Facies arrangement and cyclostratigraphic architecture of a shallow-marine, warm-water carbonate platform: the Late Carboniferous Ny Friesland Platform in eastern Spitsbergen (Pyefjellet Beds, Wordiekammen Formation, Gipsdalen Group)
During the Late Carboniferous, a spacious warm-water carbonate platform developed across the eastern part of the present Arctic archipelago of Svalbard. The platform initiated in the Moscovian on an uplifted fault block (Ny Friesland High) and progradated during the Late Moscovian to Early Kasimovia...
Gespeichert in:
Veröffentlicht in: | Facies 2009-05, Vol.55 (2), p.291-324 |
---|---|
Hauptverfasser: | , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 324 |
---|---|
container_issue | 2 |
container_start_page | 291 |
container_title | Facies |
container_volume | 55 |
creator | Blomeier, Dierk Scheibner, Christian Forke, Holger |
description | During the Late Carboniferous, a spacious warm-water carbonate platform developed across the eastern part of the present Arctic archipelago of Svalbard. The platform initiated in the Moscovian on an uplifted fault block (Ny Friesland High) and progradated during the Late Moscovian to Early Kasimovian into the adjacent Campbellryggen Basin (central Spitsbergen). The fossiliferous platform strata are characterized by a pronounced cyclicity formed by stacked parasequences, which consist of defined, subtidal to supratidal facies-set successions reflecting a general shallowing of the depositional area. Up to 17 of these shallowing-upward cycles, bounded by distinct discontinuity (marine flooding) surfaces due to the recurrent emersion and subsequent flooding of the platform surface, have been recognized within the platform strata. The stacked cycles are the result of global, glacio-eustatic, high-frequent and high-amplitudinal sea-level fluctuations with eccentricity periodicities caused by ice volume changes during the Gondwana Land glaciation. Based on systematic changes of the cycles (thickness and internal facies composition), the upper part of the platform strata is interpreted as a progradational parasequence set of a late highstand system tract. |
doi_str_mv | 10.1007/s10347-008-0163-3 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_20479993</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1893500021</sourcerecordid><originalsourceid>FETCH-LOGICAL-a412t-6669d35607b26be33a5ea6fc63cb5265233ced9e5256daeeafe641b257f084173</originalsourceid><addsrcrecordid>eNp1kV_L0zAUxosoOF_9AN4dvBCFVfOnTVfvdLgpDH1Bxctymp5umW1Sk4yxj-y3MHUvCIJXCef8znOe5Mmyp5y94oxVrwNnsqhyxlY540rm8l624IqLvFgJdj9bMF6JvOZV_TB7FMKRMVExyRbZrw1qQwHQe7R7GslGQNuBvujBhegxmr3H6WB0QvTBRNLx5AlcDwjhgMPgzvmI3lhawhn9mJ8xkgeNvnU2XWEaMPbOj28gHgh2c2n9p2l68u4U4NMFNj55GOa9t3c0GAuEIUlZ-DKZGFrye7Lw4vZC_ZGGgSK8oy4s4bvznaEfOCbvsEmjybKzS9iaKXQ4pOI2rZlePs4e9DgEenJ33mTfNu-_rj_ku8_bj-u3uxwLLmKulKo7WSpWtUK1JCWWhKrXSuq2FKoUUmrqaipFqTokwp5UwVtRVj1bFbySN9nzq-7k3c8ThdiMJujkGC2l5zaCFVVd1zKBz_4Bj-7kbfLWCKFWhZI1TxC_Qtq7EDz1zeRN-u9Lw1kzJ99ck29S8s2cfDMLi-tMSGwK1f8V_v_QbxYjtpE</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>226846391</pqid></control><display><type>article</type><title>Facies arrangement and cyclostratigraphic architecture of a shallow-marine, warm-water carbonate platform: the Late Carboniferous Ny Friesland Platform in eastern Spitsbergen (Pyefjellet Beds, Wordiekammen Formation, Gipsdalen Group)</title><source>SpringerNature Journals</source><creator>Blomeier, Dierk ; Scheibner, Christian ; Forke, Holger</creator><creatorcontrib>Blomeier, Dierk ; Scheibner, Christian ; Forke, Holger</creatorcontrib><description>During the Late Carboniferous, a spacious warm-water carbonate platform developed across the eastern part of the present Arctic archipelago of Svalbard. The platform initiated in the Moscovian on an uplifted fault block (Ny Friesland High) and progradated during the Late Moscovian to Early Kasimovian into the adjacent Campbellryggen Basin (central Spitsbergen). The fossiliferous platform strata are characterized by a pronounced cyclicity formed by stacked parasequences, which consist of defined, subtidal to supratidal facies-set successions reflecting a general shallowing of the depositional area. Up to 17 of these shallowing-upward cycles, bounded by distinct discontinuity (marine flooding) surfaces due to the recurrent emersion and subsequent flooding of the platform surface, have been recognized within the platform strata. The stacked cycles are the result of global, glacio-eustatic, high-frequent and high-amplitudinal sea-level fluctuations with eccentricity periodicities caused by ice volume changes during the Gondwana Land glaciation. Based on systematic changes of the cycles (thickness and internal facies composition), the upper part of the platform strata is interpreted as a progradational parasequence set of a late highstand system tract.</description><identifier>ISSN: 0172-9179</identifier><identifier>EISSN: 1612-4820</identifier><identifier>DOI: 10.1007/s10347-008-0163-3</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer-Verlag</publisher><subject>Archipelagoes ; Biogeosciences ; Carboniferous ; Earth and Environmental Science ; Earth Sciences ; Ecology ; Geochemistry ; Glaciation ; Marine geology ; Original Article ; Paleontology ; Regions ; Rocks ; Sedimentology ; Studies</subject><ispartof>Facies, 2009-05, Vol.55 (2), p.291-324</ispartof><rights>Springer-Verlag 2008</rights><rights>Springer-Verlag 2009</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a412t-6669d35607b26be33a5ea6fc63cb5265233ced9e5256daeeafe641b257f084173</citedby><cites>FETCH-LOGICAL-a412t-6669d35607b26be33a5ea6fc63cb5265233ced9e5256daeeafe641b257f084173</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10347-008-0163-3$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10347-008-0163-3$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Blomeier, Dierk</creatorcontrib><creatorcontrib>Scheibner, Christian</creatorcontrib><creatorcontrib>Forke, Holger</creatorcontrib><title>Facies arrangement and cyclostratigraphic architecture of a shallow-marine, warm-water carbonate platform: the Late Carboniferous Ny Friesland Platform in eastern Spitsbergen (Pyefjellet Beds, Wordiekammen Formation, Gipsdalen Group)</title><title>Facies</title><addtitle>Facies</addtitle><description>During the Late Carboniferous, a spacious warm-water carbonate platform developed across the eastern part of the present Arctic archipelago of Svalbard. The platform initiated in the Moscovian on an uplifted fault block (Ny Friesland High) and progradated during the Late Moscovian to Early Kasimovian into the adjacent Campbellryggen Basin (central Spitsbergen). The fossiliferous platform strata are characterized by a pronounced cyclicity formed by stacked parasequences, which consist of defined, subtidal to supratidal facies-set successions reflecting a general shallowing of the depositional area. Up to 17 of these shallowing-upward cycles, bounded by distinct discontinuity (marine flooding) surfaces due to the recurrent emersion and subsequent flooding of the platform surface, have been recognized within the platform strata. The stacked cycles are the result of global, glacio-eustatic, high-frequent and high-amplitudinal sea-level fluctuations with eccentricity periodicities caused by ice volume changes during the Gondwana Land glaciation. Based on systematic changes of the cycles (thickness and internal facies composition), the upper part of the platform strata is interpreted as a progradational parasequence set of a late highstand system tract.</description><subject>Archipelagoes</subject><subject>Biogeosciences</subject><subject>Carboniferous</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ecology</subject><subject>Geochemistry</subject><subject>Glaciation</subject><subject>Marine geology</subject><subject>Original Article</subject><subject>Paleontology</subject><subject>Regions</subject><subject>Rocks</subject><subject>Sedimentology</subject><subject>Studies</subject><issn>0172-9179</issn><issn>1612-4820</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kV_L0zAUxosoOF_9AN4dvBCFVfOnTVfvdLgpDH1Bxctymp5umW1Sk4yxj-y3MHUvCIJXCef8znOe5Mmyp5y94oxVrwNnsqhyxlY540rm8l624IqLvFgJdj9bMF6JvOZV_TB7FMKRMVExyRbZrw1qQwHQe7R7GslGQNuBvujBhegxmr3H6WB0QvTBRNLx5AlcDwjhgMPgzvmI3lhawhn9mJ8xkgeNvnU2XWEaMPbOj28gHgh2c2n9p2l68u4U4NMFNj55GOa9t3c0GAuEIUlZ-DKZGFrye7Lw4vZC_ZGGgSK8oy4s4bvznaEfOCbvsEmjybKzS9iaKXQ4pOI2rZlePs4e9DgEenJ33mTfNu-_rj_ku8_bj-u3uxwLLmKulKo7WSpWtUK1JCWWhKrXSuq2FKoUUmrqaipFqTokwp5UwVtRVj1bFbySN9nzq-7k3c8ThdiMJujkGC2l5zaCFVVd1zKBz_4Bj-7kbfLWCKFWhZI1TxC_Qtq7EDz1zeRN-u9Lw1kzJ99ck29S8s2cfDMLi-tMSGwK1f8V_v_QbxYjtpE</recordid><startdate>20090501</startdate><enddate>20090501</enddate><creator>Blomeier, Dierk</creator><creator>Scheibner, Christian</creator><creator>Forke, Holger</creator><general>Springer-Verlag</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2P</scope><scope>M7S</scope><scope>P5Z</scope><scope>P62</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope></search><sort><creationdate>20090501</creationdate><title>Facies arrangement and cyclostratigraphic architecture of a shallow-marine, warm-water carbonate platform: the Late Carboniferous Ny Friesland Platform in eastern Spitsbergen (Pyefjellet Beds, Wordiekammen Formation, Gipsdalen Group)</title><author>Blomeier, Dierk ; Scheibner, Christian ; Forke, Holger</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a412t-6669d35607b26be33a5ea6fc63cb5265233ced9e5256daeeafe641b257f084173</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Archipelagoes</topic><topic>Biogeosciences</topic><topic>Carboniferous</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Ecology</topic><topic>Geochemistry</topic><topic>Glaciation</topic><topic>Marine geology</topic><topic>Original Article</topic><topic>Paleontology</topic><topic>Regions</topic><topic>Rocks</topic><topic>Sedimentology</topic><topic>Studies</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Blomeier, Dierk</creatorcontrib><creatorcontrib>Scheibner, Christian</creatorcontrib><creatorcontrib>Forke, Holger</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Facies</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Blomeier, Dierk</au><au>Scheibner, Christian</au><au>Forke, Holger</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Facies arrangement and cyclostratigraphic architecture of a shallow-marine, warm-water carbonate platform: the Late Carboniferous Ny Friesland Platform in eastern Spitsbergen (Pyefjellet Beds, Wordiekammen Formation, Gipsdalen Group)</atitle><jtitle>Facies</jtitle><stitle>Facies</stitle><date>2009-05-01</date><risdate>2009</risdate><volume>55</volume><issue>2</issue><spage>291</spage><epage>324</epage><pages>291-324</pages><issn>0172-9179</issn><eissn>1612-4820</eissn><abstract>During the Late Carboniferous, a spacious warm-water carbonate platform developed across the eastern part of the present Arctic archipelago of Svalbard. The platform initiated in the Moscovian on an uplifted fault block (Ny Friesland High) and progradated during the Late Moscovian to Early Kasimovian into the adjacent Campbellryggen Basin (central Spitsbergen). The fossiliferous platform strata are characterized by a pronounced cyclicity formed by stacked parasequences, which consist of defined, subtidal to supratidal facies-set successions reflecting a general shallowing of the depositional area. Up to 17 of these shallowing-upward cycles, bounded by distinct discontinuity (marine flooding) surfaces due to the recurrent emersion and subsequent flooding of the platform surface, have been recognized within the platform strata. The stacked cycles are the result of global, glacio-eustatic, high-frequent and high-amplitudinal sea-level fluctuations with eccentricity periodicities caused by ice volume changes during the Gondwana Land glaciation. Based on systematic changes of the cycles (thickness and internal facies composition), the upper part of the platform strata is interpreted as a progradational parasequence set of a late highstand system tract.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer-Verlag</pub><doi>10.1007/s10347-008-0163-3</doi><tpages>34</tpages><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0172-9179 |
ispartof | Facies, 2009-05, Vol.55 (2), p.291-324 |
issn | 0172-9179 1612-4820 |
language | eng |
recordid | cdi_proquest_miscellaneous_20479993 |
source | SpringerNature Journals |
subjects | Archipelagoes Biogeosciences Carboniferous Earth and Environmental Science Earth Sciences Ecology Geochemistry Glaciation Marine geology Original Article Paleontology Regions Rocks Sedimentology Studies |
title | Facies arrangement and cyclostratigraphic architecture of a shallow-marine, warm-water carbonate platform: the Late Carboniferous Ny Friesland Platform in eastern Spitsbergen (Pyefjellet Beds, Wordiekammen Formation, Gipsdalen Group) |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-18T19%3A51%3A43IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Facies%20arrangement%20and%20cyclostratigraphic%20architecture%20of%20a%20shallow-marine,%20warm-water%20carbonate%20platform:%20the%20Late%20Carboniferous%20Ny%20Friesland%20Platform%20in%20eastern%20Spitsbergen%20(Pyefjellet%20Beds,%20Wordiekammen%20Formation,%20Gipsdalen%20Group)&rft.jtitle=Facies&rft.au=Blomeier,%20Dierk&rft.date=2009-05-01&rft.volume=55&rft.issue=2&rft.spage=291&rft.epage=324&rft.pages=291-324&rft.issn=0172-9179&rft.eissn=1612-4820&rft_id=info:doi/10.1007/s10347-008-0163-3&rft_dat=%3Cproquest_cross%3E1893500021%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=226846391&rft_id=info:pmid/&rfr_iscdi=true |