scholarly journals LATE WEICHSELIAN AND FLANDRIAN POLLEN DIAGRAMS FROM SOUTH-WEST SCOTLAND

1969 ◽  
Vol 68 (2) ◽  
pp. 433-467 ◽  
Author(s):  
N. T. MOAR
2013 ◽  
Vol 53 (2) ◽  
pp. 191-233 ◽  
Author(s):  
Aleksandra Jurochnik ◽  
Dorota Nalepka

ABSTRACT Late Glacial (since Oldest Dryas) and Holocene (to Subatlantic) changes of vegetation at the Węgliny site (south-west Poland) are reconstructed based mainly on pollen analysis of five cores from the palaeobasin (anaerobic sediments). The chronology of the described events is based on palynological comparison with the Lubsza Plain environs, based on LPAZs from several published pollen diagrams on 14C data, and multiple cryptotephra levels determined in the Węgliny profiles. The Węgliny record integrates well into the north European Holocene and Late Glacial biostratigraphic framework. The Węgliny site is the next (fourth) locality in Poland where the Laacher See Tephra (LST) horizon within the Allerød chronozone was identified.


1992 ◽  
Vol 58 (1) ◽  
pp. 227-247 ◽  
Author(s):  
A. C. Stevenson ◽  
R. J. Harrison

Five pollen diagrams from two mires in the province of Huelva in south-west Spain are re-evaluated in the light of 15 radiocarbon dates, and multivariate numerical analyses of modern and fossil pollen samples in the region. The results of these analyses suggest that managed woodland of dehesa type can be detected in pollen diagrams, and can be interpreted within the archaeological sequence known from the area.


1967 ◽  
Vol 67 (6) ◽  
pp. 145-187 ◽  
Author(s):  
Harvey Nichols

SynopsisPalynological investigations were made at two sites in south-west Scotland where peat bogs overlying late Quaternary marine clays and sands were dated by reference to the established British pollen zonation. The “25 foot” shoreline was formed during late Zone VI and early VIIa near Dumfries (c. 8100 to 6600 years B.P.), while the “50 foot” beach near Campbeltown has been referred to Zone III (ending c. 10,000 years B.P.). Close-interval analysis of the upper sections of the pollen diagrams has allowed the recognition of human interference with the vegetation. Minor short-term changes in Zone VI have been tentatively referred to Mesolithic activities, while from Neolithic times (Zone VIIb) onwards there is evidence for an increasingly effective modification of the natural environment. The pollen diagrams allow some conclusions to be drawn about the types of farming (including cereal cultivation) which were characteristic of the settlements near Dumfries and in south Kintyre.


2019 ◽  
Vol 25 ◽  
pp. 317
Author(s):  
Ayotunde Ale ◽  
Opeyemi Aloro ◽  
Ayanbola Adepoju
Keyword(s):  

2019 ◽  
Vol 25 ◽  
pp. 121-122
Author(s):  
Olufunmilayo Adeleye ◽  
Ejiofor Ugwu ◽  
Anthonia Ogbera ◽  
Akinola Dada ◽  
Ibrahim Gezawa ◽  
...  

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