FURONGIAN (LATE CAMBRIAN) SPONGE-MICROBIAL MAZE-LIKE REEFS IN THE NORTH CHINA PLATFORM
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Lee, Jeong-Hyun | - |
dc.contributor.author | Chen, Jitao | - |
dc.contributor.author | Choh, Suk-Joo | - |
dc.contributor.author | Lee, Dong-Jin | - |
dc.contributor.author | Han, Zuozhen | - |
dc.contributor.author | Chough, Sung Kwun | - |
dc.date.accessioned | 2021-09-05T12:54:26Z | - |
dc.date.available | 2021-09-05T12:54:26Z | - |
dc.date.created | 2021-06-15 | - |
dc.date.issued | 2014-01 | - |
dc.identifier.issn | 0883-1351 | - |
dc.identifier.uri | https://scholar.korea.ac.kr/handle/2021.sw.korea/99722 | - |
dc.description.abstract | During the Furongian (late Cambrian) and Early Ordovician, maze-like (maceriate) microbialites flourished in both Laurentia and Gondwana. The maze-like microbialites are characterized by centimeter- to decimeter-scale branching, complex structures. However, organisms responsible for the formation of maze-like structures are poorly known. In order to understand formational processes of maze-like microbialites, this study focuses on the Furongian microbialites of the North China Platform in which microbial components and siliceous sponges co-occur. The maze-like structures consist of microbial components such as microstromatolites, Girvanella, and Renalcis-like forms, as well as sponge spicule networks, whereas lime mud and bioclasts occupy the space between the structures. The maze-like structures developed on a relatively flat seafloor, forming low synoptic relief (<1 cm) above the sediment surface. Continuous growth of maze-like structures with balanced deposition of sediments led to meter-scale bioherms and biostromes, under the control of both microbes and siliceous sponges. This study suggests that siliceous sponges may have played an important role in the construction of maze-like structures between the end-Cambrian Series 2 extinction and the Great Ordovician Biodiversification Event. | - |
dc.language | English | - |
dc.language.iso | en | - |
dc.publisher | SEPM-SOC SEDIMENTARY GEOLOGY | - |
dc.subject | SILICEOUS SPONGE | - |
dc.subject | SHANDONG PROVINCE | - |
dc.subject | LOWER ORDOVICIAN | - |
dc.subject | ANTHASPIDELLID SPONGE | - |
dc.subject | CHAOMIDIAN FORMATION | - |
dc.subject | METAZOAN REEF | - |
dc.subject | SOUTH CHINA | - |
dc.subject | STRATIGRAPHY | - |
dc.subject | CARBONATES | - |
dc.subject | BUILDUPS | - |
dc.title | FURONGIAN (LATE CAMBRIAN) SPONGE-MICROBIAL MAZE-LIKE REEFS IN THE NORTH CHINA PLATFORM | - |
dc.type | Article | - |
dc.contributor.affiliatedAuthor | Lee, Jeong-Hyun | - |
dc.contributor.affiliatedAuthor | Choh, Suk-Joo | - |
dc.identifier.doi | 10.2110/palo.2013.050 | - |
dc.identifier.scopusid | 2-s2.0-84902241509 | - |
dc.identifier.wosid | 000338408300003 | - |
dc.identifier.bibliographicCitation | PALAIOS, v.29, no.1-2, pp.27 - 37 | - |
dc.relation.isPartOf | PALAIOS | - |
dc.citation.title | PALAIOS | - |
dc.citation.volume | 29 | - |
dc.citation.number | 1-2 | - |
dc.citation.startPage | 27 | - |
dc.citation.endPage | 37 | - |
dc.type.rims | ART | - |
dc.type.docType | Article | - |
dc.description.journalClass | 1 | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.relation.journalResearchArea | Geology | - |
dc.relation.journalResearchArea | Paleontology | - |
dc.relation.journalWebOfScienceCategory | Geology | - |
dc.relation.journalWebOfScienceCategory | Paleontology | - |
dc.subject.keywordPlus | SILICEOUS SPONGE | - |
dc.subject.keywordPlus | SHANDONG PROVINCE | - |
dc.subject.keywordPlus | LOWER ORDOVICIAN | - |
dc.subject.keywordPlus | ANTHASPIDELLID SPONGE | - |
dc.subject.keywordPlus | CHAOMIDIAN FORMATION | - |
dc.subject.keywordPlus | METAZOAN REEF | - |
dc.subject.keywordPlus | SOUTH CHINA | - |
dc.subject.keywordPlus | STRATIGRAPHY | - |
dc.subject.keywordPlus | CARBONATES | - |
dc.subject.keywordPlus | BUILDUPS | - |
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