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JOYCE LUCAS-CLARK<br />
Dry Branch units are from the Griffins Landing member of<br />
the Dry Branch. These <strong>as</strong>semblages are characterized by<br />
coleothrighypta, C. variabliis, Glaphyrocysta microfenestrata,<br />
and Samlandia chlamydophora.<br />
Edwards (1990) reported the occurrence of some of the<br />
species herein illustrated, and her reports are consistent with<br />
my findings. In general, the ranges of these dinoflagellate<br />
species at Savannah River Site are consistent with those<br />
reported in the literature. Some exceptions are that Spiniferites<br />
pseudofurcatus is sometimes considered to have its first<br />
occurrence in the Eocene (e.g. Williams and Bujak, 1985),<br />
but it h<strong>as</strong> been reported in unpublished literature from the<br />
Gulf and Atlantic Co<strong>as</strong>tal Plains from the late Paleocene<br />
(e.g. McLean, 1971). Hystrichokolpoma rigaudiae h<strong>as</strong> its<br />
b<strong>as</strong>e, worldwide, in older, lower Eocene rocks, but I have not<br />
found it in the Fishburne. As far <strong>as</strong> I know, the only other<br />
recorded occurrence of C. variabilis is in the late middle<br />
Eocene Barton beds of England, where<strong>as</strong> I have found it in<br />
the upper Eocene Dry Branch.<br />
REFERENCES<br />
Edwards, L.E., 1990. Dinocysts from the lower Tertiary units in the<br />
Savannah River area, South <strong>Carolina</strong> and Georgia, in Zullo,<br />
V.A., W.B. Harris, and V. Price eds. Savannah River Region:<br />
Transition Between the Gulf and Atlantic Co<strong>as</strong>tal Plains, Proceedings<br />
of the second Bald Head Island Conference on Co<strong>as</strong>tal<br />
Plains Geology, p. 97-99.<br />
Fallaw, W.C., V. Price, and P.A. Thayer, 1990. Stratigraphy of the<br />
Savannah River Site, South <strong>Carolina</strong>, in Zullo, V.A., W.B. Harris,<br />
and V. Price eds. Savannah River Region: Transition<br />
Between the Gulf and Atlantic Co<strong>as</strong>tal Plains, Proceedings of<br />
the second Bald Head Island Conference on Co<strong>as</strong>tal Plains<br />
Geology, p. 29-31.<br />
Harris, W.B., and V.A. Zullo, 1990. Sequence Stratigraphy of Paleocene<br />
an Eocene deposits in the Savannah River Region in<br />
Zullo, V.A., W.B. Harris, and V. Price eds. Savannah River<br />
Region: Transition Between the Gulf and Atlantic Co<strong>as</strong>tal<br />
Plains, Proceedings of the second Bald Head Island Conference<br />
on Co<strong>as</strong>tal Plains Geology, p. 134-142.<br />
McLean D.M., 1971. Organic-walled Phytoplankton from the lower<br />
Tertiary Pamunkey Group of Virginia and Maryland [Ph.D. dissertation]:<br />
Stanford University, 165 p.<br />
Prowell, D.C., R.C. Christopher, L.E. Edwards, and H.E. Gill,<br />
1985. Geologic section of the updip Co<strong>as</strong>tal Plain from central<br />
Georgia to western South <strong>Carolina</strong>. U.S. <strong>Geological</strong> Survey<br />
Map MF-1737.<br />
Siple, G.E., 1967. Geology and ground water of the Savannah River<br />
Plant and vicinity, South <strong>Carolina</strong>. U.S. <strong>Geological</strong> Survey<br />
Water Supply Paper 1841, 113 p.<br />
Williams, G.L. and J.P. Bujak, 1985. Mesozoic and Cenozoic<br />
dinoflagellates, in Bolli, H.M., J.B. Saunders, and K. Perch-<br />
Neilsen eds. Plankton Stratigraphy, Cambridge, Cambridge<br />
University Press. P. 847-964.<br />
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