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A Glimpse into the Natural History of Leiolepis rubritaeniata Mertens,1961(Squamata:Leiolepididae)

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Asian Herpetological Research 2023年第2期14卷 147-155页

作者： Gunther KÖHLER Panupong THAMMACHOTI senckenberg forschungsinstitut und naturmuseum Senckenberganlage 25Frankfurt a.M.60325Germany Department of Biology Faculty of ScienceChulalongkorn UniversityBangkok 10330Thailand

During the months of April through July 2020 we studied aspects of the natural history of Leiolepis rubritaeniata,a species of butterfly lizard that occurs on the Khorat Plateau in Thailand and adjacent regions of Laos and Cambodia as well as in south-central *** present data on population size and structure,as well as location,size,compass orientation,and structure of the lizard’s ***,we present climatic data(ambient air temperature and precipitation)at the study site for the duration of our field work as well as temperature data for the complete year ***,we provide data on egg laying,incubation conditions and characteristics of the ***,we present an easy to use and reliable non-invasive method for the long-term recognition of individual butterfly lizards based on their unique dorsal *** lizards are utilized as a food source for the local human *** far,there are no farming projects in Thailand involving this species and all individuals are collected from the wild *** data are available on the population dynamics of *** but it can be assumed that habitat destruction due to land use change as well as its utilization for human consumption have negative effects on the long-term survival of the local populations of this lizard *** baseline data presented here are essential for any meaningful conservation strategy for these lizards.

关键词： Burrow structure butterfly lizard ecology Khorat Plateau Southeast Asia Squamata

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Palaeobotanical and biomarker evidence for Early Permian(Artinskian) wildfire in the Rajmahal Basin, India

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Journal of Palaeogeography 2021年第1期10卷 55-75页

作者： Srikanta Murthy Vinod Atmaram Mendhe Dieter Uhl Runcie Paul Mathews Vivek Kumar Mishra Saurabh Gautam Birbal Sahni Institute of Palaeosciences 53University RoadLucknow 226007India CSIR-Central Institute of Mining and Fuel Research Dhanbad 826015JharkhandIndia senckenberg forschungsinstitut und naturmuseum Frankfurt Senckenberganlage 2560325 Frankfurt am MainGermany

This study provides a combined analysis on the palynology, fossil charcoal and biomarkers of the subsurface coal deposits from a borehole RMB #2 drilled at the Dhulia Coal Block, Rajmahal Basin, India, in attempts to establish the chronology of sedimentation and to propose palaeobotanical as well as geochemical evidence for the occurrence of wildfires in these sediments. The palynological investigation suggests a Scheuringipollenites barakarensis palynoassemblage from the lower Barakar Formation, dated as Artinskian(Early Permian) in age. This assemblage reveals the dominance of Glossopteridales and sub-dominance of taxa belonging to Cordaitales and *** charcoal in sediments is usually recognized as a direct indicator for the occurrence of palaeo-wildfires. More data involving the anatomical features of fossil charcoal analyzed by Field Emission Scanning Electronic Microscope broaden our knowledge on Early Permian wildfires from the peninsula of India. The studied macroscopic charcoal fragments exhibit anatomical details such as homogenized cell walls, uniseriate simple and biseriate alternate pitting on tracheid walls and rays of varying heights pointing to a gymnospermous wood affinitity. The excellent preservation of charcoal fragments, shown by their large sizes and almost unabraded edges, suggests a parautochthonous origin. The embedded biomarker study performed for charcoal sediments and its characterization demonstrate the presence of n-alkanes, isoprenoids, terpenoids and aromatic compounds. A bimodal distribution pattern of n-alkanes with a Cmaxat n-C25 is identified. Diterpenoids and pentacyclic terpenoids are identified, indicating the input of an early conifer vegetation and bacterial activity, respectively. The identified polyaromatic hydrocarbon(PAH) compounds, together with the charcoal fragments, clearly suggest that repeated wildfire events occurred during the deposition of these Artinskian sediments in the Rajmahal Basin.

关键词： Palaeo-wildfire Palynology Fossil charcoal Biomarker Barakar Formation Rajmahal Basin

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Middle Miocene vegetation and climate in the central and southern part of Yunnan,China

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地球环境学报 2011年第1期 329-330页

作者： ZHANG Qian-qian Ferguson D K Mosbrugger V WANG Yu-Fei LI Cheng-Sen State Key Laboratory of Systematic and Evolutionary Botany Institute of BotanyChinese Academy of Sciences Graduate University of Chinese Academy of Sciences Institute of Palaeontology University of Vienna forschungsinstitut und naturmuseum

In order to understand the Neogene vegetation succession and climatic changes in Southwest China,we reconstructed the Middle Miocene vegetation and climate at four localities,which are at different latitudes(24°19’25.3 "N / 23°35’10.2" N / 22°27’44.5 "N / 21°17’05.9" N) along the SW side of the Mao Mountains in Yunnan *** palynological assemblages obtained from the four localities suggest that the Middle Miocene vegetation there was composed of mixed evergreen and deciduous broad-leaved forests with some coniferous forests growing under subtropical *** on the palynological data,seven paleoclimatic parameters of the four localities are obtained by applying the method of Co-existence Approach and compared with the modern and the Late Miocene and Late Pliocene climatic parameters in *** comparison revealed that:1) Among the four palynological assemblages,the abundance of angiosperms increase while those of gymnosperms and pteridophytes decrease along the gradient of latitudes from north to south.2) The mean annual temperature(MAT) and mean coldest monthly temperature(MCMT) were obviously lower in Middle Miocene than today(MAT:13.2 to 14.6 comp.17.7 to 21 ℃;MCMT:2.9 comp.10.9 to 15.2℃).It suggests that the Ailao Mountains were not high enough to block the summer monsoon and the winter monsoon.3) In contrast to the Neogene global cooling,the regional values of the MAT and MCMT in Yunnan increased and accompanied by a decrease of the difference of temperature between the coldest and warmest months(18.4℃ to 19.1 ℃ comp.9.5℃ to 12.3℃) since Middle *** may be linked to a gradual reduction in the strength of the Asian winter monsoon as the Tibetan Plateau was uplifted.

关键词： Palynology Paleovegetation Paleoclimate Middle Miocene Yunnan SW China

Field workshop of IGCP 499

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Episodes 2007年第3期30卷 229-230页

作者： Peter Konigshof Silvio H. Peralta Namik Yalcin forschungsinstitut und naturmuseum senckenberg senckenberganlage 25 D-60325 Frankfurt am Main GERMANY Peter National University of San Juan 1. De la Roza Ave and Meglioli St. 5400 Rivadavia San Juan ARGENTINA Department of Geological Engineering Istanbul University TR-34850 Avcilar Istanbul TURKEY

A field workshop of the International Geoscience Programme （IGCP） Project 499 entitled ＇Devonian Land-Sea Interaction： Evolution of Ecosystems and Climate＇（DEVEC） was held between 14 and 22 May 2007 in San Juan, Argentina. The Devonian of the San Juan and Mendoza Precordillera and the San Rafeal Block are of special interest for the project due to the palaeogeographic and hiostratigraphic importance in the Devonian Malvinokaffric Realm, hut also in the tecto-sedimentary evolution of the Precordillem terrane.

关键词：国际地理项目会议研究工作会议国际组织

Diagnostics for a troubled backbone:testing topological hypotheses of trapelioid lichenized fungi in a large-scale phylogeny of Ostropomycetidae(Lecanoromycetes)

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Fungal Diversity 2015年第4期73卷 239-258页

作者： Philipp Resl Kevin Schneider Martin Westberg Christian Printzen Zdeněk Palice Göran Thor Alan Fryday Helmut Mayrhofer Toby Spribille Institute of Plant Sciences NAWI GrazUniversity of GrazHolteigasse 6A-8010 GrazAustria Department of Botany Swedish Museum of Natural HistoryP.O.Box 50007SE-10405 StockholmSweden senckenberg forschungsinstitut und naturmuseum Senckenberganlage 25D-60325 Frankfurt am MainGermany Institute of Botany Academy of Sciences of the Czech RepublicZámek 125243 PrůhoniceCzech Republic Department of Botany Faculty of SciencesCharles University in PragueBenátská212801 Praha 2Czech Republic Department of Ecology Swedish University of Agricultural SciencesP.O.Box 7044SE-75007 UppsalaSweden Herbarium Department of Plant BiologyMichigan State UniversityEast LansingMI 48824USA Division of Biological Sciences University of Montana32 Campus DriveMissoulaMT 59812USA

Trapelioid fungi constitute a widespread group of mostly crust-forming lichen mycobionts that are key to understanding the early evolutionary splits in the Ostropomycetidae,the second-most species-rich subclass of lichenized *** uncertain phylogenetic resolution of the approximately 170 species referred to this group contributes to a poorly resolved backbone for the entire *** on a data set including 657 newly generated sequences from four ribosomal and four protein-coding gene loci,we tested a series of a priori and new evolutionary hypotheses regarding the relationships of trapelioid clades within *** found strong support for a monophyletic group of nine core trapelioid genera but no statistical support to reject the long-standing hypothesis that trapelioid genera are sister to Baeomycetaceae or ***,we can reject a sister group relationship to Ostropales with high *** data also shed light on several longstanding questions,recovering Anamylopsoraceae nested within Baeomycetaceae,elucidating two major monophyletic groups within trapelioids(recognized here as Trapeliaceae and Xylographaceae),and rejecting the monophyly of the genus *** transfer eleven species of the latter genus to Lambiella and describe the genus Parainoa to accommodate a previously misunderstood species of *** phylogenetic studies in Ostropomycetidae have invoked Bdivergence order^for drawing taxonomic conclusions on higher level *** data show that if backbone support is lacking,contrasting solutions may be recovered with different or added *** accordingly urge caution in concluding evolutionary relationships from unresolved phylogenies.

关键词： Ascomycota Fungi Lambiella Lecanoromycetes Ostropomycetidae Parainoa Paraphyly SOWH test Taxon sampling

IGCP-499 Workshop ＂Depositional Environments of the Gondwanan and Laurasian Devonian＂

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Episodes 2006年第2期29卷 135-135页

作者： Peter Konigshof Eberhard Schindler Volker Wilde Jurga Lazauskiene M. Namik Yalcin forschungsinstitut und naturmuseum senckenberg Senckenberganlage 25 D-60325 Frankfurt am Main GERMANY Geological Survey of Lithuania Department of Lithostratigraphy and Tectonics Konaskio 35 LT-2009 Vilnius LITHUANIA Istanbul University Engineering Faculty Department of Geological Engineering TR-34850 Avcilar-Istanbul TURKEY

Turkey is a region of special interest for Devonian researchers because it comprises Laurasian and Gondwanan components situated on different but neighbouring tectonic blocks. The respective strata include a variety o... 详细信息

关键词：沉积物岩石劳亚古大陆地质特征