Climate During the Late Holocene in the Sahara and the Sahel: Evolution and Consequences on Human Settlement

2006 ◽  
pp. 47-63 ◽  
Author(s):  
R. Vernet
2018 ◽  
Vol 53 (2) ◽  
pp. 209-227 ◽  
Author(s):  
Karen D. Lupo ◽  
Christopher A. Kiahtipes ◽  
Dave N. Schmitt ◽  
Jean-Paul Ndanga ◽  
D. Craig Young ◽  
...  

The Holocene ◽  
2014 ◽  
Vol 24 (6) ◽  
pp. 668-678 ◽  
Author(s):  
Craig Woodward ◽  
James Shulmeister ◽  
Atun Zawadzki ◽  
Geraldine Jacobsen

2013 ◽  
Vol 32 (1) ◽  
Author(s):  
Witold Paweł Alexandrowicz

AbstractThe localities of Late Holocene fluvial sediments in the Podhale basin were subjected to malacological analysis. Two types of mollusc communities were found in these formations. The first type is characterized by a high proportion of species typical of open environments such as the zones of wide valleys. The predomination of shade-loving taxa is typical of the second type which is mainly associated with narrow, V-shaped type valleys. Malacological analysis allowed characterization of these communities and reconstruction of environmental changes over the last few hundred years. Particular attention was paid to the reconstruction of the history of human settlement in the Podhale region and its impact on the transformation of the environment. This impact resulted in massive deforestation and the introduction of wide-scale farming and pastoral practices. Application of this malacological analysis enabled the determination of the anthropogenic pressures, and changes in their intensity, over the last few hundred years.


2017 ◽  
Vol 431 ◽  
pp. 152-167 ◽  
Author(s):  
Soledad de Azevedo ◽  
Mirsha Quinto-Sánchez ◽  
Carolina Paschetta ◽  
Rolando González-José

The Holocene ◽  
2019 ◽  
Vol 30 (3) ◽  
pp. 420-427
Author(s):  
David W Steadman ◽  
Nancy A Albury ◽  
Lizabeth A Carlson ◽  
Richard Franz ◽  
Michelle J LeFebvre ◽  
...  

No native species of tortoises ( Chelonoidis spp.) live today in the Bahamian (Lucayan) Archipelago (= The Bahamas + The Turks and Caicos Islands), although a number of species inhabited these islands at the first human contact in the late-Holocene. Until their extinction, tortoises were the largest terrestrial herbivores in the island group. We report 16 accelerator mass spectrometer (AMS) radiocarbon (14C) dates determined directly on individual bones of indigenous, extinct tortoises from the six Bahamian islands (Abaco, Eleuthera, Flamingo Cay, Crooked, Middle Caicos, Grand Turk) on five different carbonate banks. These 16 specimens probably represent six or seven species of tortoises, although only one ( Chelonoidis alburyorum on Abaco) has been described thus far. Tortoises seem to have survived on most Bahamian islands for only one or two centuries after initial human settlement, which took place no earlier than AD ~700–1000. The exception is Grand Turk, where we have evidence from the Coralie archeological site that tortoises survived for approximately three centuries after human arrival, based on stratigraphically associated 14C dates from both tortoise bones and wood charcoal. The stable isotope values of carbon (σ13C) and nitrogen (σ15N) of dated tortoise fossils show a NW-to-SE trend in the archipelago that may reflect increasing aridity and more consumption of cactus.


1993 ◽  
Vol 40 (1) ◽  
pp. 98-106 ◽  
Author(s):  
David A. Burney

AbstractA 5000-yr stratigraphic record containing fossil pollen, charcoal, and bones of the extinct Quaternary megafauna from Andolonomby, a hypersaline pond in arid southwestern Madagascar, shows evidence for climatic desiccation beginning about 3000 yr B.P. Pollen spectra shift at this time from primarily arboreal taxa characteristic of forests and woodlands of more mesic western Madagascar, to wooded savanna typical of somewhat drier localities. Between 3000 and 2000 yr B.P., the site became increasingly arid. Charcoal and pollen evidence indicates that increased fire and disturbance occurred at the site beginning ca. 1900 yr B.P., probably signaling the beginning of human settlement in the area. The fossil record suggests that various human and natural factors on the island may have interacted in the subsequent millennium to culminate in the extinction of the entire endemic megafauna.


1987 ◽  
Vol 28 (2) ◽  
pp. 274-280 ◽  
Author(s):  
David A. Burney

AbstractThe classic view regarding the cause of the extinction of at least 17 species of large mammals, birds, and reptiles in Madagascar during the late Holocene implicates human use of fire to modify the environment. However, analysis of the charcoal stratigraphy of three sediment cores from Madagascar shows that late Pleistocene and early- to mid-Holocene sediments deposited prior to human settlement often contain more charcoal than postsettlement and modern sediments. This observation, which is confirmed by independent measurements from direct assay and palynological counting techniques, suggests that widely held but previously untested beliefs concerning the importance of anthropogenic fires in late Holocene environmental changes and megafaunal extinctions of Madagascar may be based on an overly simplified version of actual prehistoric conditions. Moderate to low charcoal values characterized only the late Holocene millennia immediately prior to the presumed time of arrival of the first settlers. Human settlement is probably indicated in the stratigraphy by the sharp rise in charcoal content observed beginning ca. 1500 yr B.P. Fire appears to be a significant natural component of prehuman environments in Madagascar, but some factor, probably climate, has modulated the extent of natural burning.


The Holocene ◽  
2005 ◽  
Vol 15 (5) ◽  
pp. 639-647 ◽  
Author(s):  
Gina E. Hannon ◽  
Richard H. W. Bradshaw ◽  
Emily G. Bradshaw ◽  
Ian Snowball ◽  
Stefan Wastegård

CATENA ◽  
2019 ◽  
Vol 176 ◽  
pp. 324-335 ◽  
Author(s):  
G. Bianchini ◽  
S. Cremonini ◽  
D. Di Giuseppe ◽  
R. Gabusi ◽  
M. Marchesini ◽  
...  

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