Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Burchard D. Carter"'
Autor:
Burchard D. Carter
Publikováno v:
The Paleontological Society Papers. 3:121-145
Preservational style of fossil echinoid tests allows assessment of the likelihood of post-mortem transport out of the preferred sediment type of the living echinoid. Sedimentologic study of the matrix of untransported specimens allows a check on func
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a500be831355105d8082123c5321572d
https://doi.org/10.1017/s1089332600000231
https://doi.org/10.1017/s1089332600000231
Publikováno v:
Paleobiology. 18:299-325
Faunal similarity among regions is often used as a means of identifying regions of endemism in fossil faunas. At least two large-scale taphonomic effects can affect apparent faunal similarity: stratigraphic and facies mismatching. In stratigraphic mi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e437c50dd9b4186b416c1e408de705c
https://doi.org/10.1017/s0094837300010861
https://doi.org/10.1017/s0094837300010861
Publikováno v:
Journal of Paleontology. 69:588-590
STEPHEN K. DONOVAN,' ROGER W. PORTELL,2 RON K. PICKERILL,3 EDWARD ROBINSON, AND BURCHARD D. CARTER4 'Department of Geology, University of the West Indies, Mona, Kingston 7, Jamaica, 2 Florida Museum of Natural History, University of Florida, Gainesvi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95e5d96b15a89d086e09a8eb46fb813d
https://doi.org/10.1017/s002233600003496x
https://doi.org/10.1017/s002233600003496x
Autor:
Fawzi Hamza, Burchard D. Carter
Publikováno v:
PALAIOS. 9:237
Functional morphology of echinoids, particularly spatangoids, from the Eocene rocks of Egypt suggests a fauna strongly dominated by individuals of species tolerant of fine, impermeable bottom sediments. This might be predicted from the extreme domina
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f5cb1185d157c21c6c09aa1a37b0fcb8
https://doi.org/10.2307/3515200
https://doi.org/10.2307/3515200
Autor:
Burchard D. Carter
Publikováno v:
PALAIOS. 5:176
Combining the substrate preferences of Jacksonian (late Eocene) echinoid species of Florida (Carter et al., 1989) with their geographic distributions (Carter, 1987a) allows construction of biofacies maps reflecting the spatial distribution of carbona
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c077c00de9ffa7df9d5e7b6500eb9870
https://doi.org/10.2307/3514814
https://doi.org/10.2307/3514814
Publikováno v:
Sedimentary Geology. 58:23-36
Black River and Trenton limestones of the outcrop belts in West Virginia and Maryland were deposited on a gentle carbonate ramp that sloped eastward into a deep-water shale basin. The overwhelming sediment type on the ramp was lime mud, laid down bel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::efb27e54f5de9938bf330e04bb02d18a
https://doi.org/10.1016/0037-0738(88)90003-6
https://doi.org/10.1016/0037-0738(88)90003-6
Autor:
Burchard D. Carter
Publikováno v:
Journal of Paleontology. 61:1043-1046
A new species of Brissus is described from the lower Oligocene (Rupelian–Vicksburgian) Bridgeboro limestone of southwestern Georgia. Brissus bridgeboroensis n. sp. most closely resembles the Recent Brissus unicolor (Leske) of the West Indies and th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e36f16fb32929be6d263592ea1293405
https://doi.org/10.1017/s0022336000029383
https://doi.org/10.1017/s0022336000029383
Autor:
Thomas H. Beisel, Burchard D. Carter
Publikováno v:
Journal of Paleontology. 61:1080-1083
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8d66383ce65bf91a99a4250b614a60b5
https://doi.org/10.1017/s0022336000029425
https://doi.org/10.1017/s0022336000029425
Autor:
Timothy M. Chowns, Burchard D. Carter
Middle and Upper Ordovician sediments in northwest Georgia and northeast Alabama can be separated into three facies complexes. The northwestern complex is dominated by shallow water and peritidal carbonates, the central complex by red, peritidal clas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::36e48417f1fcbcf5e357a076b20235af
https://doi.org/10.1306/st29491c2
https://doi.org/10.1306/st29491c2
