. Bulletins of American paleontology. Dominican Republic Neocene. 11: Budd 13 Table I. —List of specimens of Monlaslraea collected by E. and H. Yokes, and measured and used in the statistical analyses. See Saunders, Jung, and Biju-Duval (1986) for detailed descriptions of localities. calatogiie number locality number section species USNM 86898 TU 1231 Rio Gurabo M. endothecata USNM 86899 TU 1422 Rio Cana (Arroyo Bellaco) M. canalis USNM 86900 TU 1354 Rio Cana (Cariada de Zamba) M. limhata USNM 86901 TU 1344 Rio Gurabo M. cylindrica USNM 86902 TU 1405 Rio Yaque del Norte (Arroyo Babosico) M. en
. Bulletins of American paleontology. Dominican Republic Neocene. 11: Budd 13 Table I. —List of specimens of Monlaslraea collected by E. and H. Yokes, and measured and used in the statistical analyses. See Saunders, Jung, and Biju-Duval (1986) for detailed descriptions of localities. calatogiie number locality number section species USNM 86898 TU 1231 Rio Gurabo M. endothecata USNM 86899 TU 1422 Rio Cana (Arroyo Bellaco) M. canalis USNM 86900 TU 1354 Rio Cana (Cariada de Zamba) M. limhata USNM 86901 TU 1344 Rio Gurabo M. cylindrica USNM 86902 TU 1405 Rio Yaque del Norte (Arroyo Babosico) M. endothecata USNM 86903 TU 1405 Rio Yaque del Norte (Arroyo Babosico) M. limbata USNM 86904 TU 1215 Rio Gurabo M. brevis USNM 86905 TU 1246 Rio Gurabo M. brevis USNM 86906 TU 1278 Rio Gurabo M. endothecata USNM 86907 TU 1208 Roadcut 4 km east of Los Quemados M. limbata USNM 86908 TU 1208 Roadcut 4 km east of Los Quemados M. trinitatis USNM 86909 TU 1208 Roadcut 4 km east of Los Quemados M. cavernosa lineages that appear static based on only the NMB material. To evaluate such change adequately, many more specimens of each species need to be collected and measured from the sequence using the NMB lo- cality scheme. With the data at hand, it is difficult to determine if the changes observed in the larger data set are envi- ronmental in origin. Although the Cibao Valley Neo- gene sequence is believed to have been deposited under gradually deepening conditions, some of the material SOLENASTREA g \- o z D Li. o. 900 COMPOSITE SECTION Text-figure 6. — Solenastrea. Variation within species in the corallite character comple,\ distinguishing species through a composite strati- graphic section (constructed by correlating the two sections as in Foster, 1986, 1987). The points (labelled 1 and 2) represent means for every 100 m mterval along the composite section. 1 = S. hyades, 2 = S. bournoni. In each case, standard deviations are smaller than the size of the dot representing the mean for
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