Local vegetation dynamics and human habitation from the last interglacial to the early Holocene at Theopetra cave, central Greece: the evidence from wood charcoal analysis

2015 ◽  
Vol 25 (2) ◽  
pp. 191-206 ◽  
Author(s):  
Maria Ntinou ◽  
Nina Kyparissi-Apostolika
Author(s):  
Maria Ntinou

Wood charcoal analysis at the Sanctuary of Poseidon at Kalaureia, Poros aims to provide information on the vegetation of the area and its management and on the range of plants used in the activities taking place at the sanctuary. During the excavations of 2003–2005 in Areas D and C, systematic samples from fills and features from all the excavated strata were recovered and water flotation was used for the separation of wood charcoal from the sediment. Wood charcoal was found in two pits dated to the Early Iron Age, near the supposed altar of the Archaic period (Feature 05), in a deposit of the Hellenistic period (the “dining deposit”), in floor deposits (Early Iron Age and Late Classical/Early Hellenistic periods), and fills of different chrono-cultural periods (Archaic–Early Roman). All the taxa identified in the wood charcoal assemblages are thermophilous Mediterranean elements, most of them evergreen broad-leaved. The assemblages show that the most frequent taxon is the olive, followed by the prickly oak, the Fabaceae, and the heather. In most assemblages mock privet/buckthorn, strawberry tree, the pear and Prunus family species are present, while Aleppo pine, lentisc, the fig, and the carob trees are less frequent. Olive cultivation was an important economic activity during the whole life of the sanctuary and probably olive pruning constantly provided the sanctuary with fuel. The woodland would be the additional source of firewood for the sanctuary’s needs for fuel for mundane activities such as heating and cooking, for more formal ones, such as sacrifice, but also for industrial activities such as tile firing. Activities related to the reorganization of space and the expansion of the sanctuary may be reflected in charcoal of carpentry by-products as the fir, cypress, and maybe pine remains.


2017 ◽  
Vol 128 (1) ◽  
pp. 125-135 ◽  
Author(s):  
Thomas J. Kelly ◽  
Mark Hardiman ◽  
Michael Lovelady ◽  
J. John Lowe ◽  
Ian P. Matthews ◽  
...  

Antiquity ◽  
2018 ◽  
Vol 92 (362) ◽  
pp. 320-333 ◽  
Author(s):  
Isabelle Théry-Parisot ◽  
Stéphanie Thiébault ◽  
Jean-Jacques Delannoy ◽  
Catherine Ferrier ◽  
Valérie Feruglio ◽  
...  

Abstract


2012 ◽  
Vol 22 (2) ◽  
pp. 115-128 ◽  
Author(s):  
Maria Ntinou ◽  
Ernestina Badal ◽  
Yolanda Carrión ◽  
José Luis Menéndez Fueyo ◽  
Roberto Ferrer Carrión ◽  
...  

The Holocene ◽  
2012 ◽  
Vol 23 (1) ◽  
pp. 127-136 ◽  
Author(s):  
Auréade Henry ◽  
Nicolas Valdeyron ◽  
Laurent Bouby ◽  
Isabelle Théry-Parisot

Charred wood analyses have been performed on three Mesolithic sites located on the Causse de Gramat, a karstic plateau in southwestern France (Lot department): Les Fieux, les Escabasses and le Cuzoul de Gramat. The sites yielded occupations dating from the early to the late Mesolithic (9th to the 6th millennia cal. bc). In the absence of palynological data, charcoal analysis allowed us to characterise the woody environment exploited by Mesolithic hunter-gatherers. Our results point at the minor place of softwoods in the landscape and the local importance of Rosaceae prunoideae, marking an original type of pre-forest vegetation. In order to retrace the local vegetation dynamics, these results are synthesized and discussed thanks to a correspondence analysis, which includes previous anthracological data from Azilian and middle Mesolithic levels of two other sites of the Causse. The homogeneity of the results speaks in favour of the stability of the local environment and confirms the specific vegetation features of the area.


2000 ◽  
Vol 79 (2-3) ◽  
pp. 355-367 ◽  
Author(s):  
P.C. Tzedakis

AbstractThe extent of regional variability in vegetation development in mainland Greece during the last interglacial is considered. Three pollen sequences – Ioannina (northwest Greece),Tenaghi Philippon (northeast Greece) and Kopais (central Greece) – all located in different environmental settings, extend into the last interglacial. Examination of the vegetation histories of the three sites during the last interglacial reveals the influence of local climatic conditions with closed mixed forests in the northwest, becoming progressively more open and less diverse farther to the east and south. All three sequences contain a number of similar trends, however, in the expansion of certain taxa. In addition, they also show the presence of a two-step late glacial interval, a short episode of forest reduction in the second part of the interglacial and a final small expansion of tree populations at the very end of the interglacial. Comparison with other European records shows a number of common features, but also suggests differences consistent with the particular environmental setting of the Greek sites.


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