A Study of Diatom Communities in the Upper Main Stem of the Susquehanna River During Various Discharge Regimes, 2014-1016

The upper main stem of the Susquehanna River is formed by the confluence of the West and North Branches, each of which is chemically and physically distinctive. The upper main stem retains the signatures of the two branches due to weak lateral mixing, an

A Longitudinal Study of Diatom Communities at the Confluence, Upper Main Stem, and Tributaries of the Susquehanna River

We analyzed diatom epilithic communities taken in late June 2016 from nine sites, three on the upper main stem of the Susquehanna River (Shady Nook, Port Trevorton, Liverpool), one on the lower North branch (Northumberland), one on the lower West Branch