Results 31 to 40 of about 1,765 (143)

The stable isotope setting of Australopithecus sediba at Malapa, South Africa

open access: yesSouth African Journal of Science, 2016
We report δ13C and δ18O results from carbonate-cemented cave sediments at Malapa in South Africa. The sediments were deposited during a short-period magnetic reversal at 1.977±0.003 Ma, immediately preceding deposition of Facies D sediments that contain ...
Emily Holt   +3 more
doaj   +1 more source

Marjamurto, an interstadial site in a till covered esker area of central Ostrobothnia, western Finland [PDF]

open access: yesBulletin of the Geological Society of Finland, 1989
Till-covered glaciofluvial deposits, presumably eskers, are common in Central Ostrobothnia (Pohjanmaa) within a zone more than 50 km broad, in which no exposed eskers are present.
H. Peltoniemi   +3 more
doaj   +1 more source

Modern Pollen Assemblages From Lake Sediments and Soil in East Siberia and Relative Pollen Productivity Estimates for Major Taxa

open access: yesFrontiers in Ecology and Evolution, 2022
Modern pollen–vegetation–climate relationships underpin palaeovegetation and palaeoclimate reconstructions from fossil pollen records. East Siberia is an ideal area for investigating the relationships between modern pollen assemblages and near natural ...
Rongwei Geng   +16 more
doaj   +1 more source

Late Holocene palynology and palaeovegetation of tephra-bearing mires at Papamoa and Waihi Beach, western Bay of Plenty, North Island, New Zealand. [PDF]

open access: yes, 1995
The vegetation history of two mires associated with Holocene dunes near the western Bay of Plenty coast, North Island, New Zealand, is deduced from pollen analysis of two cores.
Campbell E. O.   +20 more
core   +2 more sources

Western Siberia, a review of Holocene climatic changes [PDF]

open access: yesЖурнал Сибирского федерального университета: Серия Биология, 2009
This article generalizes published palaeoecological and palaeoclimatic data based on pollen and other proxy data for Holocene of Western Siberia and describes the most significant palaeoreconstructions and hypothesis in explanation of past climatic ...
Tatiana A. Blyakharchuk
doaj  

Late Miocene wood flora associated with the Yuanmou hominoid fauna from Yunnan, southwestern China and its palaeoenvironmental implication

open access: yesJournal of Palaeogeography, 2014
The Upper Miocene Xiaohe Formation of the Yuanmou Basin in Yunnan Province, southwestern China, is famous for its hominoid fauna and is important for studying the Late Cenozoic human and mammal evolution.
Ye-Ming Cheng, Yu-Fei Wang, Cheng-Sen Li
doaj   +1 more source

The last glacial-interglacial cycle in Lake Ohrid (Macedonia/Albania): testing diatom response to climate [PDF]

open access: yes, 2010
Lake Ohrid is a site of global importance for palaeoclimate research. This study presents results of diatom analysis of a ca. 136 ka sequence, Co1202, from the northeast of the lake basin.
Cvetkoska, A.   +4 more
core   +5 more sources

Reconstruction of palaeovegetation and sedimentation conditions in the area of ancient Lake Burtnieks, northern Latvia [PDF]

open access: yesEstonian Journal of Earth Sciences, 2010
Palaeobotanical investigations were carried out with the aim of reconstructing the development of palaeovegetation and formation of sediments in the northeastern area of ancient Lake Burtnieks.
Kalniņa, Laimdota   +2 more
doaj  

Miocene palynoflora from the KRAM-P 218 leaf assemblage from the Bełchatów Lignite Mine (Central Poland)

open access: yesActa Palaeobotanica, 2016
During a palynological analysis of four samples from the Bełchatów KRAM-P 218 collection of plant macroremains 95 fossil species of sporomorphs were identified. Among the non-pollen palynomorphs was the fossil species Desmidiaceaesporites cosmarioformis,
Worobiec Elżbieta, Worobiec Grzegorz
doaj   +1 more source

Fossil pollen records reveal a late rise of open-habitat ecosystems in Patagonia [PDF]

open access: yes, 2012
The timing of major turnovers in terrestrial ecosystems of the Cenozoic Era has been largely interpreted from the analysis of the assumed feeding preference of extinct mammals. For example, the expansion of open-habitat ecosystems (grasslands or savannas)
Barreda, Viviana Dora, Palazzesi, Luis
core   +2 more sources

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