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5 results for “Tabulata”

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zenodo40/100

FIG. 4. — Avicenia kocyani n in A new Silurian Avicenia (Tabulata): taxonomy, growth pattern, and colony integration

FIG. 4. — Avicenia kocyani n. sp., paratypes: A, B, specimen (ZPAL T. 26 AVI-2) from Jastrzębia Góra; probably latest Llandovery- Wenlockian; C, D, specimen (ZPAL T. 26 AVI-4) from Kołobrzeg; probably latest Llandovery-Wenlockian; A, C, longitudinal sections; B, D, transverse sections. Scale bars: 500 μm.

opencc-zeroDec 2011View details →
zenodo40/100

FIG. 3 in A new Silurian Avicenia (Tabulata): taxonomy, growth pattern, and colony integration

FIG. 3. — Longitudinal section of Avicenia kocyani n. sp. (holotype; ZPAL T. 26 AVI-1) from the erratic boulder of Międzyzdroje, probably latest Llandovery-Wenlockian: high density zones in corallites (dashed line) do not correspond to high density zones in diaphragm distribution in coenenchymal tubes (continuous line). Scale bar: 500 μm.

opencc-zeroDec 2011View details →
zenodo40/100

FIG. 2 in A new Silurian Avicenia (Tabulata): taxonomy, growth pattern, and colony integration

FIG. 2. — Transverse section of Avicenia kocyani n. sp. (holotype; ZPAL T. 26 AVI-1) from the erratic boulder of Międzyzdroje, probably latest Llandovery-Wenlockian: A, B, general view (notice the dimetrism of corallites and differences in coenenchymal tissue distribution); C, a detail showing the connecting pore, polarized light. Scale bars: 500 μm.

opencc-zeroDec 2011View details →
dryad32/100

Data from: Morphometrics and paleoecology of Catenipora (Tabulata) from the Xiazhen Formation (Upper Ordovician), Zhuzhai, South China

Catenipora is one of the most common tabulate coral genera occurring in various lithofacies in the Upper Ordovician Xiazhen Formation at Zhuzhai in South China. A combination of traditional multivariate analysis and geometric morphometrics is applied to a large number of specimens to distinguish and identify species. Based on three major principal components extracted from 11 morphological characters, three major groups as determined by the cluster-analysis dendrogram are considered to be morphospecies. Their validity and distinctiveness are confirmed by discriminant analysis, descriptive statistics, and bivariate plots. Tabularium area and common wall thickness are the most meaningful characters to distinguish the three morphospecies. Geometric morphometrics is adopted to compare the morphospecies with types and/or figured specimens of species previously reported from the vicinity of Zhuzhai. Despite discrepancies in corallite size, principal component analysis and discriminant analysis, as well as consideration of overall morphological characteristics, indicate that the morphospecies represent C. zhejiangensis Yu in Yu et al., 1963, C. shiyangensis Lin and Chow, 1977, and C. dianbiancunensis Lin and Chow, 1977. Catenipora occurs in seven stratigraphic intervals in the Xiazhen Formation at Zhuzhai, representing a variety of heterogeneous environments. The coralla preservation is variable due to differential compaction; coralla preserved in limestones are commonly intact and in growth position, whereas those in shales are mostly crushed or fragmentary. The size and shape of corallites are considered primarily to be species-specific characters, but are also related to the depositional environments. In all species, morphological characters, including corallite size, septal development, and shape and size of lacunae, show high variability in accordance with lithofacies and stratigraphic position. The intraspecific differences in corallite size at various localities in the Zhuzhai area may indicate responses to local environmental factors, but may also reflect genetic differences if there was limited connection among populations.

opencc-zeroDec 2015View details →
dryad32/100

Data from: Morphometrics and paleoecology of Catenipora (Tabulata) from the Xiazhen Formation (Upper Ordovician), Zhuzhai, South China

Open the record for dataset details and reuse information.

publicFeb 2017View details →

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