Douglas Lake Member

The type locality of the Douglas Lake Member lies on the north shore of Douglas Lake, northeast of Douglas Dam, Jefferson County. It was named by Josiah Bridge for Douglas Lake, Tennessee. == Lithology==

The Douglas Lake Member is composed of a diverse set of sedimentary rocks, including rubble conglomerate, chert conglomerate, and black dolomite. In outcrops along the north shore of Lake Douglas, the chert conglomerate overlies the rubble conglomerate and both of which fill prehistoric sinkholes, called paleokarst, developed in upper surface of the Mascot Dolomite. Up to of black, fine-grained, thick-bedded dolomite fill two large, prehistoric sinkholes and grade upward almost imperceptibly into Lenoir Limestone. At Douglas Dam, the Douglas Lake Member consists of three-part sequence of volcanic ash, conglomerate and shale and / or shaly dolomite that fill one of these ancient sinkholes developed in the Mascot Dolomite of the Knox Group. This prehistoric sinkhole varies between in with and is at least deep. In 1955, the 33 beds were assigned to the Douglas Lake Member of the Lenoir Limestone. This kind of preservation by volcanic ash is paralleled by Silurian Herefordshire Lagerstätte. == Fossils==

File:20200606 Chasmataspis laurencii.png|link=|Reconstruction of chasmataspidid Chasmataspis File:Douglasocaris part.jpg|link=|Fossil of crustacean Douglasocaris At Douglas Dam, the Douglas Lake Member has long been known for its articulated Chasmataspidid Chasmataspsis laurenci and phyllocarid Douglasocaris collinsi. In 2019, he claimed finding compression fossils of a variety of non-vascular land plants, described four taxa of plants, two taxa of fungi and reinterpreted Cestites as a liverwort. While this is accepted in a few studies and review of his book, in 2022 researchers such as paleobotanist Dianne Edwards who studied about Paleozoic plants referred his study and commented "When diagnostic features are absent, such fragmentary organic materials can be misinterpreted, leading to implausible attributions". This is agreed in later review as well, considered to lack sufficient characters to be unequivocally assigned to land plants. == Age ==

The paleokarst depressions occupied by the Douglas Lake Member are part of the Knox Unconformity that separates the Lower Ordovician Knox Group from the Middle Ordovician Chickamauga Group. The Lenoir Limestone is the basal unit of the Chickamauga Group in the Douglas Lake region. In this region, the Knox Unconformity is a highly irregular surface, which appears to represent karst terrain that formed during a 12- to 13-million-year-long period of subaerial exposure that forms a hiatus in sedimentary record between the Sauk and Tippecanoe sequences. This unconformity represents periods of falling relative sea level starting in latter part of the Floian Stage, which halted the accumulation marine sediments of the Knox Group and exposed the region to terrestrial erosion and karstification. It is not until late in the Darriwilian Stage that rises in relative sea level drowned the Douglas Lake region and initiated the accumulation of the marine sediments that now comprise the Lenoir Limestone. Therefore, the Douglas Lake Member and the fossils it contains are younger than the underlying Floian strata and older than the late Darriwilian limestones of the Lenoir Limestone. ==Depositional environment==

At Douglas Dam, the Douglas Lake Member is argued to have accumulated within a within a cenote at a time of lowered sealevel and, based on paleogeographic reconstructions, to have been many kilometers from the sea. Caster and Brooks differently interpreted the environment of deposition at Douglas Dam as being a marine submarine spring fed by an underground channel or system of underground channels from the nearby land. Steinhauff and Walker suggested that a lagoonal marginal marine setting is the most likely. == See also==