. Bulletins of American paleontology. Bulletin 351. Ro Gurabo Section Coral Communities ? Q-ass flats ^^ F^efs in deeper, more turbid waters (>10-20 m) T Transported corals Environments Brackish Very shallow marine (<30m) Marine (approximately 30 to 100 m) Text-figure 3.—Part of the Ri'o Gurabo section showing the stratigraphic distributions of Corbiila species. Coral communities are based on average linkage cluster analysis of coral assemblages from Budd el al. (1996). Criteria used to distinguish environmental categories are outlined in Appendix 1. Formation in the Rio Cana section (Te
. Bulletins of American paleontology. Bulletin 351. Ro Gurabo Section Coral Communities ? Q-ass flats ^^ F^efs in deeper, more turbid waters (>10-20 m) T Transported corals Environments Brackish Very shallow marine (<30m) Marine (approximately 30 to 100 m) Text-figure 3.—Part of the Ri'o Gurabo section showing the stratigraphic distributions of Corbiila species. Coral communities are based on average linkage cluster analysis of coral assemblages from Budd el al. (1996). Criteria used to distinguish environmental categories are outlined in Appendix 1. Formation in the Rio Cana section (Text-fig. 2; Ander- son, 1994). Corbula viminea also occurs in brackish- water and shallow-marine to intermediate-marine de- posits in the study area, whereas C. sanctidominici oc- curs primarily in shallow- to intermediate-marine sedi- ments (Text-figs. 2, 3). Corbula canae only occurs in brackish-water deposits of the Rio Cana section, which were probably deposited in or near a mangrove swamp (Text-fig. 2; Anderson, 1994). Corbula sericea and C. sanctidominici also occur in deeper marine sediments. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Paleontological Research Institution (Ithaca, N. Y. ); Columbia University. Ithaca, N. Y. , Paleontological Research Institution [etc. ]
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