ProjectA3 - Revision history

Emmelyne at 12:35, 2 July 2009

2009-07-02T12:35:54Z

← Older revision		Revision as of 12:35, 2 July 2009
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	* How is the East African Rift migrating southwards and merging/dissecting the Kalahari Plateau?<br>		* How is the East African Rift migrating southwards and merging/dissecting the Kalahari Plateau?<br>
	In order to answer these questions, three subprojects have been coordinated.		In order to answer these questions, three subprojects have been coordinated.
-	</p>	+	<br>
-	<h3>A3.I: Carboniferous to Early Jurassic paleotopography and paleoclimate of South Africa: The Karroo Group</~~h3>~~	+	* <big>A3.I: Carboniferous to Early Jurassic paleotopography and paleoclimate of South Africa: The Karroo Group</big>
-	<p>	+	Coordinators: B. Rubidge, University of Witswatersrand (South Africa) & C. Robin, Rennes University (France)
-	Coordinators:	+	* <big>A3.II: The kinematics of Kalahari Plateau uplift through meso-cenozoic times: a sequence stratigraphic approach</big>
-	* South Africa: B. Rubidge, University of Witswatersrand	+	Coordinators: M.de Wit, Cape Town University (South Africa) & F. Guillocheau, Rennes University (France)
-	* France: C. Robin, Rennes University	+	* <big>A3.III: The Kalahari “Basin” infilling: age, paleotopography and paleoclimate</big>
-	<~~/p>~~	+	Coordinators: W. Cotterill, University of Cape Town (South Africa) & J.J. Tiercelin, Rennes University (France)
-	~~<h3~~>A3.II: The kinematics of Kalahari Plateau uplift through meso-cenozoic times: a sequence stratigraphic approach</~~h3>~~	+
-	<p>	+
-	Coordinators:	+
-	* South Africa: M.de Wit, Cape Town University	+
-	* France: F. Guillocheau, Rennes University	+
-	<~~/p>~~	+
-	~~<h3~~>A3.III: The Kalahari “Basin” infilling: age, paleotopography and paleoclimate</~~h3>~~	+
-	<p>	+
-	Coordinators:	+
-	* South Africa: W. Cotterill, University of Cape Town	+
-	* France: J.J. Tiercelin, Rennes University	+
	</p>		</p>

Emmelyne at 12:29, 2 July 2009

2009-07-02T12:29:49Z

← Older revision		Revision as of 12:29, 2 July 2009
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	South African pi: M. de Wit</h3></center>		South African pi: M. de Wit</h3></center>

-	~~__TOC__~~	+	__NOTOC__
	<br>		<br>
	<h3>Project Participants:</h3>		<h3>Project Participants:</h3>

Emmelyne at 12:12, 2 July 2009

2009-07-02T12:12:43Z

← Older revision		Revision as of 12:12, 2 July 2009
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	<h3>Background</h3>		<h3>Background</h3>
-	<p>The Kalahari Plateau is a 1000-1500 m high plateau that stretches ~2500 km from southern to central Africa. It is the world‟s largest subcontinental plateau away from plate margins, and is separated from the Atlantic and Indian Oceans by a narrow transition of steep scarps and mountain ranges. The origin of this plateau and its margins are not understood but can be traced back to peneplanation near sea-level during the continent-wide end-Paleozoic Gondwana glaciation (~300 My), followed by extensional intracontinental tectonics and desertification during the Late Permian-Triassic (Karoo rifts and basins) and continental break-up during the the Late Jurassic - Early Cretaceous (formation of the Atlantic and Indian Oceans). The peneplain was also affected by extensive volcanic activity: three large flood basalt events (the Karroo, 170-180 My; the Etendeka, 132 My; and the Aghulas (100-90 My) and two punctuated episodes of kimberlite emplacement (around 120 My and 90 My). By mid-end Cretaceous, uplift had started and concomittantly the inland region was transformed into a continental desert. Cenzoic evolution of the Kalahari Plateau has strongly controlled geomorphology, biological evolution (including Hominids), climate change and the hydrology of central and southern African.</p>
	[[image:A3_fig1.jpg\|left\|thumb\|380px\|3-D image showing the African surface elevation, and known kimberlites intrusions (vertical yellow lines) that extend down into the underlying lithospheric mantle. Broad arrows, representing the resultant Mesozoic exhumation (green) and erosion (grey-white) of the Kalahari highlands, removing a carapace of 2-6 km of cover, including a substantial volume of Karoo basalts, at a rate in excess of 0.5 km3/yr, with a high rate of CO2 sequestration, resulting in global climate cooling (de Wit, 2007).]]		[[image:A3_fig1.jpg\|left\|thumb\|380px\|3-D image showing the African surface elevation, and known kimberlites intrusions (vertical yellow lines) that extend down into the underlying lithospheric mantle. Broad arrows, representing the resultant Mesozoic exhumation (green) and erosion (grey-white) of the Kalahari highlands, removing a carapace of 2-6 km of cover, including a substantial volume of Karoo basalts, at a rate in excess of 0.5 km3/yr, with a high rate of CO2 sequestration, resulting in global climate cooling (de Wit, 2007).]]
		+	<p>The Kalahari Plateau is a 1000-1500 m high plateau that stretches ~2500 km from southern to central Africa. It is the world‟s largest subcontinental plateau away from plate margins, and is separated from the Atlantic and Indian Oceans by a narrow transition of steep scarps and mountain ranges. The origin of this plateau and its margins are not understood but can be traced back to peneplanation near sea-level during the continent-wide end-Paleozoic Gondwana glaciation (~300 My), followed by extensional intracontinental tectonics and desertification during the Late Permian-Triassic (Karoo rifts and basins) and continental break-up during the the Late Jurassic - Early Cretaceous (formation of the Atlantic and Indian Oceans). The peneplain was also affected by extensive volcanic activity: three large flood basalt events (the Karroo, 170-180 My; the Etendeka, 132 My; and the Aghulas (100-90 My) and two punctuated episodes of kimberlite emplacement (around 120 My and 90 My). By mid-end Cretaceous, uplift had started and concomittantly the inland region was transformed into a continental desert. Cenzoic evolution of the Kalahari Plateau has strongly controlled geomorphology, biological evolution (including Hominids), climate change and the hydrology of central and southern African.</p>
	<p>The goal of this project is to quantify the growth of this major topographic feature of the Earth – the very long wave length Plateau topography, and the associated rates of uplift over the last 300 My, in order to understand the dynamics of Africa‟s surface processes (erosion, transport, sedimentation) climate change, hydrology, and biological evolution in response to landscape evolution.</p>		<p>The goal of this project is to quantify the growth of this major topographic feature of the Earth – the very long wave length Plateau topography, and the associated rates of uplift over the last 300 My, in order to understand the dynamics of Africa‟s surface processes (erosion, transport, sedimentation) climate change, hydrology, and biological evolution in response to landscape evolution.</p>
	<p>The growth of the Kalahari Plateau is contemporaneous also with a major climatic change at global scale, as well as changes in both elevation and tenures of large lakes and wetlands (including aquifers) across the Plateau. The question of the climate change over the past few tens of millions years in Africa is of primary importance to predict the climate of the future and to understand the evolution of the Hominids in Africa.</p>		<p>The growth of the Kalahari Plateau is contemporaneous also with a major climatic change at global scale, as well as changes in both elevation and tenures of large lakes and wetlands (including aquifers) across the Plateau. The question of the climate change over the past few tens of millions years in Africa is of primary importance to predict the climate of the future and to understand the evolution of the Hominids in Africa.</p>
	<br>		<br>
		+
	<h3>Questions:</h3>		<h3>Questions:</h3>
	<p>		<p>

Emmelyne at 12:11, 2 July 2009

2009-07-02T12:11:35Z

← Older revision		Revision as of 12:11, 2 July 2009
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	South African pi: M. de Wit</h3></center>		South African pi: M. de Wit</h3></center>

		+	__TOC__
		+	<br>
	<h3>Project Participants:</h3>		<h3>Project Participants:</h3>
	<h4>South Africa</h4>		<h4>South Africa</h4>
Line 41:		Line 43:
	<p>The goal of this project is to quantify the growth of this major topographic feature of the Earth – the very long wave length Plateau topography, and the associated rates of uplift over the last 300 My, in order to understand the dynamics of Africa‟s surface processes (erosion, transport, sedimentation) climate change, hydrology, and biological evolution in response to landscape evolution.</p>		<p>The goal of this project is to quantify the growth of this major topographic feature of the Earth – the very long wave length Plateau topography, and the associated rates of uplift over the last 300 My, in order to understand the dynamics of Africa‟s surface processes (erosion, transport, sedimentation) climate change, hydrology, and biological evolution in response to landscape evolution.</p>
	<p>The growth of the Kalahari Plateau is contemporaneous also with a major climatic change at global scale, as well as changes in both elevation and tenures of large lakes and wetlands (including aquifers) across the Plateau. The question of the climate change over the past few tens of millions years in Africa is of primary importance to predict the climate of the future and to understand the evolution of the Hominids in Africa.</p>		<p>The growth of the Kalahari Plateau is contemporaneous also with a major climatic change at global scale, as well as changes in both elevation and tenures of large lakes and wetlands (including aquifers) across the Plateau. The question of the climate change over the past few tens of millions years in Africa is of primary importance to predict the climate of the future and to understand the evolution of the Hominids in Africa.</p>
		+	<br>
	<h3>Questions:</h3>		<h3>Questions:</h3>
	<p>		<p>

Emmelyne at 12:09, 2 July 2009

2009-07-02T12:09:19Z

← Older revision		Revision as of 12:09, 2 July 2009
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	* Annie Vincens, CEREGE, Marseille - III - Palynology		* Annie Vincens, CEREGE, Marseille - III - Palynology

-	<h3>~~Project~~</h3>	+	<h3>Background</h3>
	<p>The Kalahari Plateau is a 1000-1500 m high plateau that stretches ~2500 km from southern to central Africa. It is the world‟s largest subcontinental plateau away from plate margins, and is separated from the Atlantic and Indian Oceans by a narrow transition of steep scarps and mountain ranges. The origin of this plateau and its margins are not understood but can be traced back to peneplanation near sea-level during the continent-wide end-Paleozoic Gondwana glaciation (~300 My), followed by extensional intracontinental tectonics and desertification during the Late Permian-Triassic (Karoo rifts and basins) and continental break-up during the the Late Jurassic - Early Cretaceous (formation of the Atlantic and Indian Oceans). The peneplain was also affected by extensive volcanic activity: three large flood basalt events (the Karroo, 170-180 My; the Etendeka, 132 My; and the Aghulas (100-90 My) and two punctuated episodes of kimberlite emplacement (around 120 My and 90 My). By mid-end Cretaceous, uplift had started and concomittantly the inland region was transformed into a continental desert. Cenzoic evolution of the Kalahari Plateau has strongly controlled geomorphology, biological evolution (including Hominids), climate change and the hydrology of central and southern African.</p>		<p>The Kalahari Plateau is a 1000-1500 m high plateau that stretches ~2500 km from southern to central Africa. It is the world‟s largest subcontinental plateau away from plate margins, and is separated from the Atlantic and Indian Oceans by a narrow transition of steep scarps and mountain ranges. The origin of this plateau and its margins are not understood but can be traced back to peneplanation near sea-level during the continent-wide end-Paleozoic Gondwana glaciation (~300 My), followed by extensional intracontinental tectonics and desertification during the Late Permian-Triassic (Karoo rifts and basins) and continental break-up during the the Late Jurassic - Early Cretaceous (formation of the Atlantic and Indian Oceans). The peneplain was also affected by extensive volcanic activity: three large flood basalt events (the Karroo, 170-180 My; the Etendeka, 132 My; and the Aghulas (100-90 My) and two punctuated episodes of kimberlite emplacement (around 120 My and 90 My). By mid-end Cretaceous, uplift had started and concomittantly the inland region was transformed into a continental desert. Cenzoic evolution of the Kalahari Plateau has strongly controlled geomorphology, biological evolution (including Hominids), climate change and the hydrology of central and southern African.</p>
	[[image:A3_fig1.jpg\|left\|thumb\|380px\|3-D image showing the African surface elevation, and known kimberlites intrusions (vertical yellow lines) that extend down into the underlying lithospheric mantle. Broad arrows, representing the resultant Mesozoic exhumation (green) and erosion (grey-white) of the Kalahari highlands, removing a carapace of 2-6 km of cover, including a substantial volume of Karoo basalts, at a rate in excess of 0.5 km3/yr, with a high rate of CO2 sequestration, resulting in global climate cooling (de Wit, 2007).]]		[[image:A3_fig1.jpg\|left\|thumb\|380px\|3-D image showing the African surface elevation, and known kimberlites intrusions (vertical yellow lines) that extend down into the underlying lithospheric mantle. Broad arrows, representing the resultant Mesozoic exhumation (green) and erosion (grey-white) of the Kalahari highlands, removing a carapace of 2-6 km of cover, including a substantial volume of Karoo basalts, at a rate in excess of 0.5 km3/yr, with a high rate of CO2 sequestration, resulting in global climate cooling (de Wit, 2007).]]
-	<p>The goal of this project is to quantify the growth of this major topographic feature of the Earth – the very long wave length Plateau topography, and the associated rates of uplift over the last 300 My, in order to understand the dynamics of Africa‟s surface processes (erosion, transport, sedimentation) climate change, hydrology, and biological evolution in response to landscape evolution.	+	<p>The goal of this project is to quantify the growth of this major topographic feature of the Earth – the very long wave length Plateau topography, and the associated rates of uplift over the last 300 My, in order to understand the dynamics of Africa‟s surface processes (erosion, transport, sedimentation) climate change, hydrology, and biological evolution in response to landscape evolution.</p>
		+	<p>The growth of the Kalahari Plateau is contemporaneous also with a major climatic change at global scale, as well as changes in both elevation and tenures of large lakes and wetlands (including aquifers) across the Plateau. The question of the climate change over the past few tens of millions years in Africa is of primary importance to predict the climate of the future and to understand the evolution of the Hominids in Africa.</p>
		+	<h3>Questions:</h3>
		+	<p>
		+	* What was the initial topography, prior to the growth of the Plateau?
		+	* Was the Plateau growth continuous or discontinuous, and at what rate?
		+	* Did the observed uplift drive local/global climate change?
		+	* How did Plateau uplift affect lake and river drainage and biodiverity evolution?
		+	* Is the Plateau currently rising (or subsiding) and deforming?
		+	* How is the East African Rift migrating southwards and merging/dissecting the Kalahari Plateau?<br>
		+	In order to answer these questions, three subprojects have been coordinated.
		+	</p>
		+	<h3>A3.I: Carboniferous to Early Jurassic paleotopography and paleoclimate of South Africa: The Karroo Group</h3>
		+	<p>
		+	Coordinators:
		+	* South Africa: B. Rubidge, University of Witswatersrand
		+	* France: C. Robin, Rennes University
		+	</p>
		+	<h3>A3.II: The kinematics of Kalahari Plateau uplift through meso-cenozoic times: a sequence stratigraphic approach</h3>
		+	<p>
		+	Coordinators:
		+	* South Africa: M.de Wit, Cape Town University
		+	* France: F. Guillocheau, Rennes University
		+	</p>
		+	<h3>A3.III: The Kalahari “Basin” infilling: age, paleotopography and paleoclimate</h3>
		+	<p>
		+	Coordinators:
		+	* South Africa: W. Cotterill, University of Cape Town
		+	* France: J.J. Tiercelin, Rennes University
		+	</p>
		+
		+	<h3>Capacity Building through Interactive student mentoring and development</h3>
		+	<p>
		+	Exchange between South African and French students.
		+	* 1 South African PhD and 2 French MSc students on the Upper Karroo sedimentology and sequence stratigraphy (Wits/Rennes)
		+	* 1 South African PhD student on the seismic stratigraphy of the Margin (UCT/Rennes)
		+	* 1 French or South African PhD and 2 South African MSc students on the core analysis of drillings (sedimentology and sequence stratigraphy) of the Kalahari deposits (UCT/Rennes)
		+	* 2 South African MSc on palaeoegeomorphology (South African Escarpment evolution)
		+	* 1 South African Post-Doc for compilation and synthesis of palaeo-environmental scenarios in geospatial context, building on AEON databases (UCT/Rennes/IPGP
		+	</p>
		+	<h3>Economic implications and industry collaborations</h3>
		+	<p>We can expect economic implications of our studies on uranium geology (subproject I), on petroleum and gas location and migration (subproject II) and on sedimentary diamonds prospects (subprojects II and III). The following companies have shown interests in participation: South African Petroleum, De Beers, BRC diamond)</p>
		+	<h3>Relevent review reference:</h3>
		+	<p>
		+	* de Wit, M.J. 2007. The Kalahari epeirogeny and climate change: differentiating cause and effect from core to space. South African Journal of Geology, 110, 367-392
		+	</p>

Emmelyne at 12:00, 2 July 2009

2009-07-02T12:00:49Z

← Older revision		Revision as of 12:00, 2 July 2009
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	<h3>Project</h3>		<h3>Project</h3>
	<p>The Kalahari Plateau is a 1000-1500 m high plateau that stretches ~2500 km from southern to central Africa. It is the world‟s largest subcontinental plateau away from plate margins, and is separated from the Atlantic and Indian Oceans by a narrow transition of steep scarps and mountain ranges. The origin of this plateau and its margins are not understood but can be traced back to peneplanation near sea-level during the continent-wide end-Paleozoic Gondwana glaciation (~300 My), followed by extensional intracontinental tectonics and desertification during the Late Permian-Triassic (Karoo rifts and basins) and continental break-up during the the Late Jurassic - Early Cretaceous (formation of the Atlantic and Indian Oceans). The peneplain was also affected by extensive volcanic activity: three large flood basalt events (the Karroo, 170-180 My; the Etendeka, 132 My; and the Aghulas (100-90 My) and two punctuated episodes of kimberlite emplacement (around 120 My and 90 My). By mid-end Cretaceous, uplift had started and concomittantly the inland region was transformed into a continental desert. Cenzoic evolution of the Kalahari Plateau has strongly controlled geomorphology, biological evolution (including Hominids), climate change and the hydrology of central and southern African.</p>		<p>The Kalahari Plateau is a 1000-1500 m high plateau that stretches ~2500 km from southern to central Africa. It is the world‟s largest subcontinental plateau away from plate margins, and is separated from the Atlantic and Indian Oceans by a narrow transition of steep scarps and mountain ranges. The origin of this plateau and its margins are not understood but can be traced back to peneplanation near sea-level during the continent-wide end-Paleozoic Gondwana glaciation (~300 My), followed by extensional intracontinental tectonics and desertification during the Late Permian-Triassic (Karoo rifts and basins) and continental break-up during the the Late Jurassic - Early Cretaceous (formation of the Atlantic and Indian Oceans). The peneplain was also affected by extensive volcanic activity: three large flood basalt events (the Karroo, 170-180 My; the Etendeka, 132 My; and the Aghulas (100-90 My) and two punctuated episodes of kimberlite emplacement (around 120 My and 90 My). By mid-end Cretaceous, uplift had started and concomittantly the inland region was transformed into a continental desert. Cenzoic evolution of the Kalahari Plateau has strongly controlled geomorphology, biological evolution (including Hominids), climate change and the hydrology of central and southern African.</p>
-	[[image:A3_fig1.jpg\|left\|thumb\|~~300px~~\|3-D image showing the African surface elevation, and known kimberlites intrusions (vertical yellow lines) that extend down into the underlying lithospheric mantle. Broad arrows, representing the resultant Mesozoic exhumation (green) and erosion (grey-white) of the Kalahari highlands, removing a carapace of 2-6 km of cover, including a substantial volume of Karoo basalts, at a rate in excess of 0.5 km3/yr, with a high rate of CO2 sequestration, resulting in global climate cooling (de Wit, 2007).]]	+	[[image:A3_fig1.jpg\|left\|thumb\|380px\|3-D image showing the African surface elevation, and known kimberlites intrusions (vertical yellow lines) that extend down into the underlying lithospheric mantle. Broad arrows, representing the resultant Mesozoic exhumation (green) and erosion (grey-white) of the Kalahari highlands, removing a carapace of 2-6 km of cover, including a substantial volume of Karoo basalts, at a rate in excess of 0.5 km3/yr, with a high rate of CO2 sequestration, resulting in global climate cooling (de Wit, 2007).]]
	<p>The goal of this project is to quantify the growth of this major topographic feature of the Earth – the very long wave length Plateau topography, and the associated rates of uplift over the last 300 My, in order to understand the dynamics of Africa‟s surface processes (erosion, transport, sedimentation) climate change, hydrology, and biological evolution in response to landscape evolution.		<p>The goal of this project is to quantify the growth of this major topographic feature of the Earth – the very long wave length Plateau topography, and the associated rates of uplift over the last 300 My, in order to understand the dynamics of Africa‟s surface processes (erosion, transport, sedimentation) climate change, hydrology, and biological evolution in response to landscape evolution.

Emmelyne at 12:00, 2 July 2009

2009-07-02T12:00:31Z

← Older revision		Revision as of 12:00, 2 July 2009
Line 38:		Line 38:
	<h3>Project</h3>		<h3>Project</h3>
	<p>The Kalahari Plateau is a 1000-1500 m high plateau that stretches ~2500 km from southern to central Africa. It is the world‟s largest subcontinental plateau away from plate margins, and is separated from the Atlantic and Indian Oceans by a narrow transition of steep scarps and mountain ranges. The origin of this plateau and its margins are not understood but can be traced back to peneplanation near sea-level during the continent-wide end-Paleozoic Gondwana glaciation (~300 My), followed by extensional intracontinental tectonics and desertification during the Late Permian-Triassic (Karoo rifts and basins) and continental break-up during the the Late Jurassic - Early Cretaceous (formation of the Atlantic and Indian Oceans). The peneplain was also affected by extensive volcanic activity: three large flood basalt events (the Karroo, 170-180 My; the Etendeka, 132 My; and the Aghulas (100-90 My) and two punctuated episodes of kimberlite emplacement (around 120 My and 90 My). By mid-end Cretaceous, uplift had started and concomittantly the inland region was transformed into a continental desert. Cenzoic evolution of the Kalahari Plateau has strongly controlled geomorphology, biological evolution (including Hominids), climate change and the hydrology of central and southern African.</p>		<p>The Kalahari Plateau is a 1000-1500 m high plateau that stretches ~2500 km from southern to central Africa. It is the world‟s largest subcontinental plateau away from plate margins, and is separated from the Atlantic and Indian Oceans by a narrow transition of steep scarps and mountain ranges. The origin of this plateau and its margins are not understood but can be traced back to peneplanation near sea-level during the continent-wide end-Paleozoic Gondwana glaciation (~300 My), followed by extensional intracontinental tectonics and desertification during the Late Permian-Triassic (Karoo rifts and basins) and continental break-up during the the Late Jurassic - Early Cretaceous (formation of the Atlantic and Indian Oceans). The peneplain was also affected by extensive volcanic activity: three large flood basalt events (the Karroo, 170-180 My; the Etendeka, 132 My; and the Aghulas (100-90 My) and two punctuated episodes of kimberlite emplacement (around 120 My and 90 My). By mid-end Cretaceous, uplift had started and concomittantly the inland region was transformed into a continental desert. Cenzoic evolution of the Kalahari Plateau has strongly controlled geomorphology, biological evolution (including Hominids), climate change and the hydrology of central and southern African.</p>
-	[[image:A3_fig1.jpg\|left\|300px\|3-D image showing the African surface elevation, and known kimberlites intrusions (vertical yellow lines) that extend down into the underlying lithospheric mantle. Broad arrows, representing the resultant Mesozoic exhumation (green) and erosion (grey-white) of the Kalahari highlands, removing a carapace of 2-6 km of cover, including a substantial volume of Karoo basalts, at a rate in excess of 0.5 km3/yr, with a high rate of CO2 sequestration, resulting in global climate cooling (de Wit, 2007).]]	+	[[image:A3_fig1.jpg\|left\|thumb\|300px\|3-D image showing the African surface elevation, and known kimberlites intrusions (vertical yellow lines) that extend down into the underlying lithospheric mantle. Broad arrows, representing the resultant Mesozoic exhumation (green) and erosion (grey-white) of the Kalahari highlands, removing a carapace of 2-6 km of cover, including a substantial volume of Karoo basalts, at a rate in excess of 0.5 km3/yr, with a high rate of CO2 sequestration, resulting in global climate cooling (de Wit, 2007).]]
	<p>The goal of this project is to quantify the growth of this major topographic feature of the Earth – the very long wave length Plateau topography, and the associated rates of uplift over the last 300 My, in order to understand the dynamics of Africa‟s surface processes (erosion, transport, sedimentation) climate change, hydrology, and biological evolution in response to landscape evolution.		<p>The goal of this project is to quantify the growth of this major topographic feature of the Earth – the very long wave length Plateau topography, and the associated rates of uplift over the last 300 My, in order to understand the dynamics of Africa‟s surface processes (erosion, transport, sedimentation) climate change, hydrology, and biological evolution in response to landscape evolution.

Emmelyne at 11:59, 2 July 2009

2009-07-02T11:59:05Z

← Older revision		Revision as of 11:59, 2 July 2009
Line 35:		Line 35:
	* Jean-Jacques Tiercelin, Rennes 1 University - III - Sedimentology		* Jean-Jacques Tiercelin, Rennes 1 University - III - Sedimentology
	* Annie Vincens, CEREGE, Marseille - III - Palynology		* Annie Vincens, CEREGE, Marseille - III - Palynology
		+
		+	<h3>Project</h3>
		+	<p>The Kalahari Plateau is a 1000-1500 m high plateau that stretches ~2500 km from southern to central Africa. It is the world‟s largest subcontinental plateau away from plate margins, and is separated from the Atlantic and Indian Oceans by a narrow transition of steep scarps and mountain ranges. The origin of this plateau and its margins are not understood but can be traced back to peneplanation near sea-level during the continent-wide end-Paleozoic Gondwana glaciation (~300 My), followed by extensional intracontinental tectonics and desertification during the Late Permian-Triassic (Karoo rifts and basins) and continental break-up during the the Late Jurassic - Early Cretaceous (formation of the Atlantic and Indian Oceans). The peneplain was also affected by extensive volcanic activity: three large flood basalt events (the Karroo, 170-180 My; the Etendeka, 132 My; and the Aghulas (100-90 My) and two punctuated episodes of kimberlite emplacement (around 120 My and 90 My). By mid-end Cretaceous, uplift had started and concomittantly the inland region was transformed into a continental desert. Cenzoic evolution of the Kalahari Plateau has strongly controlled geomorphology, biological evolution (including Hominids), climate change and the hydrology of central and southern African.</p>
		+	[[image:A3_fig1.jpg\|left\|300px\|3-D image showing the African surface elevation, and known kimberlites intrusions (vertical yellow lines) that extend down into the underlying lithospheric mantle. Broad arrows, representing the resultant Mesozoic exhumation (green) and erosion (grey-white) of the Kalahari highlands, removing a carapace of 2-6 km of cover, including a substantial volume of Karoo basalts, at a rate in excess of 0.5 km3/yr, with a high rate of CO2 sequestration, resulting in global climate cooling (de Wit, 2007).]]
		+	<p>The goal of this project is to quantify the growth of this major topographic feature of the Earth – the very long wave length Plateau topography, and the associated rates of uplift over the last 300 My, in order to understand the dynamics of Africa‟s surface processes (erosion, transport, sedimentation) climate change, hydrology, and biological evolution in response to landscape evolution.

Emmelyne: New page:
Project A3:
Plateau uplift, epeirogeny and evolution of climate and biodiversity

French pi: F. Guillocheau
South African pi: M. de Wit

Proje...

2009-07-02T11:52:37Z

New page: <center><h2>Project A3:<br> Plateau uplift, epeirogeny and evolution of climate and biodiversity</h2> <h3>French pi: F. Guillocheau<br> South African pi: M. de Wit</h3></center> <h3>Proje...

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<center><h2>Project A3:<br>
Plateau uplift, epeirogeny and evolution of climate and biodiversity</h2>
<h3>French pi: F. Guillocheau<br>
South African pi: M. de Wit</h3></center>

<h3>Project Participants:</h3>
<h4>South Africa</h4>
* Fernando Abdala, University Witwatersrand - I - Therapsid taxonomy
* Marion Bamford, University Witwatersrand - I - Fossil wood taxonomy
* Jennifer Botha-Brink, National Museum - I - Parareptiles, Bone histology, physiology
* Doug Cole, Council for Geoscience - I - Sedimentology, lithostratigraphy
* John Compton, University of Cape Town - V - Marine Sedimentology
* Woody Cotterill, University of Cape Town - I,III - Biodiversity dynamics, palaeo drainage
* Maarten de Wit, University of Cape Town - I,II, III - Tectonics, geochronology,
* Frank Eckardt, University of Cape Town - III - Geomorphology, palaeo-drainage
* Julia Lee-Thorpe, University of Bedford - III - Biology, stable isotopes, hominims
* Johann Neveling, Council for Geoscience - I - Sedimentology, basin modelling
* Merrill Nicolas, University Witwatersrand - I - GIS database
* Rose Prevec, Albany Museum - I - Megaplant taxonomy
* Bruce Rubidge, University Witwatersrand - I - Therapsid taxonomy, biostratigraphy
* Roger Smith, SA Museum - I - Taphonomy, biodiversity changes
* Adam Yates, University Witwatersrand - I - Dinosaur taxonomy

<h4>France</h4>
* Sylvie Bourquin, Rennes 1 University - I - Fluvial sedimentology
* Jean Braun, Rennes 1 University - II - Modelling
* Luc Bulot, Marseille University - II - Biostratigraphy
* Olivier Dauteuil, Rennes 1 University - II - Tectonics
* Francois Guillocheau, Rennes 1 University - I, II, III - Sedimentology, Seismic stratigraphy
* Alain Le Herisse, Brest University - I - Palynology
* Cécile Robin, Rennes 1 University - I, II - Sedimentology, Seismic stratigraphy
* Delphine Rouby, Rennes 1 University - II - Seismic stratigraphy
* Martine Simoes, IPGP - II - Modelling
* Paul Tapponier, IPGP - II - Tectonics
* Jean-Jacques Tiercelin, Rennes 1 University - III - Sedimentology
* Annie Vincens, CEREGE, Marseille - III - Palynology

ProjectA3 - Revision history

Emmelyne at 12:35, 2 July 2009

Emmelyne at 12:29, 2 July 2009

Emmelyne at 12:12, 2 July 2009

Emmelyne at 12:11, 2 July 2009

Emmelyne at 12:09, 2 July 2009

Emmelyne at 12:00, 2 July 2009

Emmelyne at 12:00, 2 July 2009

Emmelyne at 11:59, 2 July 2009

Emmelyne: New page: Project A3: Plateau uplift, epeirogeny and evolution of climate and biodiversity French pi: F. Guillocheau South African pi: M. de Wit

Project A3: Plateau uplift, epeirogeny and evolution of climate and biodiversity

French pi: F. Guillocheau South African pi: M. de Wit

Proje...

Emmelyne: New page:
Project A3:
Plateau uplift, epeirogeny and evolution of climate and biodiversity

French pi: F. Guillocheau
South African pi: M. de Wit

Project A3:
Plateau uplift, epeirogeny and evolution of climate and biodiversity

French pi: F. Guillocheau
South African pi: M. de Wit