Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.palaeo.2020.109965 |
Uplands, lowlands, and climate: Taphonomic megabiases and the apparent rise of a xeromorphic, drought-tolerant flora during the Pennsylvanian-Permian transition | |
DiMichele, William A.; Bashforth, Arden R.; Falcon-Lang, Howard J.; Lucas, Spencer G. | |
通讯作者 | DiMichele, WA |
来源期刊 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
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ISSN | 0031-0182 |
EISSN | 1872-616X |
出版年 | 2020 |
卷号 | 559 |
英文摘要 | The Late Mississippian and Pennsylvanian have been referred to as the Coal Age due to enormous paleotropical peat accumulations (coal beds). Numerous fossil floras have been collected from these coals, and their associated seat-earth paleosols and roof-shales, over more than two centuries, leading to the inference of vast swampy wetlands covering the Pangean tropics during the Pennsylvanian. In contrast, the Permian tropics are characterized as more arid, with sparser and more heterogeneous vegetation than inferred for the Pennsylvanian. In the tropics, the Pennsylvanian to Permian transition has been described as a changeover from a pteridophytedominated Paleophytic flora, to a seed-plant dominated Mesophytic flora. This view notwithstanding, floras dominated by xeromorphic seed plants also are well known from the Pennsylvanian tropics. Some authors have characterized these plants as being occupants of uplands, subsequently transported into basinal-lowland, preservational environments. In this model, uplands are well drained, causing areas of drought under otherwise everwet climates. In this paper, we present an alternative interpretation: that the apparent transition in Pennsylvanian-Permian tropical vegetation reflects two types of taphonomic megabias. First is a preservational megabias, strongly favoring the vegetation of humid climates over that of seasonally dry climates. Accordingly, tropical-plant preservational potential fluctuated in concert with Late Paleozoic Ice Age glacial-interglacial oscillations, and contemporaneous sea-level and climatic changes. Second is an analytical megabias, strongly favoring the discovery and collection of the wetland biome from Pennsylvanian strata, overlooking the less frequently and more poorly preserved drought-tolerant biome. By Permian times, vast wetlands, and their fossil record, had largely disappeared from central Pangea (although continuing in Cathaysia), making drought-tolerant vegetation more visible to searchers, without changing its preservational circumstances. We demonstrate that the upland model is untenable, being inconsistent with the principles of plant biogeography and with geological aspects of the fossil record. |
英文关键词 | Wetland Dryland Paleophytic Mesophytic Late Paleozoic |
类型 | Article |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:000591242700009 |
WOS关键词 | CENTRAL APPALACHIAN BASIN ; TROPICAL RAIN-FOREST ; UPPER SILESIAN BASIN ; DESMOINESIAN-MISSOURIAN BOUNDARY ; PHYLOGENETIC NICHE CONSERVATISM ; WESTERN EQUATORIAL PANGEA ; INTRA-SUDETIC BASIN ; PALEOZOIC ICE-AGE ; LOWER CUTLER BEDS ; CONEMAUGH GROUP |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology |
WOS研究方向 | Physical Geography ; Geology ; Paleontology |
来源机构 | University of London |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/327579 |
作者单位 | [DiMichele, William A.] Smithsonian Inst, Dept Paleobiol, Natl Museum Nat Hist, Washington, DC 20560 USA; [Bashforth, Arden R.] Univ Copenhagen, Nat Hist Museum Denmark, Oster Voldgade 57, DK-1350 Copenhagen K, Denmark; [Falcon-Lang, Howard J.] Royal Holloway Univ London, Dept Earth Sci, Egham TW20 0EX, Surrey, England; [Lucas, Spencer G.] New Mexico Museum Nat Hist & Sci, Albuquerque, NM 87104 USA |
推荐引用方式 GB/T 7714 | DiMichele, William A.,Bashforth, Arden R.,Falcon-Lang, Howard J.,et al. Uplands, lowlands, and climate: Taphonomic megabiases and the apparent rise of a xeromorphic, drought-tolerant flora during the Pennsylvanian-Permian transition[J]. University of London,2020,559. |
APA | DiMichele, William A.,Bashforth, Arden R.,Falcon-Lang, Howard J.,&Lucas, Spencer G..(2020).Uplands, lowlands, and climate: Taphonomic megabiases and the apparent rise of a xeromorphic, drought-tolerant flora during the Pennsylvanian-Permian transition.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,559. |
MLA | DiMichele, William A.,et al."Uplands, lowlands, and climate: Taphonomic megabiases and the apparent rise of a xeromorphic, drought-tolerant flora during the Pennsylvanian-Permian transition".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 559(2020). |
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