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Savannas (tropical grasslands)  Distribution  Climate  Controlling factors: soils, fire, grazing  Savanna patchiness  Climate change  Desertification.

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Presentation on theme: "Savannas (tropical grasslands)  Distribution  Climate  Controlling factors: soils, fire, grazing  Savanna patchiness  Climate change  Desertification."— Presentation transcript:

1 Savannas (tropical grasslands)  Distribution  Climate  Controlling factors: soils, fire, grazing  Savanna patchiness  Climate change  Desertification


3 African climate and savanna distribution

4 Savanna ecosystems in W Africa 250 500 1000 1500 2000 Low grass savanna Tall grass savanna Thorn forest Rain forest Desert desert Sahel zone Sudan zone Guinea zone savanna-forest rainforest Precipitation Vegetation

5 Climatic control on savanna distribution and type in West Africa Synoptic situation J F M A M J J A S O N D 25° 20° 15° 10° 5° ITCZ = northern edge of rains rainy season

6 Savanna ecosystems in South and East Africa Low grass savanna Miombo woodland Mopane woodland

7 S American climate and savannas Llanos Cerrado 1500

8 1 2 3 4 5 6 7 1. Honduras 2. Bolivar 3. Llanos 4. Rupununi 5. Amazonas 6. Cerrado 7. S. Brazil

9 Shrubs (6 spp.) 1 2 3 4 5 6 7 0.5 1.0 0.9 0.75 1 2 3 4 5 6 7 0.67 1.0 0.83 0.5 Floristic similarity in S. American savannas (with Rupununi) Herbs (12 spp.)

10 Caribbean pine savannas (Belize - Nicaragua)

11 Are South American savannas primarily products of seasonal drought? Savanna Forest 500 1000 1500 2000 2500 “the vegetation is xerophytic in many places because of the dry season that lasts for months... But the xerophylly is also due to the the dry continental climate in general.” E. Warming, 1909 (on the southern cerrados of Brazil) the climate of the Venezuelan Llanos is “hostile to woodland” Schimper, 1903

12 Common sclerophyllous shrubs, S. American savannas Curatella americana Byrsonima crassifolia

13 Alternative (or supplementary) hypotheses Savanna Forest fire soil senility topography seasonal drought and inundation

14 Soil hydrology Van Donselaar (1969), on the basis of work in Surinam, commented: “Savanna communities are primarily correlated with the hydrology of the soil” In the wet season the savannas of the Venezuelan Llanos (and other flat-lying savanna areas) may be inundated by flood waters for several weeks; in the dry season the water table may drop to depths of several metres. Such fluctuations may be too severe for rainforest trees.

15 Topography: Monica Cole’s observations savanna forest to Brazilian coast -->

16 Topographic control on savanna/forest distribution, Rupununi

17 Savanna-forest boundary (Kakadu National Park, NT, Australia)

18 Frederick Hardy: the senile soil hypothesis

19 Characteristics of senile soils Low pH (4.4 - 5.2) Low cation exchange capacity (clay fraction dominated by kaolinite) Very low base saturation High soluble aluminium Soil nutrients inadequate to support forest growth; only alumino-tolerant trees survive.

20 Plinthite formation Development of iron-rich horizon in zone of fluctuating seasonal water table. Long-term lowering of water table causes irreversible induration of iron-rich horizon (plinthite / laterite / ferricrete). Plinthite inhibits root penetration and causes perched water tables and seasonal inundation.

21 The role of fire “..together with the degradation towards a poor savanna (following on the use of fire) many other changes occur; the soil definitely deteriorates and lateritic iron pans are formed.” Budowski, 1959 (on savanna formation in Nicaragua) Fire as an agricultural tool in the Guinea zone, W. Africa

22 Fire-maintained boundary: Rupununi savannas, Guyana

23 Dry season fires in the forest- savanna zone, Africa, 1987

24 Fire temperatures in tall grass savanna

25 Low grass savannas with sub-shrubs, Rupununi savannas; a cold fire environment

26 Effects of fire protection on tree abundance, SW Nigeria No. of trees (0.2ha plot)

27 Effects of fire protection on tree abundance in savanna, Zambia No. of trees (after 14 yrs)

28 Effects of fire protection on grass abundance in savanna, Zambia % change (1949-1963)

29 The “Oskar-Gulliver” concept “repeated fires can keep (trees) small, but (they) rarely suffer mortality, and large (trees) are virtually immune from fire damage. This.. has been called the Oskar syndrome (after Günter Grass’ character Oskar Matzerath), which emphasizes the potentially advanced age of a small individual, or the Gulliver syndrome (after Jonathan swift’s character..), which emphasizes a tree’s potential to be a giant once it escapes fire. Simulation model(s) … have shown that the distribution of fire intensities at a site can shape the structure of the tree stratum” Higgins et al., 2007 Ecology 88, 1119-1125.

30 “Oskar”: an individual of Palicourea rigida subject to frequent, low- intensity grass fires [Rupununi savannas]

31 The “Oskar- Gulliver” syndrome: field surveys of four savanna areas in South Africa subjected to fire exclusion treatments for ~50 years Higgins et al., 2007 Ecology 88, 1119-1125.

32 Fire use by hunter-gatherers (e.g. northern Australia) “The fine-scale mosaic of burnt and unburnt areas created by mid-dry season Aboriginal landscape burning has clear effects on the distribution of kangaroos. Kangaroos move into burnt moist habitats and away from burnt dry, rocky habitats. Isotopic analysis of scats suggests that the mechanism driving this effect is the increased abundance of nitrogen rich grasses in burnt moist habitats.” Murphy, B.P. & Bowman, D.M.J.S. 2007. J. Biogeography, 34, 237-250.

33 Savanna patch dynamics

34 Acacia patches in savanna: Serengeti, Tanzania

35 Herbivore defences in Acacia species Herbivore thorns companion ants

36 Acacia patch characteristics

37 Termitaria in the Rupununi savannas, Guyana

38 Termitaria in burnt savanna, Kakadu N.P. ( NT, Australia)

39 Leaf litter decomposition by termites

40 Termite mounds: high nutrient patches

41 Grazing sequence: Serengeti rains renewed grass growth zebra …. wildebeest … gazelles coarse ……. new ……….. forbs grasses shoots

42 Serengeti food chain and interactions

43 Serengeti dynamics Wolanski, E., et al., 1999. American Scientist, 87, 526-531 (Fig. 9) Lines = simulation model; dots = observed data rainfall (mm/month) grass (‘00s tons) adult wildebeest (‘000s) lions (‘000s)

44 Grazing patchiness e.g. interactions between zebra, Grant’s gazelle and wildebeest in the Serengeti: patchiness is a product of direct effects (grazing sequence), and indirect effects (nutrient cycle shunt = scat production) What are the results of loss of herbivores? (e.g. 70% of elephants in Serengeti poached in 1980s)

45 “The last acacia”: land management issues in the Serengeti 1890’s - outbreak of rinderpest in East Africa led to mega-death of cattle (and wildebeest) and starvation amongst pastoralists. Fewer people, therefore fewer fires to stimulate grass growth (and kill tree seedlings); 1930-40’s - reduction in fires led to expansion of acacia woodland; 1960’s - wet; cattle numbers increased, but wildebeest did not; fires in savanna were hot, killing tree seedlings; 1963 - rinderpest control program; ungulates recovered; 1970’s - Old acacias (which live to 60-70 years) were dying; few replacements; elephants blamed for destroying young trees; elephants culled; 1990’s - Numbers of buffalo and elephants are far lower due to heavy poaching (although elephants have been increasing since the 1990 ivory ban). The wildebeest population has soared to about 1 million; human-set fires are down to about a quarter of what they were--and the acacias have returned.

46 The last acacia? Views of the Serengeti 1980 1991 Photos: Science 19 December 1997: 278. no. 5346, p. 2059

47 Long-term climate change: Late Pleistocene lake levels in African savannas

48 Evidence of climate change: Holocene vegetation changes in the Lake Victoria region

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