Search results for "pollen analysis"

showing 4 items of 4 documents

Vegetation and climate in the eastern Iberian Peninsula during the pre-evaporitic Messinian (late Miocene). Palynological data from the Upper Turolia…

2015

International audience; The present paper reports a complete palynological study of the Upper Turolian sediments outcropping at the Venta del Moro site (eastern Iberian Peninsula). The pollen assemblages observed mainly reflect the local and regional vegetation, which must have formed part of a wetland ecosystem within a general setting of open steppe, as indicated by the great abundance and diversity of herbaceous pollen. This reflects the persistence of open vegetation in the Iberian Peninsula after the Middle Miocene when it became extensive. We here report the most recent record of Disanthus for the Iberian Peninsula. This shrub played an important role in an unusual, edaphically-mediat…

Late MiocenePollen analysisPalynologygeographygeography.geographical_feature_categorySteppePaleontologyOpen vegetationWetlandVegetationLate MiocenePalaeoclimateMediterranean BasinEastern Iberian PeninsulaPaleontology[SDU]Sciences of the Universe [physics]PeninsulaEarth ScienceEcology Evolution Behavior and SystematicsGeologyRiparian zoneReview of Palaeobotany and Palynology
researchProduct

Mid- and late-Holocene vegetation and fire history at Biviere di Gela, a coastal lake in southern Sicily, Italy

2009

The vegetation and fire history of few coastal sites has been investigated in the Mediterranean region so far. We present the first paleoecological reconstruction from coastal Sicily, the largest island in the Mediterranean Sea. We analysed pollen and charcoal in the sediments of Biviere di Gela, a lake (lagoon) on the south coast of Sicily. Our data suggest that the area became afforested after a marine transgression at ca. 7200 cal b.p. (5250 b.c.). Build-up of forest and shrublands took ca. 200–300 years, mainly with the deciduous trees Quercus, Ostrya and Fraxinus. Juniperus expanded ca. 6900 cal b.p. (4950 b.c.), but declined again 6600 cal b.p. (4650 b.c.). Afterwards, evergreen trees…

Mediterranean climateCharcoal analysis Pollen analysis Evergreen forest Human impact Mediterranean Quercus ilexOlea europaeaArcheologygeographygeography.geographical_feature_categorySettore AGR/05 - Assestamento Forestale E SelvicolturabiologyEcologyPaleontologyPlant ScienceVegetation580 Plants (Botany)OstryaEvergreenbiology.organism_classificationEvergreen forestShrublandDeciduousAnthracologyVegetation History and Archaeobotany
researchProduct

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

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. Pollen and plant macroremain studies provide information on vegetation development in the surroundings of the lake, including Stone Age settlements of Braukšas I and Braukšas II. Results of the investigations indicate that the development of vegetation together with sedimentation conditions in the palaeolake have changed since the Younger Dryas until today. Vegetation composition varies in different parts of the ancient Lake Burtnieks area due to past changes in lake water level which reached differe…

PeatAncient lakeplant macroremainslcsh:QE1-996.5VegetationSiltpalaeovegetationlcsh:GeologyPaleontologyPreborealpollen analysisBorealnorthern LatviaGeneral Earth and Planetary SciencesPhysical geographyYounger DryasPalaeolake BurtnieksGeologyWater Science and TechnologyGyttjaEstonian Journal of Earth Sciences
researchProduct

A high-quality annually laminated sequence from Lake Belau, Northern Germany: Revised chronology and ist implications for palynological and tephrochr…

2012

International audience; The annually laminated record of Lake Belau offers an exceptional opportunity to investigate with high temporal resolution Holocene environmental change, aspects of climate history and human impact on the landscape. A new chronology based on varve counts, 14C-datings and heavy metal history has been established, covering the last 9400 years. Based on multiple varve counting on two core sequences, the easily countable laminated section spans about 7850 varve years (modelled age range c. 9430 to 1630 cal. BP). Not all of the record is of the same quality but approximately 69% of the varves sequence is classified to be of high quality and only c. 5% of low quality. The …

[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and Prehistorypollen analysis[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory[SHS.ENVIR] Humanities and Social Sciences/Environmental studiesGermany[SHS.ENVIR]Humanities and Social Sciences/Environmental studieslake sediments[SHS] Humanities and Social Scienceschronology[SHS]Humanities and Social Sciences
researchProduct