{"title":"Ichnology of the Lower Cretaceous (Albian) Mesilla Valley Formation, Cerro de Cristo Rey, southeastern New Mexico, USA","authors":"Eric J. Kappus, S. Lucas","doi":"10.58799/nmg-v42n1.3","DOIUrl":null,"url":null,"abstract":"Invertebrate trace fossils from the Albian Mesilla Valley Formation (Washita Group) at Cerro de Cristo Rey, Sunland Park, NM represent the following ichnotaxa: Ancorichnus isp., Arenicolites isp., Bergueria isp., Bichordites sp., Cardioichnus foradadensis, C. biloba, Chondrites intricatus, Cochlichnus anguineus, Coprulus oblongus, Gordia marina, Helicodromites isp., Lockeia isp., Ophiomorpha nodosa, Palaeophycus tubularis, P. striatus, P. heberti, Planolites isp., Protovirgularia dichotoma, Rhizocorallium commune var. irregulare (with Coprulus oblongus), Skolithos isp., Spongeliomorpha isp., S. sublumbricoides, S. oraviense, Taenidium isp., Thalassinoides isp., T. paradoxicus, Treptichnus isp., a chimney structure (Chomatichnus?), and the biofilm Rugalichnus (“Kinneyia”). This is the first study of the invertebrate ichnology of any of the shallow marine units at Cerro de Cristo Rey. The Mesilla Valley Formation contains a medium/high diversity ichnoassemblage, including fugichnia (i.e., Skolithos), fodichnia (i.e., Chondrites), domichnia (i.e., Ophiomorpha, Thalassinoides), repichnia (Protovirgularia), paschichnia (i.e., Palaeophycus), and cubichnia (i.e., Bergaueria, Cardioichnus, Lockeia), as well as compound traces and composite traces. This ichnoassemblage was preserved in tempestites (storm deposits) from below wave base on the upper/middle continental shelf during Oceanic Anoxic Event 1d and contains ichnotaxa representative of the proximal Cruziana ichnofacies (with Skolithos influence).","PeriodicalId":35824,"journal":{"name":"New Mexico Geology","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"New Mexico Geology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.58799/nmg-v42n1.3","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
引用次数: 1
Abstract
Invertebrate trace fossils from the Albian Mesilla Valley Formation (Washita Group) at Cerro de Cristo Rey, Sunland Park, NM represent the following ichnotaxa: Ancorichnus isp., Arenicolites isp., Bergueria isp., Bichordites sp., Cardioichnus foradadensis, C. biloba, Chondrites intricatus, Cochlichnus anguineus, Coprulus oblongus, Gordia marina, Helicodromites isp., Lockeia isp., Ophiomorpha nodosa, Palaeophycus tubularis, P. striatus, P. heberti, Planolites isp., Protovirgularia dichotoma, Rhizocorallium commune var. irregulare (with Coprulus oblongus), Skolithos isp., Spongeliomorpha isp., S. sublumbricoides, S. oraviense, Taenidium isp., Thalassinoides isp., T. paradoxicus, Treptichnus isp., a chimney structure (Chomatichnus?), and the biofilm Rugalichnus (“Kinneyia”). This is the first study of the invertebrate ichnology of any of the shallow marine units at Cerro de Cristo Rey. The Mesilla Valley Formation contains a medium/high diversity ichnoassemblage, including fugichnia (i.e., Skolithos), fodichnia (i.e., Chondrites), domichnia (i.e., Ophiomorpha, Thalassinoides), repichnia (Protovirgularia), paschichnia (i.e., Palaeophycus), and cubichnia (i.e., Bergaueria, Cardioichnus, Lockeia), as well as compound traces and composite traces. This ichnoassemblage was preserved in tempestites (storm deposits) from below wave base on the upper/middle continental shelf during Oceanic Anoxic Event 1d and contains ichnotaxa representative of the proximal Cruziana ichnofacies (with Skolithos influence).
期刊介绍:
New Mexico Geology is a quarterly, peer-reviewed journal available by subscription. Articles of original research are generally less than 10,000 words in length and pertain to the geology of New Mexico and neighboring states, primarily for an audience of professional geologists or those with an interest in the geologic story behind the landscape. The journal also publishes abstracts from regional meetings, theses, and dissertations (NM schools), descriptions of new publications, book reviews, and upcoming meetings. Research papers, short articles, and abstracts from selected back issues of New Mexico Geology are now available as free downloads in PDF format. Back issues are also available in hard copy for a nominal fee.