AQUARIA-BASED OBSERVATIONS OF THE OPHIUROID OPHIOLEPIS SUPERBA AND THE TRACKWAYS IT PRODUCES

IF 1.5 4区 地球科学 Q2 GEOLOGY Palaios Pub Date : 2023-02-28 DOI:10.2110/palo.2022.035
Riley C. Morton, Reed A. Myers, M. Gingras, J. Zonneveld
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引用次数: 2

Abstract

ABSTRACT: An array of trace fossils have been ascribed to brittle-star behaviors including locomotion traces such as Biformites. Brittle-star locomotion has been well described but little work has been done to link modern brittle-star behavior to the trace fossil record. To draw this connection, a brittle star was kept in an aquarium and isolated in a “walking” tank with a fine glass-bead substrate. The animal was left in the walking tank for 30 minutes then the substrate was examined for traces. A digital camera was used to record the animal's movements and to document the resulting traces. Photographs were processed with photogrammetry software to produce digital models in order to acquire high-resolution images. Walking traces were described in detail and two morphologies were identified, which correspond with the ‘rowing’ and ‘reverse-rowing’ modes of brittle-star locomotion. Interestingly, traces similar to Biformites were not formed although some Biformites characters are observed. Morphological similarities include elongated lobate depressions and bioglyphs. Trackway dissimilarities include a repeating, paired, symmetrical pattern observed in the lab contrasting with Biformites that is often expressed as a texture of dense and overlapping, or isolated imprints. Another dissimilarity is the expression of bioglyphs in the lab as striae compared to the positive protuberances observed in Biformites. This study illustrates the utility of using actualistic observations to: (1) refine interpretations of locomotory mechanisms, such as rowing and reverse rowing, for a better understanding of walking behavior, and (2) to expand recognition criteria for ophiuroid (and other taxa) tracks in the fossil record.
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基于水瓶座的对超级蛇蛇座的观测及其产生的轨迹
摘要:一系列的痕迹化石被认为具有脆性星行为,其中包括双形虫的运动痕迹。脆星运动已经得到了很好的描述,但很少有人把现代脆星行为与化石记录联系起来。为了建立这种联系,将一只海蛇尾放在水族馆中,并将其隔离在一个带有细玻璃珠基板的“行走”水箱中。将动物放在行走槽中30分钟,然后检查基质是否有痕迹。一台数码相机被用来记录动物的活动,并记录下由此产生的痕迹。通过摄影测量软件对照片进行处理,生成数字模型,以获得高分辨率图像。详细描述了行走痕迹,并确定了两种形态,它们对应于脆性星运动的“划船”和“反划船”模式。有趣的是,虽然观察到一些双formites的特征,但没有形成类似双formites的痕迹。形态上的相似性包括细长的叶状凹陷和生物符号。轨迹差异包括在实验室中观察到的重复的、成对的、对称的图案,与通常表现为密集和重叠的纹理或孤立的印记的双孔虫形成对比。另一个不同之处是在实验室中生物标志的表达为条纹,而在双形虫中观察到阳性突起。这项研究说明了使用实际观察的效用:(1)完善运动机制的解释,如划船和反向划船,以便更好地理解行走行为;(2)扩大对化石记录中蛇属(和其他分类群)足迹的识别标准。
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来源期刊
Palaios
Palaios 地学-地质学
CiteScore
2.80
自引率
12.50%
发文量
40
审稿时长
6 months
期刊介绍: PALAIOS is a monthly journal, founded in 1986, dedicated to emphasizing the impact of life on Earth''s history as recorded in the paleontological and sedimentological records. PALAIOS disseminates information to an international spectrum of geologists and biologists interested in a broad range of topics, including, but not limited to, biogeochemistry, ichnology, paleoclimatology, paleoecology, paleoceanography, sedimentology, stratigraphy, geomicrobiology, paleobiogeochemistry, and astrobiology. PALAIOS publishes original papers that emphasize using paleontology to answer important geological and biological questions that further our understanding of Earth history. Accordingly, manuscripts whose subject matter and conclusions have broader geologic implications are much more likely to be selected for publication. Given that the purpose of PALAIOS is to generate enthusiasm for paleontology among a broad spectrum of readers, the editors request the following: titles that generate immediate interest; abstracts that emphasize important conclusions; illustrations of professional caliber used in place of words; and lively, yet scholarly, text.
期刊最新文献
NEW QUANTITATIVE DESCRIPTORS (SHAPE AND MACROBORING) OF BIOGENIC NODULES: EXAMPLES FROM THE LESSER ANTILLES AND NEW ZEALAND LOCOMOTION TRACES EMPLACED BY MODERN STALKLESS COMATULID CRINOIDS (FEATHERSTARS) A FOSSIL FOREST FROM ITALY REVEALS THAT WETLAND CONIFERS THRIVED IN EARLY PERMIAN PERI-TETHYAN PANGEA TAPHONOMY OF TINY TETRAPOD TRACKS IN AN EXAMPLE FROM THE LOWER PERMIAN (CISURALIAN) SŁUPIEC FORMATION (SW POLAND) PLANT COMMUNITY CHANGE ACROSS THE PALEOCENE–EOCENE BOUNDARY IN THE GULF COASTAL PLAIN, CENTRAL TEXAS
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