EXAMINING THE ONTOGENY OF THE PENNSYLVANIAN CLADID CRINOID ERISOCRINUS

Noel J. Hernandez Gomez, Lisette E. Melendez, Whitney A. Lapic, Sarah L. Sheffield, Ronald D. Lewis
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Abstract

Crinoids, the group known today as the sea lilies, were a major constituent of ocean environments from the late Carboniferous (323–299 million years ago). However, crinoid fossil-forming potential is poor, and they typically fell apart quickly after death. This limits our ability to study much about their life histories, including how they would have grown. Through the discovery of an area of exceptional fossil preservation in the Barnsdall Formation of Oklahoma, we have a rare chance to learn about the growth of one of these species of crinoids, Erisocrinus typus. Here we perform a growth analysis of a well-preserved series of fossils and discuss the patterns that it showed from its juvenile stage to adulthood.
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宾夕法尼亚有齿海百合的个体发育研究
海百合,今天被称为海百合,是石炭纪晚期(3.23 - 2.99亿年前)海洋环境的主要组成部分。然而,海百合形成化石的可能性很低,它们通常在人死后很快就会分解。这限制了我们研究它们的生活史的能力,包括它们是如何成长的。通过在俄克拉何马州巴恩斯德尔地层中发现一个特殊的化石保存区域,我们有了一个难得的机会来了解其中一种海蛇类的生长情况,即Erisocrinus typus。在这里,我们对一系列保存完好的化石进行了生长分析,并讨论了它从幼年到成年的生长模式。
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CONSTRAINING REDUCING CONDITIONS IN THE PRAGUE BASIN DURING THE LATE SILURIAN LAU/KOZLOWSKII EXTINCTION EVENT PALEOGEOGRAPHY AND HIGH-PRECISION GEOCHRONOLOGY OF THE NEOARCHEAN FORTESCUE GROUP, PILBARA, WESTERN AUSTRALIA THERE AND BACK AGAIN: RECYCLING OF THE APPALACHIAN SIGNATURE IN DZ U-PB RECORDS OF PHANEROZOIC NORTH AMERICA EXAMINING THE ONTOGENY OF THE PENNSYLVANIAN CLADID CRINOID ERISOCRINUS “REEF SURVIVOR” – A NEW BOARD GAME DESIGNED TO TEACH COLLEGE AND UNIVERSITY UNDERGRADUATE STUDENTS ABOUT REEF ECOLOGY, EVOLUTION, AND EXTINCTION
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