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
Gespeichert in:
| Autor*in: |
Mathias Harzhauser [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2015 |
|---|
| Rechteinformationen: |
Nutzungsrecht: © COPYRIGHT 2015 National Academy of Sciences |
|---|
| Schlagwörter: |
|---|
| 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 |
|---|---|
| Übergeordnetes Werk: |
volume:112 ; year:2015 ; number:37 ; pages:11478-11483 |
| Links: |
Volltext |
|---|
| DOI / URN: |
10.1073/pnas.1503992112 |
|---|
| Katalog-ID: |
OLC1970285095 |
|---|
| LEADER | 01000caa a2200265 4500 | ||
|---|---|---|---|
| 001 | OLC1970285095 | ||
| 003 | DE-627 | ||
| 005 | 20230714175955.0 | ||
| 007 | tu | ||
| 008 | 160211s2015 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1073/pnas.1503992112 |2 doi | |
| 028 | 5 | 2 | |a PQ20160211 |
| 035 | |a (DE-627)OLC1970285095 | ||
| 035 | |a (DE-599)GBVOLC1970285095 | ||
| 035 | |a (PRQ)c3063-cbe97688187b523537c4f1ca22b6af09706b0da6339ed482e787f8fe5179a4360 | ||
| 035 | |a (KEY)0583363920150000112003711478tectonicsclimateandtheriseanddemiseofcontinentalaq | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 500 |q DNB |
| 082 | 0 | 4 | |a 570 |q AVZ |
| 084 | |a LING |2 fid | ||
| 084 | |a BIODIV |2 fid | ||
| 100 | 0 | |a Mathias Harzhauser |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots |
| 264 | 1 | |c 2015 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 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. | ||
| 540 | |a Nutzungsrecht: © COPYRIGHT 2015 National Academy of Sciences | ||
| 650 | 4 | |a Gastropoda - physiology | |
| 650 | 4 | |a Volcanic hotspots | |
| 650 | 4 | |a Tectonics (Geology) | |
| 650 | 4 | |a Environmental aspects | |
| 650 | 4 | |a Analysis | |
| 650 | 4 | |a Basins | |
| 650 | 4 | |a Biological diversity | |
| 650 | 4 | |a Lakes | |
| 650 | 4 | |a Aquatic life | |
| 650 | 4 | |a Cenozoic | |
| 650 | 4 | |a species-area relationship | |
| 650 | 4 | |a biogeography | |
| 650 | 4 | |a Physical Sciences | |
| 650 | 4 | |a hotspot evolution | |
| 650 | 4 | |a freshwater gastropods | |
| 700 | 0 | |a Thomas A. Neubauer |4 oth | |
| 700 | 0 | |a Andreas Kroh |4 oth | |
| 700 | 0 | |a Elisavet Georgopoulou |4 oth | |
| 700 | 0 | |a Oleg Mandic |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |t Proceedings of the National Academy of Sciences of the United States of America |d Washington, DC : NAS, 1877 |g 112(2015), 37, Seite 11478-11483 |w (DE-627)129505269 |w (DE-600)209104-5 |w (DE-576)014909189 |x 0027-8424 |7 nnns |
| 773 | 1 | 8 | |g volume:112 |g year:2015 |g number:37 |g pages:11478-11483 |
| 856 | 4 | 1 | |u http://dx.doi.org/10.1073/pnas.1503992112 |3 Volltext |
| 856 | 4 | 2 | |u http://www.pnas.org/content/112/37/11478.abstract |
| 856 | 4 | 2 | |u http://www.ncbi.nlm.nih.gov/pubmed/26305934 |
| 856 | 4 | 2 | |u http://search.proquest.com/docview/1714443014 |
| 856 | 4 | 2 | |u http://www.pubmedcentral.nih.gov/articlerender.fcgi?artid=4577204&tool=pmcentrez&rendertype=abstract |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a FID-LING | ||
| 912 | |a FID-BIODIV | ||
| 912 | |a SSG-OLC-PHY | ||
| 912 | |a SSG-OLC-CHE | ||
| 912 | |a SSG-OLC-MAT | ||
| 912 | |a SSG-OLC-FOR | ||
| 912 | |a SSG-OLC-PHA | ||
| 912 | |a SSG-OLC-DE-84 | ||
| 912 | |a SSG-OPC-MAT | ||
| 912 | |a SSG-OPC-FOR | ||
| 912 | |a GBV_ILN_40 | ||
| 912 | |a GBV_ILN_59 | ||
| 951 | |a AR | ||
| 952 | |d 112 |j 2015 |e 37 |h 11478-11483 | ||
| author_variant |
m h mh |
|---|---|
| matchkey_str |
article:00278424:2015----::etncciaenteiendmsocnietlqais |
| hierarchy_sort_str |
2015 |
| publishDate |
2015 |
| allfields |
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 |
| spelling |
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 |
| allfields_unstemmed |
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 |
| allfieldsGer |
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 |
| allfieldsSound |
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 |
| language |
English |
| source |
Enthalten in Proceedings of the National Academy of Sciences of the United States of America 112(2015), 37, Seite 11478-11483 volume:112 year:2015 number:37 pages:11478-11483 |
| sourceStr |
Enthalten in Proceedings of the National Academy of Sciences of the United States of America 112(2015), 37, Seite 11478-11483 volume:112 year:2015 number:37 pages:11478-11483 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
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 |
| dewey-raw |
500 |
| isfreeaccess_bool |
false |
| container_title |
Proceedings of the National Academy of Sciences of the United States of America |
| authorswithroles_txt_mv |
Mathias Harzhauser @@aut@@ Thomas A. Neubauer @@oth@@ Andreas Kroh @@oth@@ Elisavet Georgopoulou @@oth@@ Oleg Mandic @@oth@@ |
| publishDateDaySort_date |
2015-01-01T00:00:00Z |
| hierarchy_top_id |
129505269 |
| dewey-sort |
3500 |
| id |
OLC1970285095 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a2200265 4500</leader><controlfield tag="001">OLC1970285095</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230714175955.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">160211s2015 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1073/pnas.1503992112</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20160211</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC1970285095</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC1970285095</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)c3063-cbe97688187b523537c4f1ca22b6af09706b0da6339ed482e787f8fe5179a4360</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0583363920150000112003711478tectonicsclimateandtheriseanddemiseofcontinentalaq</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">500</subfield><subfield code="q">DNB</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">570</subfield><subfield code="q">AVZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">LING</subfield><subfield code="2">fid</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">BIODIV</subfield><subfield code="2">fid</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Mathias Harzhauser</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="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.</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">Nutzungsrecht: © COPYRIGHT 2015 National Academy of Sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Gastropoda - physiology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Volcanic hotspots</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tectonics (Geology)</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Environmental aspects</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Analysis</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Basins</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Biological diversity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Lakes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Aquatic life</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Cenozoic</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">species-area relationship</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">biogeography</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Physical Sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">hotspot evolution</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">freshwater gastropods</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Thomas A. Neubauer</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Andreas Kroh</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Elisavet Georgopoulou</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Oleg Mandic</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Proceedings of the National Academy of Sciences of the United States of America</subfield><subfield code="d">Washington, DC : NAS, 1877</subfield><subfield code="g">112(2015), 37, Seite 11478-11483</subfield><subfield code="w">(DE-627)129505269</subfield><subfield code="w">(DE-600)209104-5</subfield><subfield code="w">(DE-576)014909189</subfield><subfield code="x">0027-8424</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:112</subfield><subfield code="g">year:2015</subfield><subfield code="g">number:37</subfield><subfield code="g">pages:11478-11483</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.1073/pnas.1503992112</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://www.pnas.org/content/112/37/11478.abstract</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://www.ncbi.nlm.nih.gov/pubmed/26305934</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://search.proquest.com/docview/1714443014</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://www.pubmedcentral.nih.gov/articlerender.fcgi?artid=4577204&tool=pmcentrez&rendertype=abstract</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-LING</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-BIODIV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-CHE</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-MAT</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-FOR</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-DE-84</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-MAT</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-FOR</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_59</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">112</subfield><subfield code="j">2015</subfield><subfield code="e">37</subfield><subfield code="h">11478-11483</subfield></datafield></record></collection>
|
| author |
Mathias Harzhauser |
| spellingShingle |
Mathias Harzhauser ddc 500 ddc 570 fid LING fid BIODIV misc Gastropoda - physiology misc Volcanic hotspots misc Tectonics (Geology) misc Environmental aspects misc Analysis misc Basins misc Biological diversity misc Lakes misc Aquatic life misc Cenozoic misc species-area relationship misc biogeography misc Physical Sciences misc hotspot evolution misc freshwater gastropods Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots |
| authorStr |
Mathias Harzhauser |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)129505269 |
| format |
Article |
| dewey-ones |
500 - Natural sciences & mathematics 570 - Life sciences; biology |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0027-8424 |
| topic_title |
500 DNB 570 AVZ LING fid BIODIV fid Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots 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 |
| topic |
ddc 500 ddc 570 fid LING fid BIODIV misc Gastropoda - physiology misc Volcanic hotspots misc Tectonics (Geology) misc Environmental aspects misc Analysis misc Basins misc Biological diversity misc Lakes misc Aquatic life misc Cenozoic misc species-area relationship misc biogeography misc Physical Sciences misc hotspot evolution misc freshwater gastropods |
| topic_unstemmed |
ddc 500 ddc 570 fid LING fid BIODIV misc Gastropoda - physiology misc Volcanic hotspots misc Tectonics (Geology) misc Environmental aspects misc Analysis misc Basins misc Biological diversity misc Lakes misc Aquatic life misc Cenozoic misc species-area relationship misc biogeography misc Physical Sciences misc hotspot evolution misc freshwater gastropods |
| topic_browse |
ddc 500 ddc 570 fid LING fid BIODIV misc Gastropoda - physiology misc Volcanic hotspots misc Tectonics (Geology) misc Environmental aspects misc Analysis misc Basins misc Biological diversity misc Lakes misc Aquatic life misc Cenozoic misc species-area relationship misc biogeography misc Physical Sciences misc hotspot evolution misc freshwater gastropods |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| author2_variant |
t a n tan a k ak e g eg o m om |
| hierarchy_parent_title |
Proceedings of the National Academy of Sciences of the United States of America |
| hierarchy_parent_id |
129505269 |
| dewey-tens |
500 - Science 570 - Life sciences; biology |
| hierarchy_top_title |
Proceedings of the National Academy of Sciences of the United States of America |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)129505269 (DE-600)209104-5 (DE-576)014909189 |
| title |
Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots |
| ctrlnum |
(DE-627)OLC1970285095 (DE-599)GBVOLC1970285095 (PRQ)c3063-cbe97688187b523537c4f1ca22b6af09706b0da6339ed482e787f8fe5179a4360 (KEY)0583363920150000112003711478tectonicsclimateandtheriseanddemiseofcontinentalaq |
| title_full |
Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots |
| author_sort |
Mathias Harzhauser |
| journal |
Proceedings of the National Academy of Sciences of the United States of America |
| journalStr |
Proceedings of the National Academy of Sciences of the United States of America |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2015 |
| contenttype_str_mv |
txt |
| container_start_page |
11478 |
| author_browse |
Mathias Harzhauser |
| container_volume |
112 |
| class |
500 DNB 570 AVZ LING fid BIODIV fid |
| format_se |
Aufsätze |
| author-letter |
Mathias Harzhauser |
| doi_str_mv |
10.1073/pnas.1503992112 |
| dewey-full |
500 570 |
| title_sort |
tectonics, climate, and the rise and demise of continental aquatic species richness hotspots |
| title_auth |
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. |
| collection_details |
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 |
| container_issue |
37 |
| title_short |
Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots |
| url |
http://dx.doi.org/10.1073/pnas.1503992112 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 |
| remote_bool |
false |
| author2 |
Thomas A. Neubauer Andreas Kroh Elisavet Georgopoulou Oleg Mandic |
| author2Str |
Thomas A. Neubauer Andreas Kroh Elisavet Georgopoulou Oleg Mandic |
| ppnlink |
129505269 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth oth oth oth |
| doi_str |
10.1073/pnas.1503992112 |
| up_date |
2024-07-03T14:39:16.161Z |
| _version_ |
1803569128970125313 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a2200265 4500</leader><controlfield tag="001">OLC1970285095</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230714175955.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">160211s2015 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1073/pnas.1503992112</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20160211</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC1970285095</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC1970285095</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)c3063-cbe97688187b523537c4f1ca22b6af09706b0da6339ed482e787f8fe5179a4360</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0583363920150000112003711478tectonicsclimateandtheriseanddemiseofcontinentalaq</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">500</subfield><subfield code="q">DNB</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">570</subfield><subfield code="q">AVZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">LING</subfield><subfield code="2">fid</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">BIODIV</subfield><subfield code="2">fid</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Mathias Harzhauser</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Tectonics, climate, and the rise and demise of continental aquatic species richness hotspots</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="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.</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">Nutzungsrecht: © COPYRIGHT 2015 National Academy of Sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Gastropoda - physiology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Volcanic hotspots</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tectonics (Geology)</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Environmental aspects</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Analysis</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Basins</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Biological diversity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Lakes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Aquatic life</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Cenozoic</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">species-area relationship</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">biogeography</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Physical Sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">hotspot evolution</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">freshwater gastropods</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Thomas A. Neubauer</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Andreas Kroh</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Elisavet Georgopoulou</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Oleg Mandic</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Proceedings of the National Academy of Sciences of the United States of America</subfield><subfield code="d">Washington, DC : NAS, 1877</subfield><subfield code="g">112(2015), 37, Seite 11478-11483</subfield><subfield code="w">(DE-627)129505269</subfield><subfield code="w">(DE-600)209104-5</subfield><subfield code="w">(DE-576)014909189</subfield><subfield code="x">0027-8424</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:112</subfield><subfield code="g">year:2015</subfield><subfield code="g">number:37</subfield><subfield code="g">pages:11478-11483</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.1073/pnas.1503992112</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://www.pnas.org/content/112/37/11478.abstract</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://www.ncbi.nlm.nih.gov/pubmed/26305934</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://search.proquest.com/docview/1714443014</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://www.pubmedcentral.nih.gov/articlerender.fcgi?artid=4577204&tool=pmcentrez&rendertype=abstract</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-LING</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-BIODIV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-CHE</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-MAT</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-FOR</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-DE-84</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-MAT</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-FOR</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_59</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">112</subfield><subfield code="j">2015</subfield><subfield code="e">37</subfield><subfield code="h">11478-11483</subfield></datafield></record></collection>
|
| score |
7.4000015 |