Sediment-based reconstruction of submersed aquatic vegetation distributionin the Severn River, a sub-estuary of Chesapeake Bay

A paleo-ecological reconstruction of long-term changes in the distribution of submersed aquatic Vegetation (SAV) in a Chesapeake sub-estuary was made using dated sediment cores on transects going from shallow (< 0.5 m) to dee p (> 2 m) waters. Maynedier and Saltworks Creeks, branches of the Severn Ri ver, have had substantial losses of SAV, similar to many parts of the upper Chesapeake Bay. Dating via Pb-210 established that sediment accretion rate s were 0.5-0.7 cm yr(-1) in these two systems, double the rate of sea level rise in this region. Seeds of only two SAV species were found in the sedim ents despite evidence others were present at one time or another in other t ributaries of the Severn Estuary. Of the two species found, Zannichellia pa lustris seeds were much more abundant than Ruppia maritima seeds, reflectin g the high dispersibility of the former species. The vertical pattern of se ed distribution in these cores indicates that over the past 100 years, SAV (particularly Z. palustris) has been increasingly confined to shallower wat er depths. Although there is less riverine pulsing in the two study creeks, than at the head of the Bay (where previous seed records are available), b oth data sets are consistent with the hypothesis that decreasing light avai lability due to eutrophication and sediment erosion has been a problem for SAV in Chesapeake Bay, particularly over the last several decades. Furtherm ore this study suggests that historically low species diversity may be attr ibutable to more chronic and longer term stress in the shallows of the Seve rn River than present in SAV beds at the head of the Bay.