Results 121 to 130 of about 232 (164)
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The Palaeovegetation of the Murray Basin, Late Eocene to Mid-Miocene

Australian Systematic Botany, 1993
The principles of pollen dispersal and deposition show that the pollen spectrum is produced by the plants of the locality, with a little transported in from long distances. The 'locality' has a radius of no more than 500 m, and it could be much less. Adherence to these principles has allowed a detailed reconstruction of the palaeovegetation.
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Palaeovegetation of China: a pollen data‐based synthesis for the mid‐Holocene and last glacial maximum

Journal of Biogeography, 2000
AbstractPollen data from China for 6000 and 18,000 14C yr bp were compiled and used to reconstruct palaeovegetation patterns, using complete taxon lists where possible and a biomization procedure that entailed the assignment of 645 pollen taxa to plant functional types.
Yu, G   +30 more
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Palaeovegetation and palaeoclimate evolution during the Late Miocene to Early Pliocene of SE Romania

Geological Journal, 2020
Fossil microfloral assemblages from five sedimentary successions of the Dacian Basin (Eastern Paratethys) are used to reconstruct the palaeovegetation and palaeoclimate of SE Romania during the Late Miocene to Early Pliocene (regional stages Khersonian, Meotian, Pontian, and Dacian).
Manuel Casas‐Gallego   +2 more
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Geochemical appraisal of palaeovegetation and climate oscillation in the Late Miocene of Western Bulgaria

Organic Geochemistry, 2011
Abstract Palaeobotanical methods and geochemical techniques were used to assess plant contribution and palaeoenvironment for the Staniantsi Basin, Bulgaria. The aim was to connect palaeovegetation change and climate oscillation based on pollen and statistical analysis with organic geochemical proxies for a Late Miocene lacustrine to paludial ...
Maya Stefanova   +2 more
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Early Oligocene plant taphocoenoses of the Haselbach megafloral complex and the reconstruction of palaeovegetation

Palaeobiodiversity and Palaeoenvironments, 2012
In this article, vegetational reconstructions of leaf floras from the early Oligocene Haselbach megafloral complex, which have been published by several authors since the 1960s, are compiled, summarised, reconsidered and partly revised. The geological setting of the fossil material is updated based on the most recent monographs on stratigraphy and ...
Lutz Kunzmann, Harald Walther
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Palaeovegetational and palaeoenvironmental trends in the summit of the Guaiquinima massif (Venezuelan Guayana) during the Holocene

Journal of Quaternary Science, 2005
AbstractThe summits of the table mountains (tepuis) from the Neotropical Guayana region are remote environments suitable for palaeoecological studies with evolutionary, biogeographical and palaeoclimatic implications. Here, using palynological analyses of two radiocarbon‐dated peat bogs from a tepui summit, the Holocene palaeovegetational trends are ...
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A HIGH-RESOLUTION RECORD OF THE LAST DEGLACIATION IN THE CENTRAL MEDITERRANEAN SEA: PALAEOVEGETATION AND PALAEOHYDROLOGICAL EVOLUTION

Quaternary Science Reviews, 1998
Abstract A high-resolution palynological and stratigraphical record of a marine deep-sea core in the Adriatic sea documents marine and continental palaeoenvironmental changes in the basin during the last deglaciation and early Holocene. A chronology is derived from the oxygen isotope stratigraphy.
Combourieu-Nebout, Nathalie   +3 more
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An environmental scenario for the earliest hominins in the Iberian Peninsula: Early Pleistocene palaeovegetation and palaeoclimate

Review of Palaeobotany and Palynology, 2019
Abstract The Early Pleistocene deposits of the Iberian Peninsula provided some of the oldest hominin fossil sites of Western Europe. Evidence also shows that early Homo thrived in the Mediterranean peninsulas during the Early Pleistocene ‘interglacial’ phases.
Yul Altolaguirre   +5 more
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Palaeovegetation and palaeoclimate during middle Late Palaeolithic age of Lingnan area, China

Journal of Palaeosciences, 2008
The fossil spore-pollen recovered from middle Late Palaeolithic age (i.e. late Middle Pleistocene to Late Pleistocene) of Lingnan area of China are mainly distributed in the Pearl River Mouth Basin, Pearl River Delta, Shenzhen, Zhanjiang, Leizhou Peninsula and Hainan Island.
Jin Jianhua, Liao Wenbo
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