Horizontal Plate Motion: A Key Allocyclic Factor in the Evolution of the Great Barrier Reef
The Great Barrier Reef complex of northeastern Australia thins dramatically and becomes younger from north to south. These variations are a consequence of the Cenozoic northward movement of the Indian-Australian plate. The temperate climatic conditions that applied off northeast Australia during the...
Gespeichert in:
| Veröffentlicht in: | Science (American Association for the Advancement of Science) 1987-12, Vol.238 (4834), p.1697-1700 |
|---|---|
| Hauptverfasser: | , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 1700 |
|---|---|
| container_issue | 4834 |
| container_start_page | 1697 |
| container_title | Science (American Association for the Advancement of Science) |
| container_volume | 238 |
| creator | Davies, P. J. Symonds, P. A. Feary, D. A. Pigram, C. J. |
| description | The Great Barrier Reef complex of northeastern Australia thins dramatically and becomes younger from north to south. These variations are a consequence of the Cenozoic northward movement of the Indian-Australian plate. The temperate climatic conditions that applied off northeast Australia during the early Tertiary were progressively replaced by tropical conditions. The present-day south-to-north facies distribution along the eastern Australian continental margin mimics the Cenozoic vertical facies sequence through the northern part of the Great Barrier Reef region. |
| doi_str_mv | 10.1126/science.238.4834.1697 |
| format | Article |
| fullrecord | <record><control><sourceid>gale_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_733194084</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A6251237</galeid><jstor_id>1700641</jstor_id><sourcerecordid>A6251237</sourcerecordid><originalsourceid>FETCH-LOGICAL-a738t-9c08a2a0b410e2738a54477f6c8f9b3802194beccd0c6a680f6d586e395a980f3</originalsourceid><addsrcrecordid>eNqN01tv0zAUB_AIgVgZfANAFg_sYbT4El_CW1dt3UShiNsLD5brnpRUbjxsB1E-PS6tREEVm_IQ5Zyfj2TH_6J4QvCAECpeRttAa2FAmRqUipUDIip5p-gRXPF-RTG7W_QwZqKvsORHxYMYlxjnXsXuF0dESiaFxL3iy6UPzU_fJuPQO2cSoDc-Nb59hYboNazR0Dlv19Y1Fl0Ym3xATYvSV0Dn373rNhL5-ndhHMAkdGZCaCCg9wD1w-JebVyER7v3cfHp4vzj6LI_mY6vRsNJ30imUr-yWBlq8KwkGGguGV6WUtbCqrqaMYUpqcoZWDvHVhihcC3mXAlgFTdV_mLHxcl27nXw3zqISa-aaME504LvopaM5QlYlVk-_69knGJCsLgRUkI4IRW-ERJORd4TzfDZP3Dpu9Dmc8nDGGekVJtpp1u0MA5009Y-BWMX0EIwzrdQN7k8FJQTymTWLw7o_Mxh1dgD_OQvnkWCH2lhuhj11Ye3t5XTz7eVZ-NbSjWe7MvTQ9J652ABOl-d0XRf8622wccYoNbXoVmZsNYE601S9C4pOidFb5KiN0nJ657u_kc3W8H8z6pdNDJ4vAXLmK_9Xh9jURL2C6k7Evk</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>213531480</pqid></control><display><type>article</type><title>Horizontal Plate Motion: A Key Allocyclic Factor in the Evolution of the Great Barrier Reef</title><source>American Association for the Advancement of Science</source><source>Jstor Complete Legacy</source><creator>Davies, P. J. ; Symonds, P. A. ; Feary, D. A. ; Pigram, C. J.</creator><creatorcontrib>Davies, P. J. ; Symonds, P. A. ; Feary, D. A. ; Pigram, C. J.</creatorcontrib><description>The Great Barrier Reef complex of northeastern Australia thins dramatically and becomes younger from north to south. These variations are a consequence of the Cenozoic northward movement of the Indian-Australian plate. The temperate climatic conditions that applied off northeast Australia during the early Tertiary were progressively replaced by tropical conditions. The present-day south-to-north facies distribution along the eastern Australian continental margin mimics the Cenozoic vertical facies sequence through the northern part of the Great Barrier Reef region.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.238.4834.1697</identifier><identifier>PMID: 17737670</identifier><identifier>CODEN: SCIEAS</identifier><language>eng</language><publisher>United States: The American Association for the Advancement of Science</publisher><subject>Climate models ; Coral reefs ; Earth ; Geological facies ; Geology ; Keys ; Marine ; Oceanography ; Oceans ; Paleoclimatology ; Paleogeophysics ; Reefs ; Sediments ; Temperate regions ; Tropical climates ; Tropical regions</subject><ispartof>Science (American Association for the Advancement of Science), 1987-12, Vol.238 (4834), p.1697-1700</ispartof><rights>Copyright 1987 The American Association for the Advancement of Science</rights><rights>COPYRIGHT 1987 American Association for the Advancement of Science</rights><rights>COPYRIGHT 1987 American Association for the Advancement of Science</rights><rights>Copyright American Association for the Advancement of Science Dec 18, 1987</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a738t-9c08a2a0b410e2738a54477f6c8f9b3802194beccd0c6a680f6d586e395a980f3</citedby><cites>FETCH-LOGICAL-a738t-9c08a2a0b410e2738a54477f6c8f9b3802194beccd0c6a680f6d586e395a980f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/1700641$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/1700641$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,2870,2871,27903,27904,57996,58229</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/17737670$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Davies, P. J.</creatorcontrib><creatorcontrib>Symonds, P. A.</creatorcontrib><creatorcontrib>Feary, D. A.</creatorcontrib><creatorcontrib>Pigram, C. J.</creatorcontrib><title>Horizontal Plate Motion: A Key Allocyclic Factor in the Evolution of the Great Barrier Reef</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><description>The Great Barrier Reef complex of northeastern Australia thins dramatically and becomes younger from north to south. These variations are a consequence of the Cenozoic northward movement of the Indian-Australian plate. The temperate climatic conditions that applied off northeast Australia during the early Tertiary were progressively replaced by tropical conditions. The present-day south-to-north facies distribution along the eastern Australian continental margin mimics the Cenozoic vertical facies sequence through the northern part of the Great Barrier Reef region.</description><subject>Climate models</subject><subject>Coral reefs</subject><subject>Earth</subject><subject>Geological facies</subject><subject>Geology</subject><subject>Keys</subject><subject>Marine</subject><subject>Oceanography</subject><subject>Oceans</subject><subject>Paleoclimatology</subject><subject>Paleogeophysics</subject><subject>Reefs</subject><subject>Sediments</subject><subject>Temperate regions</subject><subject>Tropical climates</subject><subject>Tropical regions</subject><issn>0036-8075</issn><issn>1095-9203</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1987</creationdate><recordtype>article</recordtype><recordid>eNqN01tv0zAUB_AIgVgZfANAFg_sYbT4El_CW1dt3UShiNsLD5brnpRUbjxsB1E-PS6tREEVm_IQ5Zyfj2TH_6J4QvCAECpeRttAa2FAmRqUipUDIip5p-gRXPF-RTG7W_QwZqKvsORHxYMYlxjnXsXuF0dESiaFxL3iy6UPzU_fJuPQO2cSoDc-Nb59hYboNazR0Dlv19Y1Fl0Ym3xATYvSV0Dn373rNhL5-ndhHMAkdGZCaCCg9wD1w-JebVyER7v3cfHp4vzj6LI_mY6vRsNJ30imUr-yWBlq8KwkGGguGV6WUtbCqrqaMYUpqcoZWDvHVhihcC3mXAlgFTdV_mLHxcl27nXw3zqISa-aaME504LvopaM5QlYlVk-_69knGJCsLgRUkI4IRW-ERJORd4TzfDZP3Dpu9Dmc8nDGGekVJtpp1u0MA5009Y-BWMX0EIwzrdQN7k8FJQTymTWLw7o_Mxh1dgD_OQvnkWCH2lhuhj11Ye3t5XTz7eVZ-NbSjWe7MvTQ9J652ABOl-d0XRf8622wccYoNbXoVmZsNYE601S9C4pOidFb5KiN0nJ657u_kc3W8H8z6pdNDJ4vAXLmK_9Xh9jURL2C6k7Evk</recordid><startdate>19871218</startdate><enddate>19871218</enddate><creator>Davies, P. J.</creator><creator>Symonds, P. A.</creator><creator>Feary, D. A.</creator><creator>Pigram, C. J.</creator><general>The American Association for the Advancement of Science</general><general>American Association for the Advancement of Science</general><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8GL</scope><scope>IBG</scope><scope>IOV</scope><scope>ISN</scope><scope>7QF</scope><scope>7QG</scope><scope>7QL</scope><scope>7QP</scope><scope>7QQ</scope><scope>7QR</scope><scope>7SC</scope><scope>7SE</scope><scope>7SN</scope><scope>7SP</scope><scope>7SR</scope><scope>7SS</scope><scope>7T7</scope><scope>7TA</scope><scope>7TB</scope><scope>7TK</scope><scope>7TM</scope><scope>7U5</scope><scope>7U9</scope><scope>8BQ</scope><scope>8FD</scope><scope>C1K</scope><scope>F28</scope><scope>FR3</scope><scope>H8D</scope><scope>H8G</scope><scope>H94</scope><scope>JG9</scope><scope>JQ2</scope><scope>K9.</scope><scope>KR7</scope><scope>L7M</scope><scope>L~C</scope><scope>L~D</scope><scope>M7N</scope><scope>P64</scope><scope>RC3</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>7TN</scope><scope>H95</scope><scope>7X8</scope></search><sort><creationdate>19871218</creationdate><title>Horizontal Plate Motion: A Key Allocyclic Factor in the Evolution of the Great Barrier Reef</title><author>Davies, P. J. ; Symonds, P. A. ; Feary, D. A. ; Pigram, C. J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a738t-9c08a2a0b410e2738a54477f6c8f9b3802194beccd0c6a680f6d586e395a980f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1987</creationdate><topic>Climate models</topic><topic>Coral reefs</topic><topic>Earth</topic><topic>Geological facies</topic><topic>Geology</topic><topic>Keys</topic><topic>Marine</topic><topic>Oceanography</topic><topic>Oceans</topic><topic>Paleoclimatology</topic><topic>Paleogeophysics</topic><topic>Reefs</topic><topic>Sediments</topic><topic>Temperate regions</topic><topic>Tropical climates</topic><topic>Tropical regions</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Davies, P. J.</creatorcontrib><creatorcontrib>Symonds, P. A.</creatorcontrib><creatorcontrib>Feary, D. A.</creatorcontrib><creatorcontrib>Pigram, C. J.</creatorcontrib><collection>PubMed</collection><collection>CrossRef</collection><collection>Gale In Context: High School</collection><collection>Gale In Context: Biography</collection><collection>Gale In Context: Opposing Viewpoints</collection><collection>Gale In Context: Canada</collection><collection>Aluminium Industry Abstracts</collection><collection>Animal Behavior Abstracts</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Calcium & Calcified Tissue Abstracts</collection><collection>Ceramic Abstracts</collection><collection>Chemoreception Abstracts</collection><collection>Computer and Information Systems Abstracts</collection><collection>Corrosion Abstracts</collection><collection>Ecology Abstracts</collection><collection>Electronics & Communications Abstracts</collection><collection>Engineered Materials Abstracts</collection><collection>Entomology Abstracts (Full archive)</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Materials Business File</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Neurosciences Abstracts</collection><collection>Nucleic Acids Abstracts</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Virology and AIDS Abstracts</collection><collection>METADEX</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ANTE: Abstracts in New Technology & Engineering</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Copper Technical Reference Library</collection><collection>AIDS and Cancer Research Abstracts</collection><collection>Materials Research Database</collection><collection>ProQuest Computer Science Collection</collection><collection>ProQuest Health & Medical Complete (Alumni)</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Computer and Information Systems Abstracts Academic</collection><collection>Computer and Information Systems Abstracts Professional</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Genetics Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Oceanic Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>MEDLINE - Academic</collection><jtitle>Science (American Association for the Advancement of Science)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Davies, P. J.</au><au>Symonds, P. A.</au><au>Feary, D. A.</au><au>Pigram, C. J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Horizontal Plate Motion: A Key Allocyclic Factor in the Evolution of the Great Barrier Reef</atitle><jtitle>Science (American Association for the Advancement of Science)</jtitle><addtitle>Science</addtitle><date>1987-12-18</date><risdate>1987</risdate><volume>238</volume><issue>4834</issue><spage>1697</spage><epage>1700</epage><pages>1697-1700</pages><issn>0036-8075</issn><eissn>1095-9203</eissn><coden>SCIEAS</coden><abstract>The Great Barrier Reef complex of northeastern Australia thins dramatically and becomes younger from north to south. These variations are a consequence of the Cenozoic northward movement of the Indian-Australian plate. The temperate climatic conditions that applied off northeast Australia during the early Tertiary were progressively replaced by tropical conditions. The present-day south-to-north facies distribution along the eastern Australian continental margin mimics the Cenozoic vertical facies sequence through the northern part of the Great Barrier Reef region.</abstract><cop>United States</cop><pub>The American Association for the Advancement of Science</pub><pmid>17737670</pmid><doi>10.1126/science.238.4834.1697</doi><tpages>4</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0036-8075 |
| ispartof | Science (American Association for the Advancement of Science), 1987-12, Vol.238 (4834), p.1697-1700 |
| issn | 0036-8075 1095-9203 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_733194084 |
| source | American Association for the Advancement of Science; Jstor Complete Legacy |
| subjects | Climate models Coral reefs Earth Geological facies Geology Keys Marine Oceanography Oceans Paleoclimatology Paleogeophysics Reefs Sediments Temperate regions Tropical climates Tropical regions |
| title | Horizontal Plate Motion: A Key Allocyclic Factor in the Evolution of the Great Barrier Reef |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-23T03%3A47%3A57IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Horizontal%20Plate%20Motion:%20A%20Key%20Allocyclic%20Factor%20in%20the%20Evolution%20of%20the%20Great%20Barrier%20Reef&rft.jtitle=Science%20(American%20Association%20for%20the%20Advancement%20of%20Science)&rft.au=Davies,%20P.%20J.&rft.date=1987-12-18&rft.volume=238&rft.issue=4834&rft.spage=1697&rft.epage=1700&rft.pages=1697-1700&rft.issn=0036-8075&rft.eissn=1095-9203&rft.coden=SCIEAS&rft_id=info:doi/10.1126/science.238.4834.1697&rft_dat=%3Cgale_proqu%3EA6251237%3C/gale_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=213531480&rft_id=info:pmid/17737670&rft_galeid=A6251237&rft_jstor_id=1700641&rfr_iscdi=true |