Palaeoclimates and their Modelling: With special reference to the Mesozoic era
The climate of the Earth has undergone many changes and for those times when geologic data are widespread and abundant the Mesozoic appears to have been one of the warmest intervals. This was a time during which the single continent Pangea disintegrated into continental units similar to those of tod...
Gespeichert in:
| Weitere Verfasser: | , , , |
|---|---|
| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Dordrecht
Springer Netherlands
1994
|
| Schlagworte: | |
| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | The climate of the Earth has undergone many changes and for those times when geologic data are widespread and abundant the Mesozoic appears to have been one of the warmest intervals. This was a time during which the single continent Pangea disintegrated into continental units similar to those of today, a time when there were no significant polar ice caps and sea level was generally much higher than at the present time, and a time when dinosaurs apparently dominated terrestrial faunas and the flowering plants evolved. Understanding this alien world, ancestral to ours, is intrinsically interesting, intellectually challenging, and offers opportunities for more effective targeting of sites where commercially important geological resources may be found. It also provides critical insights into the operation of coupled Earth systems (biospheric, atmospheric, hydrospheric and geospheric) under extreme 'greenhouse' conditions, and therefore may have relevance to possible future global change. Our intention in organizing this Discussion Meeting was to bring together those who gather and interpret geologic data with those who model global climates from first principles. The community of workers who study the Quaternary have made significant advances by integrating and comparing palaeodata and climate model experiments. Although we have focused not on the Quaternary 'icehouse' but on the Mesozoic 'hothouse' climate we are well aware that approaches used in the study of the Quaternary may have relevance to earlier times |
| Beschreibung: | 1 Online-Ressource (IX, 140 p) |
| ISBN: | 9789401112543 |
| DOI: | 10.1007/978-94-011-1254-3 |
Internformat
MARC
| LEADER | 00000nmm a2200000zc 4500 | ||
|---|---|---|---|
| 001 | BV045177933 | ||
| 003 | DE-604 | ||
| 005 | 00000000000000.0 | ||
| 007 | cr|uuu---uuuuu | ||
| 008 | 180911s1994 |||| o||u| ||||||eng d | ||
| 020 | |a 9789401112543 |9 978-94-011-1254-3 | ||
| 024 | 7 | |a 10.1007/978-94-011-1254-3 |2 doi | |
| 035 | |a (ZDB-2-EES)978-94-011-1254-3 | ||
| 035 | |a (OCoLC)1053845718 | ||
| 035 | |a (DE-599)BVBBV045177933 | ||
| 040 | |a DE-604 |b ger |e aacr | ||
| 041 | 0 | |a eng | |
| 049 | |a DE-634 | ||
| 082 | 0 | |a 551.5 |2 23 | |
| 245 | 1 | 0 | |a Palaeoclimates and their Modelling |b With special reference to the Mesozoic era |c edited by J. R. L. Allen, B. J. Hoskins, B. W. Sellwood, R. A. Spicer, P. J. Valdes |
| 264 | 1 | |a Dordrecht |b Springer Netherlands |c 1994 | |
| 300 | |a 1 Online-Ressource (IX, 140 p) | ||
| 336 | |b txt |2 rdacontent | ||
| 337 | |b c |2 rdamedia | ||
| 338 | |b cr |2 rdacarrier | ||
| 520 | |a The climate of the Earth has undergone many changes and for those times when geologic data are widespread and abundant the Mesozoic appears to have been one of the warmest intervals. This was a time during which the single continent Pangea disintegrated into continental units similar to those of today, a time when there were no significant polar ice caps and sea level was generally much higher than at the present time, and a time when dinosaurs apparently dominated terrestrial faunas and the flowering plants evolved. Understanding this alien world, ancestral to ours, is intrinsically interesting, intellectually challenging, and offers opportunities for more effective targeting of sites where commercially important geological resources may be found. It also provides critical insights into the operation of coupled Earth systems (biospheric, atmospheric, hydrospheric and geospheric) under extreme 'greenhouse' conditions, and therefore may have relevance to possible future global change. Our intention in organizing this Discussion Meeting was to bring together those who gather and interpret geologic data with those who model global climates from first principles. The community of workers who study the Quaternary have made significant advances by integrating and comparing palaeodata and climate model experiments. Although we have focused not on the Quaternary 'icehouse' but on the Mesozoic 'hothouse' climate we are well aware that approaches used in the study of the Quaternary may have relevance to earlier times | ||
| 650 | 4 | |a Earth Sciences | |
| 650 | 4 | |a Atmospheric Sciences | |
| 650 | 4 | |a Paleontology | |
| 650 | 4 | |a Ecotoxicology | |
| 650 | 4 | |a Evolutionary Biology | |
| 650 | 4 | |a Earth sciences | |
| 650 | 4 | |a Paleontology | |
| 650 | 4 | |a Atmospheric sciences | |
| 650 | 4 | |a Evolutionary biology | |
| 650 | 4 | |a Ecotoxicology | |
| 700 | 1 | |a Allen, J. R. L. |4 edt | |
| 700 | 1 | |a Hoskins, B. J. |4 edt | |
| 700 | 1 | |a Sellwood, B. W. |4 edt | |
| 700 | 1 | |a Spicer, R. A. |4 edt | |
| 776 | 0 | 8 | |i Erscheint auch als |n Druck-Ausgabe |z 9789401045469 |
| 856 | 4 | 0 | |u https://doi.org/10.1007/978-94-011-1254-3 |x Verlag |z URL des Erstveröffentlichers |3 Volltext |
| 912 | |a ZDB-2-EES | ||
| 940 | 1 | |q ZDB-2-EES_Archiv | |
| 999 | |a oai:aleph.bib-bvb.de:BVB01-030567163 | ||
| 966 | e | |u https://doi.org/10.1007/978-94-011-1254-3 |l BTU01 |p ZDB-2-EES |q ZDB-2-EES_Archiv |x Verlag |3 Volltext | |
Datensatz im Suchindex
| _version_ | 1804178867538100224 |
|---|---|
| any_adam_object | |
| author2 | Allen, J. R. L. Hoskins, B. J. Sellwood, B. W. Spicer, R. A. |
| author2_role | edt edt edt edt |
| author2_variant | j r l a jrl jrla b j h bj bjh b w s bw bws r a s ra ras |
| author_facet | Allen, J. R. L. Hoskins, B. J. Sellwood, B. W. Spicer, R. A. |
| building | Verbundindex |
| bvnumber | BV045177933 |
| collection | ZDB-2-EES |
| ctrlnum | (ZDB-2-EES)978-94-011-1254-3 (OCoLC)1053845718 (DE-599)BVBBV045177933 |
| dewey-full | 551.5 |
| dewey-hundreds | 500 - Natural sciences and mathematics |
| dewey-ones | 551 - Geology, hydrology, meteorology |
| dewey-raw | 551.5 |
| dewey-search | 551.5 |
| dewey-sort | 3551.5 |
| dewey-tens | 550 - Earth sciences |
| discipline | Geologie / Paläontologie |
| doi_str_mv | 10.1007/978-94-011-1254-3 |
| format | Electronic eBook |
| fullrecord | <?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>03285nmm a2200517zc 4500</leader><controlfield tag="001">BV045177933</controlfield><controlfield tag="003">DE-604</controlfield><controlfield tag="005">00000000000000.0</controlfield><controlfield tag="007">cr|uuu---uuuuu</controlfield><controlfield tag="008">180911s1994 |||| o||u| ||||||eng d</controlfield><datafield tag="020" ind1=" " ind2=" "><subfield code="a">9789401112543</subfield><subfield code="9">978-94-011-1254-3</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/978-94-011-1254-3</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ZDB-2-EES)978-94-011-1254-3</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)1053845718</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)BVBBV045177933</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-604</subfield><subfield code="b">ger</subfield><subfield code="e">aacr</subfield></datafield><datafield tag="041" ind1="0" ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="049" ind1=" " ind2=" "><subfield code="a">DE-634</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">551.5</subfield><subfield code="2">23</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Palaeoclimates and their Modelling</subfield><subfield code="b">With special reference to the Mesozoic era</subfield><subfield code="c">edited by J. R. L. Allen, B. J. Hoskins, B. W. Sellwood, R. A. Spicer, P. J. Valdes</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Dordrecht</subfield><subfield code="b">Springer Netherlands</subfield><subfield code="c">1994</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (IX, 140 p)</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The climate of the Earth has undergone many changes and for those times when geologic data are widespread and abundant the Mesozoic appears to have been one of the warmest intervals. This was a time during which the single continent Pangea disintegrated into continental units similar to those of today, a time when there were no significant polar ice caps and sea level was generally much higher than at the present time, and a time when dinosaurs apparently dominated terrestrial faunas and the flowering plants evolved. Understanding this alien world, ancestral to ours, is intrinsically interesting, intellectually challenging, and offers opportunities for more effective targeting of sites where commercially important geological resources may be found. It also provides critical insights into the operation of coupled Earth systems (biospheric, atmospheric, hydrospheric and geospheric) under extreme 'greenhouse' conditions, and therefore may have relevance to possible future global change. Our intention in organizing this Discussion Meeting was to bring together those who gather and interpret geologic data with those who model global climates from first principles. The community of workers who study the Quaternary have made significant advances by integrating and comparing palaeodata and climate model experiments. Although we have focused not on the Quaternary 'icehouse' but on the Mesozoic 'hothouse' climate we are well aware that approaches used in the study of the Quaternary may have relevance to earlier times</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth Sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Atmospheric Sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Paleontology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ecotoxicology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Evolutionary Biology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Paleontology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Atmospheric sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Evolutionary biology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ecotoxicology</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Allen, J. R. L.</subfield><subfield code="4">edt</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Hoskins, B. J.</subfield><subfield code="4">edt</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sellwood, B. W.</subfield><subfield code="4">edt</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Spicer, R. A.</subfield><subfield code="4">edt</subfield></datafield><datafield tag="776" ind1="0" ind2="8"><subfield code="i">Erscheint auch als</subfield><subfield code="n">Druck-Ausgabe</subfield><subfield code="z">9789401045469</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1007/978-94-011-1254-3</subfield><subfield code="x">Verlag</subfield><subfield code="z">URL des Erstveröffentlichers</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-2-EES</subfield></datafield><datafield tag="940" ind1="1" ind2=" "><subfield code="q">ZDB-2-EES_Archiv</subfield></datafield><datafield tag="999" ind1=" " ind2=" "><subfield code="a">oai:aleph.bib-bvb.de:BVB01-030567163</subfield></datafield><datafield tag="966" ind1="e" ind2=" "><subfield code="u">https://doi.org/10.1007/978-94-011-1254-3</subfield><subfield code="l">BTU01</subfield><subfield code="p">ZDB-2-EES</subfield><subfield code="q">ZDB-2-EES_Archiv</subfield><subfield code="x">Verlag</subfield><subfield code="3">Volltext</subfield></datafield></record></collection> |
| id | DE-604.BV045177933 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:48Z |
| institution | BVB |
| isbn | 9789401112543 |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030567163 |
| oclc_num | 1053845718 |
| open_access_boolean | |
| owner | DE-634 |
| owner_facet | DE-634 |
| physical | 1 Online-Ressource (IX, 140 p) |
| psigel | ZDB-2-EES ZDB-2-EES_Archiv ZDB-2-EES ZDB-2-EES_Archiv |
| publishDate | 1994 |
| publishDateSearch | 1994 |
| publishDateSort | 1994 |
| publisher | Springer Netherlands |
| record_format | marc |
| spelling | Palaeoclimates and their Modelling With special reference to the Mesozoic era edited by J. R. L. Allen, B. J. Hoskins, B. W. Sellwood, R. A. Spicer, P. J. Valdes Dordrecht Springer Netherlands 1994 1 Online-Ressource (IX, 140 p) txt rdacontent c rdamedia cr rdacarrier The climate of the Earth has undergone many changes and for those times when geologic data are widespread and abundant the Mesozoic appears to have been one of the warmest intervals. This was a time during which the single continent Pangea disintegrated into continental units similar to those of today, a time when there were no significant polar ice caps and sea level was generally much higher than at the present time, and a time when dinosaurs apparently dominated terrestrial faunas and the flowering plants evolved. Understanding this alien world, ancestral to ours, is intrinsically interesting, intellectually challenging, and offers opportunities for more effective targeting of sites where commercially important geological resources may be found. It also provides critical insights into the operation of coupled Earth systems (biospheric, atmospheric, hydrospheric and geospheric) under extreme 'greenhouse' conditions, and therefore may have relevance to possible future global change. Our intention in organizing this Discussion Meeting was to bring together those who gather and interpret geologic data with those who model global climates from first principles. The community of workers who study the Quaternary have made significant advances by integrating and comparing palaeodata and climate model experiments. Although we have focused not on the Quaternary 'icehouse' but on the Mesozoic 'hothouse' climate we are well aware that approaches used in the study of the Quaternary may have relevance to earlier times Earth Sciences Atmospheric Sciences Paleontology Ecotoxicology Evolutionary Biology Earth sciences Atmospheric sciences Evolutionary biology Allen, J. R. L. edt Hoskins, B. J. edt Sellwood, B. W. edt Spicer, R. A. edt Erscheint auch als Druck-Ausgabe 9789401045469 https://doi.org/10.1007/978-94-011-1254-3 Verlag URL des Erstveröffentlichers Volltext |
| spellingShingle | Palaeoclimates and their Modelling With special reference to the Mesozoic era Earth Sciences Atmospheric Sciences Paleontology Ecotoxicology Evolutionary Biology Earth sciences Atmospheric sciences Evolutionary biology |
| title | Palaeoclimates and their Modelling With special reference to the Mesozoic era |
| title_auth | Palaeoclimates and their Modelling With special reference to the Mesozoic era |
| title_exact_search | Palaeoclimates and their Modelling With special reference to the Mesozoic era |
| title_full | Palaeoclimates and their Modelling With special reference to the Mesozoic era edited by J. R. L. Allen, B. J. Hoskins, B. W. Sellwood, R. A. Spicer, P. J. Valdes |
| title_fullStr | Palaeoclimates and their Modelling With special reference to the Mesozoic era edited by J. R. L. Allen, B. J. Hoskins, B. W. Sellwood, R. A. Spicer, P. J. Valdes |
| title_full_unstemmed | Palaeoclimates and their Modelling With special reference to the Mesozoic era edited by J. R. L. Allen, B. J. Hoskins, B. W. Sellwood, R. A. Spicer, P. J. Valdes |
| title_short | Palaeoclimates and their Modelling |
| title_sort | palaeoclimates and their modelling with special reference to the mesozoic era |
| title_sub | With special reference to the Mesozoic era |
| topic | Earth Sciences Atmospheric Sciences Paleontology Ecotoxicology Evolutionary Biology Earth sciences Atmospheric sciences Evolutionary biology |
| topic_facet | Earth Sciences Atmospheric Sciences Paleontology Ecotoxicology Evolutionary Biology Earth sciences Atmospheric sciences Evolutionary biology |
| url | https://doi.org/10.1007/978-94-011-1254-3 |
| work_keys_str_mv | AT allenjrl palaeoclimatesandtheirmodellingwithspecialreferencetothemesozoicera AT hoskinsbj palaeoclimatesandtheirmodellingwithspecialreferencetothemesozoicera AT sellwoodbw palaeoclimatesandtheirmodellingwithspecialreferencetothemesozoicera AT spicerra palaeoclimatesandtheirmodellingwithspecialreferencetothemesozoicera |