Evolution of New Zealand's terrestrial fauna: a review of molecular evidence
New Zealand biogeography has been dominated by the knowledge that its geophysical history is continental in nature. The continental crust (Zealandia) from which New Zealand is formed broke from Gondwanaland ca 80 Ma, and there has existed a pervading view that the native biota is primarily a product...
Gespeichert in:
| Veröffentlicht in: | Philosophical transactions of the Royal Society of London. Series B. Biological sciences 2008-10, Vol.363 (1508), p.3319-3334 |
|---|---|
| Hauptverfasser: | , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 3334 |
|---|---|
| container_issue | 1508 |
| container_start_page | 3319 |
| container_title | Philosophical transactions of the Royal Society of London. Series B. Biological sciences |
| container_volume | 363 |
| creator | Goldberg, Julia Trewick, Steven A Paterson, Adrian M |
| description | New Zealand biogeography has been dominated by the knowledge that its geophysical history is continental in nature. The continental crust (Zealandia) from which New Zealand is formed broke from Gondwanaland ca 80 Ma, and there has existed a pervading view that the native biota is primarily a product of this long isolation. However, molecular studies of terrestrial animals and plants in New Zealand indicate that many taxa arrived since isolation of the land, and that diversification in most groups is relatively recent. This is consistent with evidence for species turnover from the fossil record, taxonomic affinity, tectonic evidence and observations of biological composition and interactions. Extinction, colonization and speciation have yielded a biota in New Zealand which is, in most respects, more like that of an oceanic archipelago than a continent. |
| doi_str_mv | 10.1098/rstb.2008.0114 |
| format | Article |
| fullrecord | <record><control><sourceid>jstor_royal</sourceid><recordid>TN_cdi_jstor_primary_20208748</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><jstor_id>20208748</jstor_id><sourcerecordid>20208748</sourcerecordid><originalsourceid>FETCH-LOGICAL-a710t-788fde28811c587a664adf66a79d17d1be9e89cd9de8c1671bda1d1de9c772433</originalsourceid><addsrcrecordid>eNp9Uk1vEzEUXCEQDYUrN9Ce4LTBH7v-4ICAquUrKhIUhLhYjv22dbpZB3s3Jfx6vN0oECF6suw3M-_NG2fZQ4ymGEnxLMRuPiUIiSnCuLyVTXDJcUEkR7ezCZKMFKKk7CC7F-MCISQrXt7NDrDggnAiJtnseO2bvnO-zX2dn8JV_h10o1v7NOYdhACxC043ea37Vj_PdR5g7RIqgZe-AdM3OuTpyUJr4H52p9ZNhAfb8zD7cnJ8dvS2mH188-7o1azQHKOu4ELUFogQGJtKcM1YqW3NmObSYm7xHCQIaay0IAxmHM-txhZbkIZzUlJ6mL0YdVf9fAnWQNsF3ahVcEsdNsprp_YrrbtQ536tCEOc8ioJPNkKBP-jTx7V0kUDTTIOvo-KyYpWvJIJOB2BJvgYA9S7JhipIQA1BKCGANQQQCI8_nu0P_DtxhOAjoDgN2lH3jjoNmrh-9Cm6_9lL29iffp89npNGXW4GhiCYsTLqqrUL7capVJRuRh7UNeQffl_uz0auy1i58POA0EECV4OHoqx7mIHP3d1HS4VG_arvopSzT6cMoLfn6hvCY9H_IU7v7hyAdSejXRZbUe8Ho5SPGz-5Y2cYWLj2y4lvM9Udd-kv2Br-hu9A_kI</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>69535759</pqid></control><display><type>article</type><title>Evolution of New Zealand's terrestrial fauna: a review of molecular evidence</title><source>Jstor Complete Legacy</source><source>MEDLINE</source><source>PubMed Central</source><creator>Goldberg, Julia ; Trewick, Steven A ; Paterson, Adrian M</creator><creatorcontrib>Goldberg, Julia ; Trewick, Steven A ; Paterson, Adrian M</creatorcontrib><description>New Zealand biogeography has been dominated by the knowledge that its geophysical history is continental in nature. The continental crust (Zealandia) from which New Zealand is formed broke from Gondwanaland ca 80 Ma, and there has existed a pervading view that the native biota is primarily a product of this long isolation. However, molecular studies of terrestrial animals and plants in New Zealand indicate that many taxa arrived since isolation of the land, and that diversification in most groups is relatively recent. This is consistent with evidence for species turnover from the fossil record, taxonomic affinity, tectonic evidence and observations of biological composition and interactions. Extinction, colonization and speciation have yielded a biota in New Zealand which is, in most respects, more like that of an oceanic archipelago than a continent.</description><identifier>ISSN: 0962-8436</identifier><identifier>EISSN: 1471-2970</identifier><identifier>DOI: 10.1098/rstb.2008.0114</identifier><identifier>PMID: 18782728</identifier><language>eng</language><publisher>London: The Royal Society</publisher><subject>Animals ; Biodiversity ; Biogeography ; Biological Evolution ; Biological taxonomies ; Biota ; Demography ; Dispersal ; Evolution ; Fauna ; Fossils ; Geography ; Geology ; Gondwanan ; New Zealand ; Phylogeny ; Phylogeography ; Review ; Species extinction ; Taxa ; Zealandia</subject><ispartof>Philosophical transactions of the Royal Society of London. Series B. Biological sciences, 2008-10, Vol.363 (1508), p.3319-3334</ispartof><rights>Copyright 2008 The Royal Society</rights><rights>2008 The Royal Society</rights><rights>2008 The Royal Society 2008</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a710t-788fde28811c587a664adf66a79d17d1be9e89cd9de8c1671bda1d1de9c772433</citedby><cites>FETCH-LOGICAL-a710t-788fde28811c587a664adf66a79d17d1be9e89cd9de8c1671bda1d1de9c772433</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/20208748$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/20208748$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>230,314,723,776,780,799,881,27901,27902,53766,53768,57992,58225</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/18782728$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Goldberg, Julia</creatorcontrib><creatorcontrib>Trewick, Steven A</creatorcontrib><creatorcontrib>Paterson, Adrian M</creatorcontrib><title>Evolution of New Zealand's terrestrial fauna: a review of molecular evidence</title><title>Philosophical transactions of the Royal Society of London. Series B. Biological sciences</title><addtitle>Philos Trans R Soc Lond B Biol Sci</addtitle><description>New Zealand biogeography has been dominated by the knowledge that its geophysical history is continental in nature. The continental crust (Zealandia) from which New Zealand is formed broke from Gondwanaland ca 80 Ma, and there has existed a pervading view that the native biota is primarily a product of this long isolation. However, molecular studies of terrestrial animals and plants in New Zealand indicate that many taxa arrived since isolation of the land, and that diversification in most groups is relatively recent. This is consistent with evidence for species turnover from the fossil record, taxonomic affinity, tectonic evidence and observations of biological composition and interactions. Extinction, colonization and speciation have yielded a biota in New Zealand which is, in most respects, more like that of an oceanic archipelago than a continent.</description><subject>Animals</subject><subject>Biodiversity</subject><subject>Biogeography</subject><subject>Biological Evolution</subject><subject>Biological taxonomies</subject><subject>Biota</subject><subject>Demography</subject><subject>Dispersal</subject><subject>Evolution</subject><subject>Fauna</subject><subject>Fossils</subject><subject>Geography</subject><subject>Geology</subject><subject>Gondwanan</subject><subject>New Zealand</subject><subject>Phylogeny</subject><subject>Phylogeography</subject><subject>Review</subject><subject>Species extinction</subject><subject>Taxa</subject><subject>Zealandia</subject><issn>0962-8436</issn><issn>1471-2970</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><recordid>eNp9Uk1vEzEUXCEQDYUrN9Ce4LTBH7v-4ICAquUrKhIUhLhYjv22dbpZB3s3Jfx6vN0oECF6suw3M-_NG2fZQ4ymGEnxLMRuPiUIiSnCuLyVTXDJcUEkR7ezCZKMFKKk7CC7F-MCISQrXt7NDrDggnAiJtnseO2bvnO-zX2dn8JV_h10o1v7NOYdhACxC043ea37Vj_PdR5g7RIqgZe-AdM3OuTpyUJr4H52p9ZNhAfb8zD7cnJ8dvS2mH188-7o1azQHKOu4ELUFogQGJtKcM1YqW3NmObSYm7xHCQIaay0IAxmHM-txhZbkIZzUlJ6mL0YdVf9fAnWQNsF3ahVcEsdNsprp_YrrbtQ536tCEOc8ioJPNkKBP-jTx7V0kUDTTIOvo-KyYpWvJIJOB2BJvgYA9S7JhipIQA1BKCGANQQQCI8_nu0P_DtxhOAjoDgN2lH3jjoNmrh-9Cm6_9lL29iffp89npNGXW4GhiCYsTLqqrUL7capVJRuRh7UNeQffl_uz0auy1i58POA0EECV4OHoqx7mIHP3d1HS4VG_arvopSzT6cMoLfn6hvCY9H_IU7v7hyAdSejXRZbUe8Ho5SPGz-5Y2cYWLj2y4lvM9Udd-kv2Br-hu9A_kI</recordid><startdate>20081027</startdate><enddate>20081027</enddate><creator>Goldberg, Julia</creator><creator>Trewick, Steven A</creator><creator>Paterson, Adrian M</creator><general>The Royal Society</general><scope>BSCLL</scope><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope><scope>5PM</scope></search><sort><creationdate>20081027</creationdate><title>Evolution of New Zealand's terrestrial fauna: a review of molecular evidence</title><author>Goldberg, Julia ; Trewick, Steven A ; Paterson, Adrian M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a710t-788fde28811c587a664adf66a79d17d1be9e89cd9de8c1671bda1d1de9c772433</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2008</creationdate><topic>Animals</topic><topic>Biodiversity</topic><topic>Biogeography</topic><topic>Biological Evolution</topic><topic>Biological taxonomies</topic><topic>Biota</topic><topic>Demography</topic><topic>Dispersal</topic><topic>Evolution</topic><topic>Fauna</topic><topic>Fossils</topic><topic>Geography</topic><topic>Geology</topic><topic>Gondwanan</topic><topic>New Zealand</topic><topic>Phylogeny</topic><topic>Phylogeography</topic><topic>Review</topic><topic>Species extinction</topic><topic>Taxa</topic><topic>Zealandia</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Goldberg, Julia</creatorcontrib><creatorcontrib>Trewick, Steven A</creatorcontrib><creatorcontrib>Paterson, Adrian M</creatorcontrib><collection>Istex</collection><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><collection>PubMed Central (Full Participant titles)</collection><jtitle>Philosophical transactions of the Royal Society of London. Series B. Biological sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Goldberg, Julia</au><au>Trewick, Steven A</au><au>Paterson, Adrian M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Evolution of New Zealand's terrestrial fauna: a review of molecular evidence</atitle><jtitle>Philosophical transactions of the Royal Society of London. Series B. Biological sciences</jtitle><addtitle>Philos Trans R Soc Lond B Biol Sci</addtitle><date>2008-10-27</date><risdate>2008</risdate><volume>363</volume><issue>1508</issue><spage>3319</spage><epage>3334</epage><pages>3319-3334</pages><issn>0962-8436</issn><eissn>1471-2970</eissn><abstract>New Zealand biogeography has been dominated by the knowledge that its geophysical history is continental in nature. The continental crust (Zealandia) from which New Zealand is formed broke from Gondwanaland ca 80 Ma, and there has existed a pervading view that the native biota is primarily a product of this long isolation. However, molecular studies of terrestrial animals and plants in New Zealand indicate that many taxa arrived since isolation of the land, and that diversification in most groups is relatively recent. This is consistent with evidence for species turnover from the fossil record, taxonomic affinity, tectonic evidence and observations of biological composition and interactions. Extinction, colonization and speciation have yielded a biota in New Zealand which is, in most respects, more like that of an oceanic archipelago than a continent.</abstract><cop>London</cop><pub>The Royal Society</pub><pmid>18782728</pmid><doi>10.1098/rstb.2008.0114</doi><tpages>16</tpages><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0962-8436 |
| ispartof | Philosophical transactions of the Royal Society of London. Series B. Biological sciences, 2008-10, Vol.363 (1508), p.3319-3334 |
| issn | 0962-8436 1471-2970 |
| language | eng |
| recordid | cdi_jstor_primary_20208748 |
| source | Jstor Complete Legacy; MEDLINE; PubMed Central |
| subjects | Animals Biodiversity Biogeography Biological Evolution Biological taxonomies Biota Demography Dispersal Evolution Fauna Fossils Geography Geology Gondwanan New Zealand Phylogeny Phylogeography Review Species extinction Taxa Zealandia |
| title | Evolution of New Zealand's terrestrial fauna: a review of molecular evidence |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-13T14%3A45%3A03IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstor_royal&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Evolution%20of%20New%20Zealand's%20terrestrial%20fauna:%20a%20review%20of%20molecular%20evidence&rft.jtitle=Philosophical%20transactions%20of%20the%20Royal%20Society%20of%20London.%20Series%20B.%20Biological%20sciences&rft.au=Goldberg,%20Julia&rft.date=2008-10-27&rft.volume=363&rft.issue=1508&rft.spage=3319&rft.epage=3334&rft.pages=3319-3334&rft.issn=0962-8436&rft.eissn=1471-2970&rft_id=info:doi/10.1098/rstb.2008.0114&rft_dat=%3Cjstor_royal%3E20208748%3C/jstor_royal%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=69535759&rft_id=info:pmid/18782728&rft_jstor_id=20208748&rfr_iscdi=true |