Antelope Species of Botswana and Kenya

The antelope species make up the vast majority of Africa’s wild mammal population.* There are millions of them grazing across the land. They are vegetarian. Grazing animals consume the annual growth of the Savana and woodlands. They trim the grass, shrubs and trees. They are prey for the carnivores and spread the seeds of the plants. They are an integral part of this great ecosystem.

The feature image is a magnificent male Greater Kudu in a forested area of the Okavango Delta

These animals are part of an animal clade called Ungulates(**) because of their toes with hooves. The ungulates also have horns that are bilaterally symmetric without branches but with variations such as twists, spirals, rings and flutes. These appendages are bone covered with keratin. They are well adapted to their coarse vegetarian diet and have a specialized digestive system which allows them to digest cellulose.

They all move together in groups because safety is in numbers. Part of that behavior includes mixing with a herd of other similar grazing animals for added protection. Included in this group are Gazelle, Bushbuck, Waterbuck, Eland, Reedbuck, Gerenuk, Dik-dik, Kudu (lesser & greater), Wildebeest, Ayala, Bongo, Oryx and Impala.

My first introduction to the antelopes was a charmer. The little doe wandered into our campsite and simply walked in front of me as if by magic. Fortunately, I had my camera and like it was by plan she waited and posed for me for this portraits.

Cape Bush Buck faun. This animal is usually shy but will become habituated to humans and stay near the lodge. A real cutie!

These animals had the most interesting behaviors, colors and horns. I found the Impala to be the most beautiful. They have such large eyes and their coats are gorgeous; so shiny and without any blemishes. The distinctive markings on their rumps are narrow vertical black stripes. They are also very busy. Unlike the big cats, they are always involved in some activity. Since they are grazers they eat the low grasses. This unfortunately distracts their attention and they can’t look up for dangerous prey like lions or dogs. Therefore, when you see them, there is a rotation of grazers and sentinels with their heads up. When they are chased or pursued they are extraordinarily fast and agile. When fighting for dominance in their herd they use their horns, sometimes with deadly precision.

Female Impalas (Aephyceros melampus) in wooded area of the Okavango. Note their shorter horns compared to the males.
Two male impala dueling with interlaced horns They were probably sparing and not fighting for dominance because the males were not separated from the females. Boys! Be careful when you play with those sharp things!
Male and female Impala drinking from a small creek in Maasai Mara. These antelope were everywhere. They were probably the most numerous and sometimes they herded together in groups of 50 or more.
Hoof print of an antelope. Probably Impala. Note the “split” of the keratin hoof, showing the characteristic two toes. (***)
Impala and Lesser Kudu sharing space at the riverside in Chobe National Park, Okavango, Botswana. Check out the Impala scouting the background.

Perhaps one of the remarkable features of the giant Kudu antelopes was their spiral horns. Spiraled but nearly straight, the antlers of the Kudu were the most distinguished. The white stripes of their coats were also easily recognizable.

Greater Kudo, (Tragelaphus strepsiceros) with beautifully spiraled horns
Greater Kudu mixed with a herd of Zebra in the marshland of Okavango Delta of Botswana. It was easy to identify these large animals. Birds on the bodies of the Kudu eat the insects that are a pest for the large mammal.
Tsessebe are sometimes called the “Blue Jeans antelope” because of its distinctive leg coloration.
Lechwe (Kobus leche) Standing in front of our tent in late afternoon.

During a game drive through the shallow swamp the water buck obliged us with his massive ringed horns.

Water buck (Kobus ellipsiprymnus) In the Okavango Delta marsh.

If our guide had not pointed it out I would have easily missed seeing the Dik-dik. It is so small and blends so easily with the ground color that it was almost invisible. It was smaller than the tiny doe that visited the camp site on another occasion.

Dik-dik (Madoqua kirkii) Smallest of the antelope species is only18 inches tall.
Gerenuk (Litocranius walleri) standing on its hind legs eating leaves. This is a typical behavior.
Oryx (Oryx beisa) Long straight ringed horns and painted face are signature trademarks for this large animal.
Thompson’s Gazelle (Eudorcas thompsonii) Straight horns with rings dark band along the lateral aspect of the ribcage. Smaller than the Impala and the Grant’s gazelle. Almost as fast as a cheetah and very numerous.
Grant’s Gazelle (Gazella granti) (Nanger granti) White rump, straight horns and black facial patches. Beautiful dramatic evening lighting.
Hartebeest (AKA Kongoni) (Alcelaphus buselaphus) This is a very rare finding because this animal is facing imminent extinction. A five party group of them was grazing in the Maasai Mara.
Roan antelope (Hippotragus equinus). One of the largest of the antelope with a roan color or a reddish-brown coat.
Wildebeest (Connabaetes taurines). We have previously posted on this species of antelope and the Great Migration.

Along with the general mix of the population, the antelope species have an important and sometimes grim role in the African landscape. They are the object of the predators. We have already reviewed the predators of this region. Check out our blog site that describes the wild dogs of Africa.


* Uganda antelope

** What is an ungulate?

*** African Animal Tracks

#antelope #Gazelle #Bushbuck #Waterbuck #Gerenuk, #Dik-dik #Kudu #Wildebeest #Oryx #Impala #Africa #Botswana #Okavango #Kenya #Maasai Mara #horns #hoof #ungulates

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Wild Africa – A Trip In the Plan for 30 Years

An overview:

The previous posting on Africa showed the photographic preparation for the trip. This posting is an introduction to the upcoming blogs which will feature the animal and plant wildlife in more detail. This photo safari was planned for thirty years. It has been postponed three times. At last, this was the opportunity to go. Botswana and Kenya are the two countries we visited in sub-Saharan Africa. The reasons to go there were their diversity of wildlife, ecosystems, and safety. The month of August was selected to be timely to see the greatest density of animals in the most clement season. It was also an opportunity to look for the similarities and differences of the comparable African and US locations. Here are thoughts, impressions and recounting of the two weeks of experience there.

The title sunset image is typical of the African sky. The beautiful sunset red comes from sand and minerals of the desert suspended in the air and refracted by the light. These same sands which are blown across the Atlantic Ocean color our Floridian sunsets too.

This lengthy monologue is only a rudimentary description of a very large subject. It is intended to help understand and appreciate the reasons for these features seen on this expedition and to summarize the complexities of the climate, geology, the flow of water on the land, the interdependency of species and some similarities to areas in the USA. The two major eco systems were marshlands and savanna. In Botswana the wetlands of the Okavango delta were the focal point. In Kenya the savanna of the Maasai Mara section of the Serengeti was of greatest interest. The Okavango delta ecosystem has some similarities to the wetlands found in the Southwest Florida Everglades National and State Park systems. The Maasai Mara is more like the grasslands of Montana where, 250 years ago, buffalo, antelope, elk, and wolf roamed in their own great migration.

Climate and Geology:

The Okavango delta is 19 degrees south of the Equator. The Florida Everglades are 19 degrees north of the equator. They receive approximately the same amount of energy from the sun. The marshlands of the Okavango delta and the Florida Everglades are both essentially inland dispersions of fresh water. The Okavango is a unique feature of the Kalahari Desert. This delta is deep in the interior of the land mass and the climate is continental. Unlike the Everglades, it does not have the moderating exposure to a neighboring ocean. It has a soil basis of sand that averages 200 feet deep. On top of that is a soil of a few inches depth with mixtures of soil brought by wind, flood, and a thin organic compost. The average elevation is 3100 ft. The delta has three biome types that include savanna, woodlands, and swamp. The Okavango River supply is derived from the confluence of the Cubango and Cuito rivers in Angola. The annual flow reaches the delta between March and June with maximum flow in July. Additionally, there is seasonal 18-inch rainfall in the Okavango from November to February which adds to water shed. 

Floridian Everglades are at sea level and are founded on petrified sea bottom called sedimentary rock with a high calcium carbonate basis called limestone. The Florida Everglades topsoil is an average 17-foot-thick layer of marl (calcitic mud), peat and muck. The Everglades are subtropical wetlands whose freshwater system begins near Orlando in the Kissimmee River. The average annual rainfall is 60 inches. The Everglades have a maritime weather with tropical storms and moderation of climate. Climatically, there are no hurricanes in the Okavango and in the Everglades there is no drought.

In support of the science of plate tectonics. The Americas and Africa were one land mass 200 million years ago.

The concept of moving plates of the crust of the earth suggests that at a distant time in the past the assembly of the plates separated into the various land bodies. The shapes of the land mass fragments seen today can be manipulated as puzzle pieces into a larger land mass that fits together quite well. This particular assembly is called Pangea. If this is how the continents formed then there is a strong relationship between the eastern geology of the Americas and the western African geology. This fit is not entirely perfect, however, when considering the length of time for the division to transpire it is remarkably good. This has been supported by substantial evidence of rock formations that span the continents.The science is based on continental fit, matching rocks, fossils, corals, mountains, glacial striations, magnetic lineages and direct measurement of the movement.

Plate tectonics

Comparison of ecosystems:

Water and Land:

About 98% of the water that goes into the Okavango delta is eventually lost through evaporation and transpiration.  Transpiration results when water moves through the plant and evaporates from leaves and flowers. Despite the subtropical sun generating intense evaporation, the delta’s water is fresh, not salty. I was surprised by this because non circulating ponds of water in the middle parts of the islands have very high chemical and salt concentrations. This chemical concentration occurs in thousands of islands. The reason the water is fresh is that trees on the edges of the islands create a barrier of natural filters between the inner part of the islands and the floodplain. The second reason is a process of transpiration caused by trees. Water flows into the delta and carries with it silica and soluble minerals like sodium carbonate. As the water is lost from the trees, the silica and salts remain to build islands. The center of the islands concentrates the accumulated salt and as a result the vegetation dies from dehydration leaving a central bare white mineral spot. Termites facilitate island formation when they build nests of organic material, fungus, soil and water. These mounds of soil and nutrients promote tree and other plant growth.  When the seasonal water rises the termites build skyward forming islands. Eventually the nest is abandoned to form a new colony. The mound then collapses from animal invasion and erosion. Termites are the keystone species of the Okavango. Without them the delta would be like the desert. Water would be lost, and life would be less dense and less diverse.The Okavango has no palm trees and pines are also nearly absent. 

Pond in center of a large island in the Okavango delta. Salt has accumulated in the water causing the trees to dehydrate and die.
Okavango Savana, for centuries built from sedimentation and termite mound building. Trees in the center of the island died from dehydration caused by salt accumulation. Grass is a monocot and is salt tolerant. The termites moved out and the mound is vacant.
Intermittently flooded lowland in the high water season of the Okavango delta
Freely flowing fresh water in a branch of the Okavango river. The plant is Pampas grass (Miscanthus juncos).

The vegetation in Florida also plays an important role. The ocean barrier to salt invasion are mangroves which are salt tolerant. These mangroves are key to prevention of back flow of the salty ocean and hold the soil preventing erosion. Some fresh water flow does reach the ocean creating a relative partial positive pressure. The soils of the Everglades are rich in nitrates and farmers increase the nitrogen of a large portion of the Everglades. This has resulted in an overgrowth of a complex of bacteria species which feeds on the nitrates and deplete the nutrient value of the topsoil. The Everglades have no Acacia trees and lots of mosquitos.

The Kenyan savanna is climatically and geologically very different from the Okavango savanna. Kenya is at the Equator. It is a mile high in altitude and the soil is volcanic in origin. It is more like the area around Denver CO. It is surrounded by hills and mountains and has two rivers flowing through it. The major river flow is the Mara. The other is the Talek. It is part of the Mara-Serengeti ecosystem spanning Tanzania and Kenya and has been geologically very active with ancient and recent rock formations. It is in the Great Rift Valley. It is in this valley that the million-year-old petrified remains of very early hominoids have been found. 

High planes savanna of the Maasai Mara portion of the Serengeti plane. Mt Kenya is on the right horizon.
River cut into the Mara plane providing water to the vegetation and wildlife. This is a spot where the Wildebeests would cross during their migration. They would climb the banks of the river during a stampede. The animals are subject to the risks of death from the crocodiles that ply the river during the crossing.
Igneous rock formation on exposed hill side in the western Mt Kenya highlands.

The plants and animals are widely different in speciation in these three areas but they have similar behavior. This may be the result of adaptation to similar geologic and weather conditions. The apex predators of all locations are big cats. All have eagles, egrets, large carnivorous reptiles and cats and lots of grass.

Human impact:

The effect of the behavior of large numbers of modern people on the Florida ecosystem is dramatically different from the African locations. The Everglades water flow is highly engineered and not necessarily for the best. Southward flow of the Florida delta is interfered by highways and farms to the point that it does not meet the sea as it original did. The Okavango delta also does not meet the sea. In Africa the observed locations have relatively low populations and have been benignly neglected or protected from hunting, industrialization, mining or drilling and farming so that the plants and animals have survived basically unchanged for centuries or even millennia.

Romancing Wild Africa:

We went to see the animal life of Africa and did not go to see the cities, towns, or villages. We did not have much contact with the people of the areas we visited. Africa is a huge, populous, resource rich continent with a history that dates to the origin of most species. There is great wealth and great poverty. Too many people have nothing. They live an impoverished stone age existence in the space age. I acknowledge that many of these are desperately poor and politically persecuted to enslavement and/or death. The NGOs, like CARE, work to help many but must be careful to manage their limited resources. They also try not to support the migrant people in camps to a better level than the local people. The native residents also live by subsistence on gardening, raising a few cattle, contract farm working, tourism, and crafts. Some also engage in a variety of illegal endeavors such as poaching and grazing their animals on park land. You can read the newspapers for details of other antisocial behaviors such as intertribal warfare, abduction, extortion, theft, civil insurrection etc. Desperate people do desperate things.

The wilderness of the savanna of Africa is nothing like anything in eastern US. There is no sense of luxury to the plants or the soil. Much of the topsoil is sand deposited by wind and water. The stark beige color varies little by the source of volcanic mineralization. The organic content is not a rich loam of plant breakdown. It is thin and the organic content is from the sparse droppings from animals or the occasional bush or more rarely from a tree. Animal droppings are recycled by the life on the planes and provide an episodic line of trees from incompletely digested seeds. The brilliant emerald green plants, startling blue sky and the breathtaking color of twilight is such a relief from the monotony.


We will look in greater detail at the findings of this two-week photo expedition in the following blogs. They will focus more on species than locations. 

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#Africa #Okavango #Botswana #Kenya #Everglades #transpiration #Maasai Mara #salt #tectonics #transpiration #evaporation #Tanzania #marsh land #savanna

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