1503992112 Volltext http://www.pnas.org/content/112/37/11478.abstract http://www.ncbi.nlm.nih.gov/pubmed/26305934 http://search.proquest.com/docview/1714443014 http://www.pubmedcentral.nih.gov/articlerender.fcgi?artid=4577204&tool=pmcentrez&rendertype=abstract GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-MAT SSG-OPC-FOR GBV_ILN_40 GBV_ILN_59 AR 112 2015 37 11478-11483 |
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10.1073/pnas.1503992112 doi PQ20160211 (DE-627)OLC1970285095 (DE-599)GBVOLC1970285095 (PRQ)c3063-cbe97688187b523537c4f1ca22b6af09706b0da6339ed482e787f8fe5179a4360 (KEY)0583363920150000112003711478tectonicsclimateandtheriseanddemiseofcontinentalaq DE-627 ger DE-627 rakwb eng 500 DNB 570 AVZ LING fid BIODIV fid Mathias Harzhauser verfasserin aut Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Continental aquatic species richness hotspots are unevenly distributed across the planet. In present-day Europe, only two centers of biodiversity exist (Lake Ohrid on the Balkans and the Caspian Sea). During the Neogene, a wide variety of hotspots developed in a series of long-lived lakes. The mechanisms underlying the presence of richness hotspots in different geological periods have not been properly examined thus far. Based on Miocene to Recent gastropod distributions, we show that the existence and evolution of such hotspots in inland-water systems are tightly linked to the geodynamic history of the European continent. Both past and present hotspots are related to the formation and persistence of long-lived lake systems in geological basins or to isolation of existing inland basins and embayments from the marine realm. The faunal evolution within hotspots highly depends on warm climates and surface area. During the Quaternary icehouse climate and extensive glaciations, limnic biodiversity sustained a severe decline across the continent and most former hotspots disappeared. The Recent gastropod distribution is mainly a geologically young pattern formed after the Last Glacial Maximum (19 ky) and subsequent formation of postglacial lakes. The major hotspots today are related to long-lived lakes in preglacially formed, permanently subsiding geological basins. Nutzungsrecht: © COPYRIGHT 2015 National Academy of Sciences Gastropoda - physiology Volcanic hotspots Tectonics (Geology) Environmental aspects Analysis Basins Biological diversity Lakes Aquatic life Cenozoic species-area relationship biogeography Physical Sciences hotspot evolution freshwater gastropods Thomas A. Neubauer oth Andreas Kroh oth Elisavet Georgopoulou oth Oleg Mandic oth Enthalten in Proceedings of the National Academy of Sciences of the United States of America Washington, DC : NAS, 1877 112(2015), 37, Seite 11478-11483 (DE-627)129505269 (DE-600)209104-5 (DE-576)014909189 0027-8424 nnns volume:112 year:2015 number:37 pages:11478-11483 http://dx.doi.org/10.1073/pnas.1503992112 Volltext http://www.pnas.org/content/112/37/11478.abstract http://www.ncbi.nlm.nih.gov/pubmed/26305934 http://search.proquest.com/docview/1714443014 http://www.pubmedcentral.nih.gov/articlerender.fcgi?artid=4577204&tool=pmcentrez&rendertype=abstract GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-MAT SSG-OPC-FOR GBV_ILN_40 GBV_ILN_59 AR 112 2015 37 11478-11483 |
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10.1073/pnas.1503992112 doi PQ20160211 (DE-627)OLC1970285095 (DE-599)GBVOLC1970285095 (PRQ)c3063-cbe97688187b523537c4f1ca22b6af09706b0da6339ed482e787f8fe5179a4360 (KEY)0583363920150000112003711478tectonicsclimateandtheriseanddemiseofcontinentalaq DE-627 ger DE-627 rakwb eng 500 DNB 570 AVZ LING fid BIODIV fid Mathias Harzhauser verfasserin aut Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Continental aquatic species richness hotspots are unevenly distributed across the planet. In present-day Europe, only two centers of biodiversity exist (Lake Ohrid on the Balkans and the Caspian Sea). During the Neogene, a wide variety of hotspots developed in a series of long-lived lakes. The mechanisms underlying the presence of richness hotspots in different geological periods have not been properly examined thus far. Based on Miocene to Recent gastropod distributions, we show that the existence and evolution of such hotspots in inland-water systems are tightly linked to the geodynamic history of the European continent. Both past and present hotspots are related to the formation and persistence of long-lived lake systems in geological basins or to isolation of existing inland basins and embayments from the marine realm. The faunal evolution within hotspots highly depends on warm climates and surface area. During the Quaternary icehouse climate and extensive glaciations, limnic biodiversity sustained a severe decline across the continent and most former hotspots disappeared. The Recent gastropod distribution is mainly a geologically young pattern formed after the Last Glacial Maximum (19 ky) and subsequent formation of postglacial lakes. The major hotspots today are related to long-lived lakes in preglacially formed, permanently subsiding geological basins. Nutzungsrecht: © COPYRIGHT 2015 National Academy of Sciences Gastropoda - physiology Volcanic hotspots Tectonics (Geology) Environmental aspects Analysis Basins Biological diversity Lakes Aquatic life Cenozoic species-area relationship biogeography Physical Sciences hotspot evolution freshwater gastropods Thomas A. Neubauer oth Andreas Kroh oth Elisavet Georgopoulou oth Oleg Mandic oth Enthalten in Proceedings of the National Academy of Sciences of the United States of America Washington, DC : NAS, 1877 112(2015), 37, Seite 11478-11483 (DE-627)129505269 (DE-600)209104-5 (DE-576)014909189 0027-8424 nnns volume:112 year:2015 number:37 pages:11478-11483 http://dx.doi.org/10.1073/pnas.1503992112 Volltext http://www.pnas.org/content/112/37/11478.abstract http://www.ncbi.nlm.nih.gov/pubmed/26305934 http://search.proquest.com/docview/1714443014 http://www.pubmedcentral.nih.gov/articlerender.fcgi?artid=4577204&tool=pmcentrez&rendertype=abstract GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-MAT SSG-OPC-FOR GBV_ILN_40 GBV_ILN_59 AR 112 2015 37 11478-11483 |
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10.1073/pnas.1503992112 doi PQ20160211 (DE-627)OLC1970285095 (DE-599)GBVOLC1970285095 (PRQ)c3063-cbe97688187b523537c4f1ca22b6af09706b0da6339ed482e787f8fe5179a4360 (KEY)0583363920150000112003711478tectonicsclimateandtheriseanddemiseofcontinentalaq DE-627 ger DE-627 rakwb eng 500 DNB 570 AVZ LING fid BIODIV fid Mathias Harzhauser verfasserin aut Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Continental aquatic species richness hotspots are unevenly distributed across the planet. In present-day Europe, only two centers of biodiversity exist (Lake Ohrid on the Balkans and the Caspian Sea). During the Neogene, a wide variety of hotspots developed in a series of long-lived lakes. The mechanisms underlying the presence of richness hotspots in different geological periods have not been properly examined thus far. Based on Miocene to Recent gastropod distributions, we show that the existence and evolution of such hotspots in inland-water systems are tightly linked to the geodynamic history of the European continent. Both past and present hotspots are related to the formation and persistence of long-lived lake systems in geological basins or to isolation of existing inland basins and embayments from the marine realm. The faunal evolution within hotspots highly depends on warm climates and surface area. During the Quaternary icehouse climate and extensive glaciations, limnic biodiversity sustained a severe decline across the continent and most former hotspots disappeared. The Recent gastropod distribution is mainly a geologically young pattern formed after the Last Glacial Maximum (19 ky) and subsequent formation of postglacial lakes. The major hotspots today are related to long-lived lakes in preglacially formed, permanently subsiding geological basins. Nutzungsrecht: © COPYRIGHT 2015 National Academy of Sciences Gastropoda - physiology Volcanic hotspots Tectonics (Geology) Environmental aspects Analysis Basins Biological diversity Lakes Aquatic life Cenozoic species-area relationship biogeography Physical Sciences hotspot evolution freshwater gastropods Thomas A. Neubauer oth Andreas Kroh oth Elisavet Georgopoulou oth Oleg Mandic oth Enthalten in Proceedings of the National Academy of Sciences of the United States of America Washington, DC : NAS, 1877 112(2015), 37, Seite 11478-11483 (DE-627)129505269 (DE-600)209104-5 (DE-576)014909189 0027-8424 nnns volume:112 year:2015 number:37 pages:11478-11483 http://dx.doi.org/10.1073/pnas.1503992112 Volltext http://www.pnas.org/content/112/37/11478.abstract http://www.ncbi.nlm.nih.gov/pubmed/26305934 http://search.proquest.com/docview/1714443014 http://www.pubmedcentral.nih.gov/articlerender.fcgi?artid=4577204&tool=pmcentrez&rendertype=abstract GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-MAT SSG-OPC-FOR GBV_ILN_40 GBV_ILN_59 AR 112 2015 37 11478-11483 |
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10.1073/pnas.1503992112 doi PQ20160211 (DE-627)OLC1970285095 (DE-599)GBVOLC1970285095 (PRQ)c3063-cbe97688187b523537c4f1ca22b6af09706b0da6339ed482e787f8fe5179a4360 (KEY)0583363920150000112003711478tectonicsclimateandtheriseanddemiseofcontinentalaq DE-627 ger DE-627 rakwb eng 500 DNB 570 AVZ LING fid BIODIV fid Mathias Harzhauser verfasserin aut Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Continental aquatic species richness hotspots are unevenly distributed across the planet. In present-day Europe, only two centers of biodiversity exist (Lake Ohrid on the Balkans and the Caspian Sea). During the Neogene, a wide variety of hotspots developed in a series of long-lived lakes. The mechanisms underlying the presence of richness hotspots in different geological periods have not been properly examined thus far. Based on Miocene to Recent gastropod distributions, we show that the existence and evolution of such hotspots in inland-water systems are tightly linked to the geodynamic history of the European continent. Both past and present hotspots are related to the formation and persistence of long-lived lake systems in geological basins or to isolation of existing inland basins and embayments from the marine realm. The faunal evolution within hotspots highly depends on warm climates and surface area. During the Quaternary icehouse climate and extensive glaciations, limnic biodiversity sustained a severe decline across the continent and most former hotspots disappeared. The Recent gastropod distribution is mainly a geologically young pattern formed after the Last Glacial Maximum (19 ky) and subsequent formation of postglacial lakes. The major hotspots today are related to long-lived lakes in preglacially formed, permanently subsiding geological basins. Nutzungsrecht: © COPYRIGHT 2015 National Academy of Sciences Gastropoda - physiology Volcanic hotspots Tectonics (Geology) Environmental aspects Analysis Basins Biological diversity Lakes Aquatic life Cenozoic species-area relationship biogeography Physical Sciences hotspot evolution freshwater gastropods Thomas A. Neubauer oth Andreas Kroh oth Elisavet Georgopoulou oth Oleg Mandic oth Enthalten in Proceedings of the National Academy of Sciences of the United States of America Washington, DC : NAS, 1877 112(2015), 37, Seite 11478-11483 (DE-627)129505269 (DE-600)209104-5 (DE-576)014909189 0027-8424 nnns volume:112 year:2015 number:37 pages:11478-11483 http://dx.doi.org/10.1073/pnas.1503992112 Volltext http://www.pnas.org/content/112/37/11478.abstract http://www.ncbi.nlm.nih.gov/pubmed/26305934 http://search.proquest.com/docview/1714443014 http://www.pubmedcentral.nih.gov/articlerender.fcgi?artid=4577204&tool=pmcentrez&rendertype=abstract GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-MAT SSG-OPC-FOR GBV_ILN_40 GBV_ILN_59 AR 112 2015 37 11478-11483 |
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Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots |
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tectonics, climate, and the rise and demise of continental aquatic species richness hotspots |
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Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots |
abstract |
Continental aquatic species richness hotspots are unevenly distributed across the planet. In present-day Europe, only two centers of biodiversity exist (Lake Ohrid on the Balkans and the Caspian Sea). During the Neogene, a wide variety of hotspots developed in a series of long-lived lakes. The mechanisms underlying the presence of richness hotspots in different geological periods have not been properly examined thus far. Based on Miocene to Recent gastropod distributions, we show that the existence and evolution of such hotspots in inland-water systems are tightly linked to the geodynamic history of the European continent. Both past and present hotspots are related to the formation and persistence of long-lived lake systems in geological basins or to isolation of existing inland basins and embayments from the marine realm. The faunal evolution within hotspots highly depends on warm climates and surface area. During the Quaternary icehouse climate and extensive glaciations, limnic biodiversity sustained a severe decline across the continent and most former hotspots disappeared. The Recent gastropod distribution is mainly a geologically young pattern formed after the Last Glacial Maximum (19 ky) and subsequent formation of postglacial lakes. The major hotspots today are related to long-lived lakes in preglacially formed, permanently subsiding geological basins. |
abstractGer |
Continental aquatic species richness hotspots are unevenly distributed across the planet. In present-day Europe, only two centers of biodiversity exist (Lake Ohrid on the Balkans and the Caspian Sea). During the Neogene, a wide variety of hotspots developed in a series of long-lived lakes. The mechanisms underlying the presence of richness hotspots in different geological periods have not been properly examined thus far. Based on Miocene to Recent gastropod distributions, we show that the existence and evolution of such hotspots in inland-water systems are tightly linked to the geodynamic history of the European continent. Both past and present hotspots are related to the formation and persistence of long-lived lake systems in geological basins or to isolation of existing inland basins and embayments from the marine realm. The faunal evolution within hotspots highly depends on warm climates and surface area. During the Quaternary icehouse climate and extensive glaciations, limnic biodiversity sustained a severe decline across the continent and most former hotspots disappeared. The Recent gastropod distribution is mainly a geologically young pattern formed after the Last Glacial Maximum (19 ky) and subsequent formation of postglacial lakes. The major hotspots today are related to long-lived lakes in preglacially formed, permanently subsiding geological basins. |
abstract_unstemmed |
Continental aquatic species richness hotspots are unevenly distributed across the planet. In present-day Europe, only two centers of biodiversity exist (Lake Ohrid on the Balkans and the Caspian Sea). During the Neogene, a wide variety of hotspots developed in a series of long-lived lakes. The mechanisms underlying the presence of richness hotspots in different geological periods have not been properly examined thus far. Based on Miocene to Recent gastropod distributions, we show that the existence and evolution of such hotspots in inland-water systems are tightly linked to the geodynamic history of the European continent. Both past and present hotspots are related to the formation and persistence of long-lived lake systems in geological basins or to isolation of existing inland basins and embayments from the marine realm. The faunal evolution within hotspots highly depends on warm climates and surface area. During the Quaternary icehouse climate and extensive glaciations, limnic biodiversity sustained a severe decline across the continent and most former hotspots disappeared. The Recent gastropod distribution is mainly a geologically young pattern formed after the Last Glacial Maximum (19 ky) and subsequent formation of postglacial lakes. The major hotspots today are related to long-lived lakes in preglacially formed, permanently subsiding geological basins. |
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title_short |
Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots |
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