6 edition of Holocene palaeoenvironmental history of the central Sahara found in the catalog.
Includes bibliographical references and index.
|Statement||editors, Roland Baumhauer, Jürgen Runge.|
|Contributions||Baumhauer, Roland., Runge, Jürgen, 1962-|
|LC Classifications||QE720.2.S24 H65 2009|
|The Physical Object|
|LC Control Number||2008045244|
Thank you for your fast sending for my order of the book "Holocene Settlement of the Egyptian Sahara: Volume 1: The Archaeology of Nabta Playa". I am so sorry to write such a thing but I should ask you. I happened to find out that the page 56 and 57 is lack. Then I ask you to send at least the copy of lacking page. Please fulfill my hope/5(3). During the middle Holocene the central Sahara had a monsoonal summer rain climate with an effective rainfall of – mm per year near the desert-savanna boundary (ca. 22° N). Interaction between the monsoon and the atlantic cyclones also allowed rainfall in other periods of the by:
New discovery of rock fulgurites in the Central Sahara. Chapter 7. In: Baumhauer, R. and Runge, J. (eds), Holocene Palaeoenvironmental History of the Central Sahara. Holocene Palaeoenvironmental History of the Central Sahara: Palaeoecology of Africa Vol. 29, An International Yearbook of Landscape Evolution and Palaeoenvironments Modeling morphodynamic evolution in alluvial estuaries.
The Holocene, () ` [ ] it is important to stress the objective contribution that these volumes make to the prehistory of the eastern Sahara. They are extremely well produced, with ample illustrations and statistics, and no detail is spared in the description of habitation sites and small finds. The central Sahara was intensely occupied at the very onset of the Holocene, when moister conditions re-established after the Younger Dryas. In the study area (SW Libya), a solid 14C chronology dates the occupation of Early Acacus H/G between
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1 geomorphological and palaeoenvironmental research in the south-central sahara in review —roland baumhauer, peter felix-henningsen & brigitta schütt. 2 comparison of proxy-based palaeoenvironmental reconstructions and hindcastmodelled annual precipitation—a review of holocene palaeoenvironmental research in the central sahara.
Get this from a library. Holocene palaeoenvironmental history of the central Sahara. [Roland Baumhauer; Jürgen Runge;] -- "The environmental setting within the Central Sahara was subject to considerable changes during Late Quaternary, mainly driven by major global climate variations, although human impact increased.
In memoriam / Johanna Alida Coetzee () / Klaus Heine --Geomorphological and palaeoenvironmental research in the south-central Sahara in review / Roland Baumhauer, Peter Felix-Henningsen & Brigitta Schütt --Comparison of proxy-based palaeoenvironmental reconstructions and hindcast modelled annual precipitation --a review of Holocene.
Holocene Palaeoenvironmental History of the Central Sahara: Palaeoecology of Africa Vol. 29, An International Yearbook of Landscape Evolution and Palaeoenvironments of Africa and the Surrounding Islands) Roland Baumhauer, Jürgen Runge.
/ Holocene palaeoenviromental changes in Central Sahara inferred from new records from Seggedim scarpfoot depression (NE-Niger) / Of transitions and boundaries. The desert in the Sahara. / Palaeoclimatic interpretation of soil development on Sahelian ancient dunes of different age in Niger, Chad and Mauretania.
Supraregional investigations of the Holocene occupational history of the eastern Sahara west of the Nile combined with the study of climatic, environmental, and geomorphological archives were carried out in contrasting desert regions from the Mediterranean coast strip to Wadi Howar in Sudan.
Holocene palaeoenvironmental changes in the central Sahara (NE-Niger) Holocene paleoenvironmental history of the Central. Sahara, by study of a long sedi ment core from an. The abundant faunal remains from the Takarkori rock shelter in the Tadrart Acacus region of southwestern Libya are described.
The material that covers the period betw to years cal BP illustrates the more humid environmental conditions in the Central Sahara during early and middle Holocene times. Particular attention is focussed on the aquatic fauna that shows marked diachronic Author: Wim Van Neer, Wim Van Neer, Francesca Alhaique, Wim Wouters, Katrien Dierickx, Monica Gala, Quentin.
Holocene Palaeoenvironmental History of the Central Sahara: Palaeoecology of Africa Vol. 29, An International Yearbook of Landscape Evolution and Palaeoenvironments 1st Edition. Roland Baumhauer, Jürgen Runge Febru Johanna Alida Coetzee (also known as Joey Coetzee) was a researcher at the University of the Free State.
Coetzee was born in and was educated first in the Jeppe High School for Girls in Johannesburg before completing a master's degree at the University of the died on 28 April in Somerset West. Coetzee was an expert in pollen research of Africa, whose research Born: Sahara is a adventure novel by Clive Cussler.
It is the eleventh book in Cussler's Dirk Pitt series. The film Sahara was based on the novel. Plot summary. A week before the surrender of Confederate forces of Robert E. Lee inthe Confederate Navy ship CSS Texas is being loaded at a dock with crates supposedly filled with documents. The ship's captain Tombs has been ordered to Author: Clive Cussler.
Palaeoecological studies of terminal Pleistocene and Holocene deposits in the Central Sahara allow some new insights of the palaeoenvironmental development of the vast Ténéré sand plain, Erg of.
Highlights Mangrove dynamics during the p yr was studied by pollen, facies, δ 13 C and C/N. The Amazon mangrove belt is a consequence of the post-glacial sea-level rise.
Marine influence was wider on the Amazon littoral between and cal yr BP. Mangroves were replaced by freshwater vegetation near the Amazon in the late Holocene.
The fragmentation of the mangrove belt was Cited by: Schütt B, Krause J () Comparison of proxy-based palaeoenvironmental reconstructions and hindcast modelled annual precipitation—a review of Holocene palaeoenvironmental research in the Central Sahara. In: Baumhauer R, Runge J (eds) Holocene palaeoenvironmental history of the Central Sahara.
CRC Press, Bota Raton, pp 23–37 Google ScholarCited by: 1. Since the end of the s it has generally been accepted that, during the mid-Holocene humid period, the central Saharan mountain vegetation (Ahaggar, Tassili-n-Ajjer and Tibesti) was clearly Mediterranean or even forest in by: This engrossing book covers so much--from the physical terrain of the Sahara to the explorers and would-be conquerors drawn to it, from the dramatic political and religious history of the region to the well-known movies filmed and set there (Star Wars, The English Patient)/5(8).
Timing of green Sahara periods since 8 Ma Our compilation of middle Pleistocene to Holocene paleoenvironmental records (Figure 3) indicates that marine records provide excellent documentation of circum-Saharan monsoon variability, which complements a continental record that becomes more scarce, fragmentary and difficult to date at older times.
Patches of more arid terrain, for example, are hypothesized for parts of the Central Sahara based on pollen core records from the North Atlantic (Hooghiemstra et al., ) and Holocene lakes in the Central Sahara (Hély et al., ) as well as the fact that some sub-Saharan aquatic species do not exhibit trans-Saharan spatial distributions Cited by: _Sahara_ by Marq de Villiers and Sheila Hirtle is an interesting and thorough book on the natural and human history of the Sahara.
Very informative and comprehensive in scope, the authors tackled a variety of subjects relating to a land known also as the Endless Emptiness or the Great Nothingness/5.
Cremaschi, M () Late Pleistocene and Holocene climatic changes in the Central Sahara. The case of study of the south-western Fezzan, Libya. In: Hassan, FA (ed.) Droughts, Food and by:.
Roland Baumhauer, Jürgen Runge, "Holocene Palaeoenvironmental History of the Central Sahara: Palaeoecology of Africa Vol. 29, An International Yearbook of Landscape Evolution and Palaeoenvironments" CRC; 1 edition (Febru ) | English | | pages |.
In the Central Sahara lying approximately between 27° N and 18° N, rains were primarily due to tropical depressions in the early Holocene up to about BP. Then the monsoon rains of Cited by: HOLOCENE AN ENVIRONMENTAL HISTORY THIRD EDITION NEIL ROBERTS f r e e c o m p a n i o n w e b s i t e f r e e c o m p a n i o n w e b s i t e THE HOLOCENE THIRD EDITION sincewhen the first edition of this book was published, holocene research has File Size: 4MB.