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DOI | 10.1016/j.palaeo.2018.08.008 |
Big bedding planes: Outcrop size and spatial heterogeneity influence trace fossil analyses | |
Marenco K.N.; Hagadorn J.W. | |
发表日期 | 2019 |
ISSN | 0031-0182 |
起始页码 | 14 |
结束页码 | 24 |
卷号 | 513 |
英文摘要 | Roadcuts, core, cliffs and even mountainside exposures often limit the lateral extent to which we can assess bioturbation on bedding planes, simply because exposures of such surfaces are generally rare or small. Such constraints may hamper paleoenvironmental and paleoecological interpretations drawn from facies where most bioturbation is bed-parallel or patchily distributed. To explore how acute such constraints are, we conducted a pilot study of bioturbation in three exceptionally large (>5 m2), well-exposed, paleoenvironmentally similar bedding planes from the Cambrian of Wisconsin. The goal was to test the hypothesis that trace fossils and biogenic sediment disruption can be distributed heterogeneously at the scale of meters to decameters. Mapping the size variation and distribution of trace fossils across these bedding planes reveals variable patchiness. Individual bioturbated patches tend to be large (m-scale), but the density of biogenic sediment disruption within these patches is quite heterogeneous. In addition, bioturbated areas are separated by zones of undisturbed sediment that vary in size from <0.5 m2 to >3 m2. These observations suggest that ancient bedding planes, like modern substrate surfaces, can exhibit considerable lateral bioturbation heterogeneity at a range of spatial scales. Caution is thus urged when extrapolating the distribution and diversity of trace fossils and other biogenic sedimentary structures across broad sedimentary horizons based on small (≤1 m2) bedding plane exposures. © 2018 Elsevier B.V. |
英文关键词 | Bioturbation; Cambrian; Ichnofabric; Patchiness; Sandstone; Wisconsin |
语种 | 英语 |
scopus关键词 | bedding plane; biogenic deposit; bioturbation; Cambrian; facies; heterogeneity; ichnofabric; outcrop; paleoecology; paleoenvironment; patchiness; sandstone; sedimentary structure; trace fossil; Wisconsinan |
来源期刊 | Palaeogeography, Palaeoclimatology, Palaeoecology |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/151202 |
作者单位 | Department of Geology, Bryn Mawr College, 101 North Merion Avenue, Bryn Mawr, PA 19010, United States; Department of Earth Sciences, Denver Museum of Nature & Science, 2001 Colorado Boulevard, Denver, CO 80205, United States |
推荐引用方式 GB/T 7714 | Marenco K.N.,Hagadorn J.W.. Big bedding planes: Outcrop size and spatial heterogeneity influence trace fossil analyses[J],2019,513. |
APA | Marenco K.N.,&Hagadorn J.W..(2019).Big bedding planes: Outcrop size and spatial heterogeneity influence trace fossil analyses.Palaeogeography, Palaeoclimatology, Palaeoecology,513. |
MLA | Marenco K.N.,et al."Big bedding planes: Outcrop size and spatial heterogeneity influence trace fossil analyses".Palaeogeography, Palaeoclimatology, Palaeoecology 513(2019). |
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