scholarly journals RECONSTRUCTION OF REGIONAL DYNAMICS OF FOREST COVER ON DRY LANDS OF THE CENTRAL SYM-DUBCHES INTERFLUVE IN THE MIDDLE AND LATE HOLOCENE

2015 ◽  
Vol 84 (1) ◽  
pp. 12-20 ◽  
Author(s):  
Juan M. Rubiales ◽  
Mar Génova

Macro- and megafossil studies are of great value in palaeoecology because such evidence is spatially precise, directly radiocarbon dated, and usually taxon-specific. Here, we present new macro- and megafossil data from ten sites from the Gredos Mountains, central Iberian Peninsula, that suggest persistent forest cover through the late Holocene, with a widespread belt of pinewoods in the highlands of the Central Iberian Mountains. Well-preserved pine cones found at several sites revealed that bothPinus sylvestrisandPinus nigrawere present in the area during the middle and late Holocene at locations of important biogeographical interest. TheP. sylvestrisforests represent one of the southernmost locations of its entire range.P. nigrawas not known to have occurred in central Spain during the Holocene; it was found at the westernmost edge of its range in siliceous soils, a rare environment compared with the rest of its distribution. Finally, we explored the potential for obtaining a long pine chronology from central Iberia using tree-ring measurements and radiocarbon dating of pine subfossil logs.


The Holocene ◽  
2018 ◽  
Vol 29 (2) ◽  
pp. 244-261 ◽  
Author(s):  
Pablo G Messineo ◽  
Marcela S Tonello ◽  
Silvina Stutz ◽  
Alfonsina Tripaldi ◽  
Nahuel Scheifler ◽  
...  

The main objective of this work is to generate and integrate interpretations of human occupation strategies and inferences of the environmental-climatic conditions in the central Pampas during the middle and late Holocene. We present a novel archeological–geological–paleoecological analysis in the area of the Cabeza de Buey lake, placed in an aeolian landscape. During the middle Holocene, two events of human occupations were recognized at Laguna Cabeza de Buey 2 archeological site. Both events present a small amount of lithic materials, a low diversity of tools and activities developed with them (principally hard material), and the hunting and primary processing of artiodactyls. These evidences suggest a locus of specific activity associated with an ephemeral human settlement under climate conditions drier than present and the presence of small, brackish, and shallow water bodies. For the late late Holocene, the hunter-gatherer occupation has a higher depositional rate of lithic assemblage, stones with diverse origins, presence of pottery fragments, a great lithic tool diversity, knapping techniques, and activities developed with these tools (processing wood, bone, hide, non-woody plant, and soft material). These evidences reveal an occupation with a higher degree of recurrence represented by a locus of multiple activities associated with a more stable landscape, such as an environment of dunes fixed by grass vegetation, and the establishment of a permanent water body. The different environmental characteristics for the middle and late Holocene in this area promoted that human groups develop two different patterns of mobility, settlement and use of space.


Boreas ◽  
2019 ◽  
Vol 49 (1) ◽  
pp. 1-16 ◽  
Author(s):  
Jonathan Warnock ◽  
Elinor Andrén ◽  
Steve Juggins ◽  
Jonathan Lewis ◽  
David B. Ryves ◽  
...  

The Holocene ◽  
2020 ◽  
Vol 31 (1) ◽  
pp. 38-49
Author(s):  
Hui Shen ◽  
Xiaoqiang Li ◽  
Robert Spengler ◽  
Xinying Zhou ◽  
Keliang Zhao

The question of what the ecology communities of the Loess Plateau looked like before the extensive anthropogenic reshaping processes of the late-Holocene has stirred a long debate. A better understanding of these human-induced changes will not only help us understand the extent of paleoeconomic practices, but also inform future conservation actions on this ecologically fragile landscape. This paper presents a systematic study of wood charcoal from a series of archaeological sites, demonstrating that woody plants and woodlands were widely distributed and geographically diverse on the Loess Plateau in response to the East Asian Monsoon. In the Guanzhong Basin, oak ( Quercus spp.) woodlands were associated with a few tropical-subtropical taxa, which changed to oak and pine ( Pinus spp.) mixed forests on the eastern plateau, while on the northern plateau coniferous woodlands were dominant. On the western Loess Plateau, oak and elm ( Ulmus spp.) woodland and spruce ( Picea spp.) forests were widespread. The charcoal results suggest that human impacts on the dominant species might have begun as early as ca. 3500 cal yr BP, with oak replaced by Prunus as the dominant taxon, including many economically significant species, such as peaches ( P. persica) and apricots ( P. armeniaca). Furthermore, the charcoal data show that due to warm and wet climatic conditions in the mid-Holocene, the distribution of tropical-subtropical taxa shifted markedly northwards into the Guanzhong and Tianshui Basins, and the central part of the eastern Loess Plateau, which became characterized by high frequencies of Bamboo.


The Holocene ◽  
2011 ◽  
Vol 22 (1) ◽  
pp. 23-30 ◽  
Author(s):  
Basil Gomez ◽  
Lionel Carter ◽  
Alan R. Orpin ◽  
Kim M. Cobb ◽  
Michael J. Page ◽  
...  

2009 ◽  
Vol 1 (1) ◽  
pp. 109-123 ◽  
Author(s):  
Torben Rick ◽  
Jon Erlandson ◽  
Kristina Horton

2011 ◽  
Vol 38 (2) ◽  
pp. 172-181 ◽  
Author(s):  
Khikmatulla Arslanov ◽  
Olga Druzhinina ◽  
Larisa Savelieva ◽  
Dmitry Subetto ◽  
Ivan Skhodnov ◽  
...  

Abstract The raised bog sediments that have been continuously accumulated over time represent the most suitable natural object which enables us to reconstruct Late Glacial and Holocene vegetation and palaeoclimates. Bog peat consists of organic carbon formed in situ. It contains moss, plant fragments and microfossils that are necessary for the study of palaeovegetation and palaeoclimate. However, a successful study of palaeoenvironment can be carried out on the basis of investigation of a great quantity of samples along the whole peatbog thickness. In the present paper, the authors present the results of palynological, botanical investigations and radiocarbon dating of 31 peat samples taken from the raised bog Velikoye, located in the eastern part of Kaliningrad Region. The data obtained have enabled us to reconstruct the palaeovegetation, reveal the evolution of the bog and determine rate of peat formation at different evolutional stages over the last 7500 cal BP.


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