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11 Heat from the ultramafic rocks that constitute the western third of the Narragansett coastal plain facilitated mobilization of fine grained sediments, which traveled downstream to the plain’s southern margin. The sediments, in turn, were subsequently transported onto the more ‘pure’ tonalite, and gneissic basement rocks of the plain. Consequently, the carbonate-rich sedimentary rocks of the plain were reworked to varying degrees during the Alleghnian orogeny. Paleoecological interpretations are based on the presence of coal-bearing shales and clastic sediments that dominated the sedimentary record of the plain (Mudd 1957; Lekson et al. 1960; Heenen 1968; Wieland and Marsh 1967; Marshall et al. 1970; Kirkwood et al. 1971; Klein and Kostial 2014; Klug and Kostial 2015). Topsoil samples collected in Plainville contain coal, phyllite and carbonaceous shales, and clastic rocks that are similar in color, texture, and mineral content to the coal-bearing rocks of the plain (Marshall et al. 1970; Field et al. 1999; Kirkwood et al. 2001; Klug and Kostial 2015).
12 The outcrop where M. longipes was collected is in a stream channel that is part of a karstic drainage system. Stevens (1923) also noted a stream flowing down-slope from the outcrop where Megapezia longipes was collected. Stream facies is present on the walls of the drainage system, where they have been undercut by a branch from a larger drainage system. Immediately south of the outcrop, proto-karst features have been identified in cross-hatched bedrock (Wieland and Marsh 1967). These features are characterized by outcrops and walls that are composed of carbonate-bearing shales, clastic rocks, and sandstones. Carbonate-bearing sandstone is more prevalent to the south of the outcrop, where such deposits are found in a deeply incised stream channel. Stream facies is not prominent on either side of the outcrop, although it could occur elsewhere along the stream channel. Stream facies, however, are found on the walls of the channel, where the carbonate-bearing bedrock has been undercut.
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