Lydie Dupont Enno Schefuß, Florian Rommerskirchen, Sebastian Hoetzel, Gerlinde Jung, Gesine Mollenhauer Climate and Vegetation Change in South Africa and.

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Presentation transcript:

Lydie Dupont Enno Schefuß, Florian Rommerskirchen, Sebastian Hoetzel, Gerlinde Jung, Gesine Mollenhauer Climate and Vegetation Change in South Africa and Namibia in relation to the Benguela Upwelling System

Benguela Upwelling System (BUS) geography, importance, development West South Africa & Namibia precipitation and vegetation

SST [°C] Eastern Boundary Currents

Importance of the Benguela Upwelling System (BUS) Etourneau et al. 2010, 2012 Robur.q high marine productivity CO 2 draw down Pleistocene glaciations coastal aridity J Paterson

Brierley et al Eastern Boundary Currents driven by meridional SST gradient Right: Pliocene weaker meridional sea surface temperature gradient results in  weaker and broader atmospheric circulation  weaker Hadley cells  weaker trade winds  weaker Eastern Boundary Currents  weaker upwelling

BUS also driven by uplift of southern Africa Benguela Jet (trade winds pp)

BUS also driven by uplift of southern Africa Benguela Jet (trade winds pp) Jung et al.,  SST [°C] Benguela Jet (trade winds pp) 2 m/s

°E10°E0° 40°S 30°S 20°S 10°S 10°W BUS 30°E SST [°C] ODP sites record BUS development since 10 Ma

Marlow et al. 2000, Rommerskirchen et al. 2011, Hoetzel et al. 2013, Rosell-Melé et al SST development of the BUS since 10 Ma, Northern BUS, ~20°S Middle BUS, ~25°S Southern BUS, ~30°S age [Ma] [°C] Sea Surface Temperatures Pliocene Pleistocene Miocene

Benguela Upwelling System (BUS) geography, importance, development West South Africa & Namibia precipitation and vegetation

Temperature effect Continent effect Altitude effect Amount effect Bowen & Revenaugh, 2003 Deuterium in precipitation

Marlow et al. 2000, Rommerskirchen et al. 2011, Dupont et al. 2013, Hoetzel et al. 2013, Rosell-Melé et al Development of continental precipitation age [Ma] [°C] δD[‰]δD[‰] Deuterium of plant wax Amount Continent, Pliocene Pleistocene Miocene

Vegetation development Dupont et al. 2011, 2013, Hoetzel et al. 2013, δD[‰]δD[‰] tropical element Petalidium fynbos element Stoebe/Elytropappus Deuterium [% pollen] northern BUS southern BUS age [Ma]

Petalidium grass mountain/fynbos: Stoebe/Elytropappus age [Ma] [% pollen] [% pollen] northern BUS southern BUS tropical element Petalidium grass mountain/fynbos: Stoebe/Elytropappus fynbos element Stoebe/Elytropappus grass Dupont et al. 2011, 2013, Hoetzel et al. 2013, 2015

grass  13 C wax [‰] [% pollen] age [Ma] Savanna development Dupont et al southern BUS C 4 plants

C 4 plants age [Ma] desert grass [‰] [% pollen] C 31 C 33 Hoetzel et al. 2013, 2015 northern BUS  13 C wax [% pollen]

[particles/pollen] charcoal grass age [Ma] [‰] [% pollen] C 31 C 33 Hoetzel et al  13 C wax C 4 plants northern BUS

Summary Ma: increased aridity, retreat tropical vegetation elements, expansion C 3 grasses Ma: shift of the precipitation source to the Indian Ocean, further increase in aridity, expansion C 4 grasses/savannas, increased fire activity Ma: further increase in aridity, development of winter rain vegetation, retreat savannas, increase desert vegetation After 2.7 Ma: strong decline in SST, development of the intense upwelling in the middle BUS Thank you for your attention

Bowen GJ, Revenaugh J, Interpolating the isotopic composition of modern meteoric precipitation. Water Resources research, 39, doi: /2003WR Brierley CM, Fedorov AV, Liu Z, Herbert TH, Lawrence KT, Lariviere JP, Greatly Expanded Tropical Warm Pool and Weakened Hadley Circulation in the Early Pliocene. Science, 323: Dupont LM, Linder HP, Rommerskirchen F, Schefuß E, Climate-driven rampant speciation of the Cape flora. Journal of Biogeography, 38: 1059–1068. Dupont LM, Rommerskirchen F, Mollenhauer G, Schefuß E, Miocene to Pliocene changes in South African hydrology and vegetation in relation to the expansion of C4 plants. Earth and Planetary Science Letters, 375: Etourneau J, Schneider RR, Blanz T, Martinez P, Intensification of the Walker and Hadley atmospheric circulations during the Pliocene–Pleistocene climate transition. Earth and Planetary Science Letters, 297: Etourneau J, Ehlert C, Frank M, Martinez P, Schneider RR, Contribution of changes in opal productivity and nutrient distribution in the coastal upwelling systems to Late Pliocene/Early Pleistocene climate cooling. Climate of the Past, 8: Hoetzel S, Dupont LM, Schefuß E, Rommerskirchen F, Wefer G, The role of fire in Miocene to Pliocene C4 grassland and ecosystem evolution. Nature Geoscience, 6: Hoetzel S, Dupont LM, Wefer G, Miocene–Pliocene vegetation change in south-western Africa (ODP Site 1081, offshore Namibia). Palaeogeography, Palaeoclimatology, Palaeoecology, 423: Jung G, Prange M, Schulz M, Uplift of Africa as a potential cause for Neogene intensification of the Benguela upwelling system. Nature Geoscience, 7: Marlow JR, Lange CB, Wefer G, Rosell-Melé A, Upwelling intensification as part of the Pliocene-Pleistocene climate transition. Science, 290: Rommerskirchen F, Condon T, Mollenhauer G, Dupont LM, Schefuß E, Miocene to Pliocene development of surface and sub-surface temperatures in the Benguela Current System. Paleoceanography, 26, PA3216. doi: /2010PA Rosell-Melé A, Martinéz-Garcia A, McClamont EL, Persistent warmth across the Benguela upwelling system during the Pliocene epoch. Earth and Planetary Science Letters, 386: References