首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Paucispecific macroinvertebrate communities in the Upper Cretaceous of El Hassana Dome (Abu Roash,Egypt): Environmental controls vs adaptive strategies
Institution:1. Paleontological Research Institution, 1259 Trumansburg Road, Ithaca, NY 14850, USA;2. Department of Earth & Atmospheric Sciences, Cornell University, Ithaca, NY 14853, USA;3. Natural History Museum of Los Angeles County, Los Angeles, CA 90007, USA;4. Center for Tropical Paleontology and Archaeology, Smithsonian Tropical Research Institute, Balboa Ancon, Panama, Panama;5. Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA 19104, USA;1. Department of Earth Sciences, Carleton University, Ottawa, Ontario K1S 5B6, Canada;2. Department of Geology, Portland State University, Portland, OR 97207-0751, USA;3. Institute of Geosciences, Goethe-University Frankfurt, D-60438 Frankfurt am Main, Germany;4. Geological Survey of Canada, 3303-33 St. NW, Calgary, Alberta T2L 2A7, Canada;5. Geological Survey of Canada, 1500-605 Robson Street, Vancouver, British Columbia V6B 5J3, Canada;6. Biodiversity and Climate Research Centre (BIK-F) D-60325 Frankfurt am Main, Germany
Abstract:Based on rock and fossil data from the Upper Cretaceous of the El Hassana Dome (Abu Roash, Egypt), factors controlling facies architecture and the nature of biotopes are highlighted. The succession formed on a non-rimmed shelf, the architecture of which varied from an inner to an outer shelf setting upsection. Macrobenthic biotopes are reconstructed and their palaeoecological significance assessed using a novel ternary plot. Based on diversity and community structure (770 specimens assigned to 28 bivalve and gastropod taxa), four paucispecific associations are identified. These are: 1. the ‘Cucullaea’ Assemblage, a low-energy, soft-substrate, oligotrophic outer shelf environment with reduced terrigenous input dominated by infaunal bivalves and hexactinellid sponges; 2. the ‘Plicatula’ Assemblage, a low-energy, restricted inner shelf lagoonal setting with soupy substrates and dysoxia below the sediment-water interface dominated by plicatulid and ostreid bivalves, 3. the ‘Durania’ Assemblage, a high-energy, high-temperature, shoal environment dominated by elevator rudists with minor numbers of echinoids, corals and bryozoans, which together form several biostromes. and 4. The ‘Trochactaeon’ Assemblage, which share the same characteristics of the ‘Durania’ Assemblage. The paucispecific nature of these biotopes is indicative of different stress factors. Consequently, the predominant taxa exhibit different degrees of adaptive strategies. In addition to global sea level, local tectonics have significantly affected facies distribution and biotope structure. The shallower facies during the early Turonian and the dysoxia spanning the Coniacian–Santonian were linked to synsedimentary tectonics, which formed many barriers and led to circulation restrictions.
Keywords:Environmental control  Facies associations  Biotope reconstruction  Late Mesozoic  North Africa
本文献已被 ScienceDirect 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号