DOI: 10.1016/j.palaeo.2015.05.023
论文题名: Estimation of late Eocene (Bartonian-Priabonian) terrestrial palaeoclimate: Contributions from megafloral assemblages from central Germany
作者: Moraweck K. ; Uhl D. ; Kunzmann L.
刊名: Palaeogeography, Palaeoclimatology, Palaeoecology
ISSN: 0031-0182
出版年: 2015
卷: 433 起始页码: 247
结束页码: 258
语种: 英语
英文关键词: CLAMP
; Coexistence Approach
; Eocene climate
; Fossil leaves
; Leaf margin analysis
; Weißelster Basin
英文摘要: The Eocene, the world's last global greenhouse period, shows distinct climatic developments through time, from subtropical towards warm-temperate conditions in Europe. The present paper investigates the response of five floras of the central German Weißelster Basin from different stratigraphic ages to terrestrial palaeoclimatic variations. The floras were selected from the Zeitz Floral Assemblage ("Florenkomplex") and cover a time interval of ca. 3.5 Myr within the late Eocene, which is supposed to be a period of gradual decline of global mean annual temperatures. The Zeitz Floral Assemblage was characterized by mainly evergreen, notophyllous intrazonal vegetation, consisting of subtropical and warm-temperate elements. The five floras as well as the entire Zeitz Floral Assemblage have been analysed using the following quantitative techniques: leaf margin analysis (LMA), Climate Leaf Analysis Multivariate Program (CLAMP) and Coexistence Approach (CA). Furthermore, the results have been compared with previously published estimates for additional localities from the same area and age. The temperature estimates derived for the Zeitz Floral Assemblage are in a good agreement with those of previous studies i.e. mean annual temperature (MAT) 16.1-20.0 °C, warmest month mean temperature (WMMT) 24.9-26.4 °C, coldest month mean temperature (CMMT) 9.2-13.3 °C. Deviations have been determined for the calculated mean annual precipitation (MAP 1308-1335 mm) compared to previously published data, indicating values of about 2000 mm. Both CLAMP and CA reveal clear hints for seasonality in precipitation which is in agreement with previous phytosociological assumptions and palynological data. The estimates for the individual sites differ between the different techniques as well as among the individual sites, but generally indicate no temporal trends in temperature and precipitation development. Additionally, the applicability of these techniques for fluvial-estuarine plant assemblages, as well as the applicability of intrazonal vegetation for reconstructing transregional climate conditions are discussed. Taphonomic and methodical biases are also subject of debate. © 2015 Elsevier B.V. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/68886
Appears in Collections: 过去全球变化的重建
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作者单位: Senckenberg Natural History Collections Dresden, Königsbrücker Landstraße 159, Dresden, Germany; Senckenberg Research Institute, Natural History Museum Frankfurt/Main, Senckenberganlage 25, Frankfurt/Main, Germany; Senckenberg Centre for Human Evolution and Palaeoenvironments, Department of Geosciences, Tübingen University, Sigwartstraße 10, Tübingen, Germany
Recommended Citation:
Moraweck K.,Uhl D.,Kunzmann L.. Estimation of late Eocene (Bartonian-Priabonian) terrestrial palaeoclimate: Contributions from megafloral assemblages from central Germany[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2015-01-01,433