A paleozoological perspective on unionid (Mollusca: Unionidae) zoogeography in the upper Trinity River basin, Texas.

In north central Texas, USA, the zoogeography of unionids in the Trinity River is thought to consist of upland and lowland biogeographic components reflective of differences in upstream and downstream hydraulic conditions. Historical and modern surveys from a limited number of localities were used to delineate these zoogeographic provinces based on the absence of several species thought to occur only in the lower Trinity River drainage. Available zooarchaeological data indicate that at least one species considered absent from the upper Trinity River basin was present during the late Holocene (roughly the last 2500 years), suggesting that both biogeographical provinces shared similar mussel fauna in the recent geological past. The discrepancy between historical and zooarchaeological data is probably the result of inadequate sampling and of an extirpation gradient related to impoundments that have been constructed in this drainage during the last century. The presence of lower Trinity species during the late Holocene in the upper Trinity drainage challenges interpretations drawn from modern biogeographic studies.