Late Holocene palaeoclimate variability: The significance of bog pine dendrochronology related to peat stratigraphy. The Puścizna Wielka raised bog case study (Orawa – Nowy Targ Basin, Polish Inner Carpathians)

2016 ◽  
Vol 148 ◽  
pp. 192-208 ◽  
Author(s):  
Marek Krąpiec ◽  
Włodzimierz Margielewski ◽  
Katarzyna Korzeń ◽  
Elżbieta Szychowska-Krąpiec ◽  
Dorota Nalepka ◽  
...  
2015 ◽  
Vol 367 ◽  
pp. 62-76 ◽  
Author(s):  
Steffen Schneider ◽  
Albrecht Matthaei ◽  
Marlen Schlöffel ◽  
Cornelius Meyer ◽  
Mario Kronwald ◽  
...  

2022 ◽  
pp. 89-103
Author(s):  
S.J. Sangode ◽  
D.C. Meshram ◽  
A.M. Kandekar ◽  
Amol Abhale ◽  
S.S. Gudadhe ◽  
...  

2016 ◽  
Vol 459 ◽  
pp. 570-584 ◽  
Author(s):  
Elena Yu. Novenko ◽  
Andrey N. Tsyganov ◽  
Elena M. Volkova ◽  
Dmitrii A. Kupriyanov ◽  
Iya V. Mironenko ◽  
...  

Geomorphology ◽  
2014 ◽  
Vol 216 ◽  
pp. 58-78 ◽  
Author(s):  
Knut Kaiser ◽  
Mathias Küster ◽  
Alexander Fülling ◽  
Martin Theuerkauf ◽  
Elisabeth Dietze ◽  
...  

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.


The Holocene ◽  
2004 ◽  
Vol 14 (4) ◽  
pp. 579-588 ◽  
Author(s):  
Mark D. Bateman ◽  
Steven P. Godby

Antiquity ◽  
2008 ◽  
Vol 82 (317) ◽  
pp. 560-570 ◽  
Author(s):  
César A. Méndez M. ◽  
Omar R. Reyes B.

How early did steppe dwellers penetrate the forests? The authors compare and contrast settlement on the steppe, in the forest and on the steep sea coast of western Patagonia, finding that the steppe is occupied first, from 11400 calendar years BP. But around 2800 calendar years BP settlements enter the forest almost simultaneously for a brief period along the length of the Cisnes river valley. Within a few centuries the experiment appears to be abandoned, and the focus of prehistoric peoples returns to the steppe.


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