Question: What kind of rock do cambarus cryptodytes live near?

full_context: Document 1: Neolissochilus subterraneus: Neolissochilus subterraneus is a species of cyprinid cavefish that is endemic to the Tham Phra Wang Daeng cave in Thailand. The genus name derives from the Greek words "neos", "lissos", and "cheilos"; they mean new, smooth, and lip respectively.
Document 2: Atlantic and Gulf Coastal Plain Province: The Atlantic and Gulf Coastal Plain Province is a coastal plain floristic province within the North American Atlantic Region, a floristic region within the Holarctic Kingdom. It lies to the east and south of the Appalachian Province, from southern Nova Scotia to eastern Texas. The narrow coastal strip in New England widens in New Jersey to a broad plain through the Delmarva Peninsula, Virginia, the Carolinas, southern Georgia, and much of Florida. Along the Mississippi Embayment, the province stretches up to the confluence of the Ohio and Mississippi rivers in Cairo, Illinois. The province can be further subdivided into the Atlantic coastal plain and Gulf coastal plain.
Document 3: Murray crayfish: The Murray crayfish, Euastacus armatus, is a species of freshwater crayfish endemic to Australia that belongs to the family Parastacidae. The Murray crayfish has the largest geographic range of any of the "Euastacus" crayfish in Australia, being found in the Murray and Murrumbidgee Rivers as well as many of their tributaries. Murray crayfish are also known as "Murray River crayfish", "Murray crays", "freshwater crays", "spiny freshwater crays", "spinies" and in the Wagga Wagga region of southern New South Wales they are simply known as "lobsters".
Document 4: Cambarus cryptodytes: Cambarus cryptodytes, the Dougherty Plain cave crayfish or Apalachicola cave crayfish, is a small, freshwater crayfish endemic to Florida and Georgia in the United States. It is an underground species known only from waters associated with the Floridan aquifer.
Document 5: Snake River Aquifer: The Snake River Aquifer is a large reservoir of groundwater underlying the Snake River Plain in the southern part of the U.S. state of Idaho. Most of the water in the aquifer comes from rain and melting snow that flows onto the plain from the Snake River, Big Lost River, Bruneau River, and other watercourses of southern Idaho. Measuring about 400 mi from east to west, it is an important water source for agricultural irrigation in the Plain. The Snake River Aquifer is commonly defined as two separate parts, separated by Salmon Falls Creek. These are the Eastern Snake River Plain Aquifer and Western Snake River Plain Aquifer.
Document 6: Cambarus diogenes: Cambarus diogenes (known as the "devil crayfish", "chimney crayfish", "thunder crawfish" or "meadow crayfish") is a crayfish that grows to be 11.5 cm , not including the claws. It tends to live in wetlands and moist woodlands. They are most active in the summer and spring where they can be found near streams and floodplains near their mud chimney, where they live.
Document 7: The Floridas: The Floridas was a region of the southeastern United States comprising the historical colonies of East Florida and West Florida. The borders of East and West Florida varied. In 1783, when Spain acquired West Florida and re-acquired East Florida from Great Britain through the Peace of Paris (1783), the eastern British boundary of West Florida was the Apalachicola River, but Spain in 1785 moved it eastward to the Suwannee River. The purpose was to transfer San Marcos and the district of Apalachee from East Florida to West Florida. From 1810 to 1813, the United States extended piecemeal control over the part of West Florida that comprised the modern-day Gulf coasts of Alabama and Mississippi and the Florida Parishes of Louisiana. After the ratification of the Adams-Onis Treaty in 1821 the United States combined East Florida and what had been the remaining Spanish-controlled rump of West Florida into the territory that comprised modern-day Florida.
Document 8: List of decapod crustaceans of Dominica: Thirty-two species of decapod crustaceans have been recorded in Dominica, an island nation in the Caribbean Lesser Antilles. They include eighteen species of true crabs (infraorder Brachyura); one species of hermit crab and one species of porcelain crab (infraorder Anomura); and eleven species of freshwater shrimp (infraorder Caridea).
Document 9: Ogallala Aquifer: The Ogallala Aquifer is a shallow water table aquifer surrounded by sand, silt, clay and gravel located beneath the Great Plains in the United States. One of the world's largest aquifers, it underlies an area of approximately 174000 sqmi in portions of eight states (South Dakota, Nebraska, Wyoming, Colorado, Kansas, Oklahoma, New Mexico, and Texas). It was named in 1898 by geologist N. H. Darton from its type locality near the town of Ogallala, Nebraska. The aquifer is part of the High Plains Aquifer System, and rests on the Ogallala Formation, which is the principal geologic unit underlying 80% of the High Plains.
Document 10: Bayou: In usage in the United States, a bayou ( or , from Cajun French) is a body of water typically found in a flat, low-lying area, and can be either an extremely slow-moving stream or river (often with a poorly defined shoreline), or a marshy lake or wetland. The term "bayou" can also refer to a creek whose current reverses daily due to tides and which contains brackish water highly conducive to fish life and plankton. Bayous are commonly found in the Gulf Coast region of the southern United States, notably the Mississippi River Delta, with the states of Louisiana and Texas being famous for them. A bayou is frequently an anabranch or minor braid of a braided channel that is moving much more slowly than the mainstem, often becoming boggy and stagnant. Though fauna varies by region, many bayous are home to crawfish, certain species of shrimp, other shellfish, catfish, frogs, toads, American alligators, American crocodiles, herons, turtles, spoonbills, snakes, leeches, and many other species.
Document 11: Procambarus tenuis: Procambarus tenuis is a species of crayfish in the genus "Procambarus" in the family Cambaridae. It is the only species in the subgenus Procambarus (Tenuicambarus). "P. tenuis" is rare throughout its range, which is restricted to the Ouachita Mountains of Le Flore County, Oklahoma and Polk County, Arkansas.
Document 12: Floridan aquifer: The Floridan aquifer system, composed of the Upper and Lower Floridan aquifers, is a thick sequence of Paleogene carbonate rock which spans an area of about in the southeastern United States. It underlies the entire state of Florida and parts of Alabama, Georgia, Mississippi, and South Carolina.
Document 13: Gulf Coastal Lowlands: The Gulf Coastal Lowlands is a geomorphological province in Florida. The province extends along the coast of the Gulf of Mexico from the western end of the Florida Panhandle to near Ft. Myers in southern Florida. The average width of the province is 40 km. While much of the province is less than 15 m above mean sea level (msl), it rises to about 100 ft above msl along its inland side. It is the largest geomorphological province in Florida. Due to its low elevation, the province was at sea level during warmer periods of the Pliocene and Pleistocene, and features such as ancient dunes and sand bars are found far inland. Marine terraces found in the Gulf Coastal Lowlands include the Silver Bluff [1 ft to 10 ft above mean sea level (msl)], Pamlico [8 ft to 25 ft above msl], Talbot [25 ft to 42 ft above msl], Penholoway [42 ft to 72 ft above msl] and Wicomico [70 ft to 100 ft above msl] terraces.
Document 14: Florida Reef: The Florida Reef (also known as the Great Florida Reef, Florida reefs, Florida Reef Tract and Florida Keys Reef Tract) is the only living coral barrier reef in the continental United States. It is the third largest coral barrier reef system in the world (after the Great Barrier Reef and Belize Barrier Reef). It lies a few miles seaward of the Florida Keys, is about 4 miles (6 to 7 km) wide and extends (along the 20 meter depth contour) 270 km from Fowey Rocks just east of Soldier Key to just south of the Marquesas Keys. The barrier reef tract forms a great arc, concentric with the Florida Keys, with the northern end, in Biscayne National Park, oriented north-south and the western end, south of the Marquesas Keys, oriented east-west. The rest of the reef outside Biscayne National Park lies within John Pennekamp Coral Reef State Park and the Florida Keys National Marine Sanctuary. Isolated coral patch reefs occur northward from Biscayne National Park as far as Stuart, in Martin County. Coral reefs are also found in Dry Tortugas National Park west of the Marquesas Keys. There are more than 6,000 individual reefs in the system. The reefs are 5,000 to 7,000 years old, having developed since sea levels rose following the Wisconsinan glaciation.
Document 15: Southern Appalachian low-elevation pine forest: The Southern Appalachian low-elevation pine forest is a forest system that occurs in Indiana, Kentucky, Tennessee, Alabama, Virginia, North Carolina, South Carolina, and Georgia. It is found in the lower elevations of the southern Appalachian Mountains and adjacent Piedmont and Cumberland Plateau, extending into part of the Interior Low Plateaus.
ground_truth: Paleogene carbonate rock