Systematics, Phylogenetics, and Biogeography of Early Mississippian Camerate Crinoids of the Nunn Member, Lake Valley Formation, in south-central New Mexico Elizabeth C. Rhenberg The Lake Valley Formation has long been known for the crinoids that are abundant in the formation. The crinoids were noted in the first descriptions of the formations in the late 1800's, but there has never been a comprehensive study done on the crinoids and as a result there is no complete list of crinoids that existed in south-central New Mexico during the Early Mississippian. Although all subclasses of crinoids are found in the Nunn Member, it is the camerate crinoids that dominate the fauna and will be the focus of this study. Most of the specimens studied came from the Macurda collection from the University of Michigan. This collection was supplemented with specimens from the Laudon collection from the University of New Mexico and additional samples collected in the field. These collections provided more than 7000 specimens to be examined, with approximately 4500 of those being identifiable camerate crinoids. The first chapter of this paper is a systematic review of the camerates. Sixty-one species are recorded from the Nunn Member, five of which are new species: Blairocrinus macurdai, Iotacrinus novamexicana, Agaricocrinus alamogordoensis, Uperocrinus kuesi, and Collicrinus laudoni. An updated list of camerates found in the Lake Valley allows for better understanding and easier comparison of crinoid faunas across North America during this time. Environmental preferences were also examined to see if there was a difference between the faunas found in the shallow water shelf and those found associated with Waulsortian mounds in deeper water. The majority of the camerates found in the Lake Valley Formation are from the Family Actinocrinitidae. This family has been a source of much taxonomic confusion due to generic concepts not equally applied between Europe in North America. The second chapter of this paper objectively defines the actinocrinitids by discrete characters and reevaluates the generic assignments of North American species. A phylogenetic hypothesis is presented for the relationships of the Actinocrinitidae genera based on a parsimony-based analysis and plotted against stratigraphic ranges. Although groupings were revealed in this analysis, the Actinocrinitidae cannot be readily divided into subfamilies. Twenty-one genera of Actinocrinitidae are described, 17 of which are found in North America. A total of 125 species were evaluated of which 34 species and one open-nomenclature taxon are reassigned to different genera, and four species are designated as nomina dubia. The third chapter evaluates the similarities of camerate genera in three coeval North American formations with the Lake Valley Formation. These formations are the lower Burlington Limestone of the Mississippi Valley, the Redwall Limestone of Arizona, and the Anchor Limestone of Nevada. These similarities are based on presence-absence data with the Jaccard Coeff...