Please use this identifier to cite or link to this item: http://bura.brunel.ac.uk/handle/2438/10703
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dc.contributor.authorSandström, S-
dc.contributor.authorKershaw, S-
dc.date.accessioned2015-04-30T14:28:41Z-
dc.date.available2008-
dc.date.available2015-04-30T14:28:41Z-
dc.date.issued2008-
dc.identifier.citationActa Palaeontological Polonica, 2008, 53 (2), pp. 293 - 302en_US
dc.identifier.issn0567-7920-
dc.identifier.urihttp://bura.brunel.ac.uk/handle/2438/10703-
dc.description.abstractSix well exposed mid−Ludlow stromatoporoid−dominated reef biostromes in four localities from the Hemse Group in southeastern Gotland, Sweden comprise a stromatoporoid assemblage dominated by four species; Clathrodictyon mohicanum, “Stromatopora” bekkeri, Plectostroma scaniense, and Lophiostroma schmidtii. All biostromes investigated in this area (of approximately 30 km2) are interpreted to belong to a single faunal assemblage forming a dense accumulation of fossils that is probably the best exposed stromatoporoid−rich deposit of the Silurian. The results from this comprehensive study strengthen earlier interpretations of a combination of genetic and environmental control on growth−forms of the stromatoporoids. Growth styles are similar for stromatoporoids in all six biostromes. Differences in biostrome fabric are due to variations in the degree of disturbance by storms. The uniformity of facies and the widespread low−diversity fauna support the view that palaeoenvironmental conditions were similar across the area where these biostromes crop out, and promoted the extraordinary growth of stromatoporoids in this shallow shelf area.en_US
dc.format.extent293 - 302-
dc.language.isoenen_US
dc.subjectStromatoporoidsen_US
dc.subjectPalaeoecologyen_US
dc.subjectDepositional environmenten_US
dc.subjectMorphotypeen_US
dc.subjectSilurianen_US
dc.subjectGotlanden_US
dc.subjectSwedenen_US
dc.titlePalaeobiology, ecology, and distribution of stromatoporoid faunas in biostromes of the mid-Ludlow of Gotlanden_US
dc.typeArticleen_US
dc.identifier.doihttp://dx.doi.org/10.4202/app.2008.0210-
dc.relation.isPartOfActa Palaeontological Polonica-
pubs.issue2-
pubs.issue2-
pubs.volume53-
pubs.volume53-
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