“…For example, micropaleontologists have used plant pollen to document the fossil and modern history of environmental change (Von Post, 1916;1924;Janssen, 1967;Brewster-Wingard and Ishman, 1999;Owens, 2020), while others have used singled-celled protists, such as diatoms and foraminifera, and tiny animals such as ostracodes, to reconstruct past aquatic environments, document pollution, and chart the history of sea level and climate change (e.g., Ehrenberg, 1829;Cleve, 1894;Patrick, 1957;Alve, 1991;Culver and Buzas, 1995;Hallock, 2000;Karlsen et al, 2000;Martin, 2000;Zachos et al, 2001;Cronin et al, 2003;Smol, 2009;Smol and Stoermer, 2010). Freshwater mollusks are also used to examine the history and effects of pollution in rivers and lakes starting in the 1800s (Ortman, 1909;Baker, 1922;van der Schalie, 1936;Ingram, 1957) and continues to this day (Dettman and Lohmann, 1993;Goewert et al, 2007;Lundquist et al, 2019;Kusnerik et al, 2022). The first application of stable isotopes (δ 18 O) for obtaining paleotemperature and climatic records was tested with marine mollusks (Urey et al, 1951;Epstein and Lowenstam, 1953;Valentine and Meade, 1960;Krantz et al, 1987) and as the ability to sample smaller organisms improved, deep-sea foraminifera have given us the best record of Cenozoic climate change (Zachos et al, 2001).…”