THE LEAKEYS AND THEIR DISCOVERIES AT OLDUPAI GORGE, TANZANIA.

THE LEAKEYS AND THEIR DISCOVERIES AT OLDUPAI GORGE, TANZANIA.

Featured image: The camp of Louis and Mary Leakey at Oldupai Gorge, Tanzania, 1965.

To the casual eye, Oldupai Gorge, in Tanzania’s Ngorongoro Conservation Area, seems much like any other network of scrub-littered ravines draining (whenever it rains) dry rangeland areas in the world. However, it stands out from the rest in being a special place, a UNESCO World Heritage Site yielding up artifacts invaluable to understanding early human evolution.

Oldupai Gorge (David Bygott)

(David Bygott & Jeannette Hanby)

Oldupai Gorge’s fame reflects its unique geological history:

  • Basalt flows from Ngorongoro’s Crater Highlands which flooded the area almost two million years ago.
  • The subsequent, intermittent formation of shallow alkaline lakes attractive to a rich diversity of animals, apes and early humans (Lakebed clays aided in fossilizing their remains).
  • Periodic volcanic eruptions in the nearby Crater Highlands which added successive layers of ash that helped preserve animal and hominid remains.*
  • Geologically recent earth movements which tilted the Oldupai area, creating the stream that cut the ( up to 90 meter / 295 ft deep) Oldupai Gorge, exposing an orderly sequence of nearly two million years of layered deposits containing animal, pre-human, and human artifacts.

* Hominid–Family of erect, bipedal primates including humans together with extinct ancestral and related forms and the gorillas, chimp, bonobo and orangutan.

In this way, Nature first created, and then exposed, a treasure trove of artifacts illustrating human evolutionary history.

All that was needed now was for someone to piece that history together.

Layered deposits exposed by erosion in Oldupai Gorge.

(David Bygott)

The volcanic ash comprising most of the layered deposits in the gorge came from once active volcanoes in the Ngorongoro Crater Highlands (background).

Enter Louis and Mary Leakey. Born in Kenya to missionary parents, Cambridge-educated Louis was raised among the Kikuyu, whose language he spoke and about whom he later wrote a book. For her part, Mary, despite receiving only a sporadic education, already was a woman pioneer in the fields of archaeology and paleoanthropology. Their complimentary skills, hers in excavating artifacts and his in interpreting and publicizing them, made them an effective husband-wife team.

Mary and Louis Leakey

(Smithsonian Institution Archives. Accession 90-105, Science Service Records, Image no. SIA 2008-5175)

Beginning in 1931, the Leakeys spent most of their professional careers excavating Oldupai Gorge’s layered deposits, from the lowest and oldest (1,750,000 years) to the highest and youngest (present day).

Time sequence of depositional beds at Oldupai Gorge related to environment and human evolution.

(Jeannette Hanby & David Bygott: 1992. Ngorongoro Conservation Area Guidebook. David Bygott & Co)

Their first major find, in 1959, was a large, robust ape, which Louis Leakey classified as Zinjanthropus boisei (Later classified as Australopithecus boisei, and then reclassified as Paranthropus boisei). He initially considered it to be a direct ancestor of humans because it walked upright and was found with an abundance of faunal remains and rudimentary stone tools (so named because the stones chosen already resembled the final product and were simply altered by chipping off a few flakes). Its massive teeth (for which it was nicknamed Nutcracker Man) implied a diet of coarse plant material.

It was a welcome discovery for the Leakeys who up to this point had, whenever Louis could find enough funds to support their work, spent 28 years at Oldupai uncovering animal fossils and crude stone tools. Zinjanthropus, however, caught the world’s attention, enabling Louis to secure proper long-term financial support–from the National Geographic Society.

A reconstruction of Zinjanthropus boisei (now Paranthropus boisei)

(Cicero Moraes and Dr. Moacir Elias Santos. Attribution-Share Alike 4.0 International License.)

But then in 1960, remains of another hominid species, discovered by Mary and her son, John, came to light. Similar in age to Zinjanthropus boisei but smaller in stature, it had smaller teeth and a larger brain, which at 600 cc was 100 cc larger than Zinjanthropus’s. This changed Louis’s mind–Here was the real direct ancestor of man, one more likely to have used stone tools. Louis named the new find, Homo habilis. Handy man.

A reconstruction of Homo habilis.

(Cicero Moraes. C.C. Attribution-Share Alike 4.0 International License.)

Still largely ape-like, H. habilis remained partially arboreal (long arms) but ate more meat (implied by its smaller teeth) than apes, and probably scavenged and hunted smaller animals, while still eating lots of plants.

A chopper associated with Zinjanthropus (Australopithecus / Paranthropus) boisei and Homo habilis remains at Oldupai Gorge.

(Picasa. CCO 1.0 Universal Public Domain Dedication.)

Louis’s and Mary’s announcement that they had found a new species of early human provoked controversy as many experts thought they had too little evidence to support such an important conclusion. Only in the 1980’s, following Richard Leakey’s discovery, in 1972, of Homo habilis remains on the shores of Kenya’s Lake Turkana, did the scientific community fully accept that Homo habilis was a true human ancestor.

Richard, one of three Leakey children. Still young when this picture was taken in 1965, he was to become a noted paleoanthropologist in his own right.

The Leakey’s later excavation of Homo erectus (Upright Man) remains in higher level, 0.7 – 1.2 million-year-old, deposits in the gorge, created less of a stir because remains of H. erectus already had been discovered elsewhere (Java in 1892 and China in 1927). Nonetheless, finding H. erectus , Paranthropus boisei, and H. habilis, as well as 17,000-year-old artifacts of H. sapiens (Modern Man) at Oldupai made it possible to demonstrate the full sequence of human evolution at a single site.

Reconstruction of Homo erectus. Upright Man.

(Cicero Moraes. C.C. Attribution-Share Alike 4.0 International License)

At 950 cc, H. erectus had a larger brain than H. habilis. Upright Man also used more sophisticated stone tools, including hand axes and cleavers, had a more modern gait and body proportions (flat face, prominent nose) and sparse body hair, carried out coordinated hunting of medium-large animals (bovines-elephants) and possibly was the first human ancestor to use fire, have a proto-language, and practice monogamy (as inferred from males and females being similar in size). H. erectus also was the first human ancestor to spread from Africa into Eurasia.

Stone tool hand axe used by Homo erectus.

(Loctus Borg. C.C. Attribution-Share Alike 4.0 International License.)

Stone Age Homo sapiens, represented by the 17,000 year-old remains excavated at Oldupai Gorge, used stone tools tools characterized by microliths, which are smaller, finer, and sharper than stone tools made by H. erectus. They include spear points and arrow heads. Microliths were advanced technology in their day because they were portable as well as easier to make than the hafts of spears and bows. Thus, when a spear point broke it could be easily replaced without having to make a new haft.

Microliths.

(Birmingham Museums Trust. C.C. A. 2.0 Generic License.)

SUMMARY

From the early 1930’s until Mary died in 1996 (Louis died in 1972), the Leakeys were responsible for most of the stone tool and hominid fossil discoveries at Oldupai Gorge (and Laetoli). These discoveries, which were major contributions to understanding human evolution, proved that:

  • Humans were far older than previously believed
  • Human evolution centered in Africa rather than Asia, as earlier discoveries had suggested
  • The earliest humans coexisted with a species of ape which, like them, walked upright.

They also demonstrated the relationship between the evolving features (especially brain size) of increasingly modern species of humans and the sophistication and frequency of use of stone tools.

Louis and Mary Leakey worked at Oldupai Gorge for 41 and 65 years respectively. It was time well spent.

REFERENCES

Bygott, D. 1992. Ngorongoro Conservation Area Guidebook. Tanzania Printers Ltd.

Leakeyfoundation.org.

Ward, C.V. & A.S. Hammond. 2016. Australopithecus and kin. Nature Education Knowledge 7(3)1.

Wikipedia: (a) Richard Leakey, (b) Microliths, (c) Paranthropus, (d) Aistralopithecine, (e) Oldupai Gorge, (f) Homo habilis, (g) Homo erectus.

NGORONGORO SCENERY

NGORONGORO SCENERY

Tanganyika, East Africa. 1964.

Man, it was cold! Dense fog had formed during the night to wrap my little house on the rim of Ngorongoro Crater in a silent, gauzy blindfold. Peering through the window, I shivered, something I hadn’t expected to do so close to the equator. But then I also hadn’t expected to be living at 7,000 ft elevation ( 2,134 m). On the other hand, a fire in the fireplace was beginning to making its presence felt. Pulling up a chair to huddle near its warmth, I reviewed what I had learned from my first staff meeting as the Ngorongoro Conservation Area’s new assistant conservator (forests).

Ngorongoro’s forests and crater rim are often cold and foggy during the wet and early dry seasons. Photo by David Bygott.

Wearing a sweater to ward off the cool morning air, Henry Fosbrooke, conservator of the Ngorongoro Conservation Area, addressed the assembled officers from behind his sturdy African olive-wood desk. He confirmed that I was to oversee a large forest reserve, ten forest guards, a tree nursery, and a small fuelwood plantation of eucalyptus trees. He emphasized the need to stop livestock trespassing in the forest reserve, but he also wanted me to locate game-viewing tracks for tourists in and around Ngorongoro Crater. Then, he said something I hadn’t expected. Pausing to wipe his glasses, Henry admitted that neither activity would be possible until he obtained more vehicle fuel and a bulldozer. In the meantime I was to take over the conservation area’s rain gauge system and set up a meteorological station near the office. Also, I was informed, Richard Leakey had ordered a lorry load of bamboo for the archeological site at Oldupai Gorge; buffaloes had broken the fence around the tree plantation again; and I needed to familiarize myself with the files in my office. After the meeting, John Goddard, a Canadian wildlife biologist, and my neighbor, invited me to accompany him into the crater while he studied rhinos. Checking the fog again through the window, I decided I was in little danger of being bored. I also decided to borrow a heavy sweater from John.

In fact, I was never to be bored for long at Ngorongoro, especially when my official duties expanded to take me throughout the entire Ngorongoro Conservation Area. And, what a place it was, too!

A relief map of the Ngorongoro Conservation Area. Yellow (grassland), gray (bushland and woodland), green (forest), and brown (agriculture). Courtesy of David Bygott and Jeannette Hanby (more about them later).

Bracketed by three rift valley lakes, Manyara, Eyasi, and Natron, the Ngorongoro Conservation Area, at 3,200 sq. miles (8,300 sq. k), is nearly as large as Yellowstone National Park, which it rivals in scenic appeal and biological diversity (both are UNESCO World Heritage Sites). And how could it not what with the high peaks, plateau, and volcanic calderas of the Crater Highlands in the east, the vast sweep of the world-famous Serengeti Plains in the west, and, in the southwest, Lake Eyasi and the rugged Eyasi Escarpment (not to mention extensive areas of thorn tree bushland and woodland).

For instance:

Zebra and wildebeest on the floor of Ngorongoro Crater. At 2,000 ft (609 m) deep and 100 sq. miles (260 sq. km) in area, the crater, home to 25,000 large animals, and one of Africa’s densest populations of lions, is considered one of the seven natural wonders of Africa.
(Don’t know them? Check out https://www.worldatlas.com/articles/the-seven-natural-wonders-of-africa-unique-and-mesmerizing-travel-destinations.html.)
Empakaai Crater dramatically backdropped by Oldoinyo Lengai, an active volcano rising from the rift valley floor. At 10,700 ft (3,200 m) elevation and 980 ft (300 m) deep, Empakaai is highly scenic. Views from the crater rim often include Mt. Kilimanjaro 90 miles (145 km) to the east.
The Melinda grasslands, a high plateau (including the Embulbul Depression) in the rain shadow of >11,000 ft (3353 m) Loolmalison and Olosirwa mtns. The trails reflect many millennia of use by wildlife and, for at the least the last 2,000 years, livestock of a succession of pastoral peoples. The area is now grazed by Maasai livestock. The distant peak is Oldeani Mountain.
Composed of numerous species, including bamboo on Oldeani Mtn., montane evergreen forest is sustained by high rainfall, primarily on the southern and eastern flanks of the Crater Highlands. It is a major habitat for rhino, buffalo, and elephant. The pictured tree is a species of Dracaena.
Thorn tree woodland on the drier, west slope of the Crater Highlands. The dominant tree here is a species of Commiphora. This is giraffe and impala country. The eastern Serengeti Plains are visible in the distance.
Migratory wildebeest on the eastern Serengeti Plains. During my time at Ngorongoro (1964-67), approximately 400,000 wildebeest moved onto the eastern plains every wet season to graze and calve, only returning to the Serengeti National Park when the grass and water dried up. (In 1980 they numbered around 1,400,000.)
The Eyasi Escarpment rising 1300 ft (400 m) above Lake Eyasi (barely visible at far left). Shallow Lake Eyasi fluctuates widely in area both seasonally and annually. Flamingoes and waterbirds visit the lake. Agriculturalists, Hadza hunter-gatherers, and Datoga pastoralists use the adjacent semi-arid thorn bush flats.

Pretty cool, eh?

(The authors/artists Jeannette Hanby and David Bygott lived for nineteen years in Mangola Village near Lake Eyasi’s eastern shore just a few miles east of the area pictured above. Their books, Spirited Oasis: Tales from a Tanzanian Village, and Beyond the Oasis: Safaris of Song and Stone, relate their experiences during this time. Check them out at https://www.youtube.com/watch?v=MU1L-sZJs8Q; David and Jeannette tell a good story.)

(For more information on the present-day Ngorongoro Conservation Area see https://www.ncaa.go.tz/

ON THE ROAD TO NGORONGORO: PART II

ON THE ROAD TO NGORONGORO: PART II

“What a view!” I yelped before snapping another photo. “Mmm, yes,” murmured Henry who had seen it many times before. While driving from Arusha to Ngorongoro we had topped the escarpment overlooking Lake Manyara (Fig. 1) and been confronted by an eye-grabbing view—steep, two to three thousand ft slopes fronting Lake Manyara and the Maasai Steppe like the ramparts of an immense fortress (Fig. 2). Wow!

Figure 1. Map of the Crater Highlands area. The Great Rift Escarpment passes west of Lake Manyara, east of the Crater Highlands (Loolmalassin Mts., Olmoti Crater etc.) and west of Lake Natron.
Figure 2. View south over Lake Manyara and along the Great Rift Escarpment. The Lake Manyara Hotel swimming pool is in the foreground.

However, I would have been even more impressed had I known this was only a small part of one of the geologic wonders of the world, a system of separate but related rift basins, composed of escarpments, and troughs some 30-40 miles wide, stretching 3,700 miles all the way from Turkey to Mozambique (Fig. 3).

Figure 3. The Great Rift Valley includes the Dead Sea and the Sea of Galilee. In Africa, it cuts through the highlands of Ethiopia before dividing into the Albertine Rift and the Eastern or Gregory Rift. Lake Manyara is in the latter. (Author: Redogeographica. Creative Commons Attribution-Share Alike 4.0 International license.)

And, it’s all caused by the earth’s crust pulling apart. In Eastern Africa, the Somali Tectonic Plate, which lies east of the Eastern or Gregory Rift (Fig. 3) is splitting away from the larger African or Nubian Plate causing huge chunks of land to sink between parallel faults (Fig. 4).

Figure 4. Parts of the rift system are not distinct valleys (Graben) but, as at lake Manyara, a single escarpment (Footwall) rising above a shallow depression (Half-Graben). (Author: Aymaith 2. Creative Common Attribution-Share Alike 3.0 Unoported License)

Geologists postulate that elevated heat flow from the earth’s mantle is causing “thermal bulges,” creating the highlands of Kenya and Ethiopia. As they form, these “bulges” stretch and fracture into a series of faults forming rift valleys. Huge chunks of land sinking between parallel fault lines force up molten rock in volcanic eruptions. Consequently, the East African Rift System (EARS), especially the Eastern or Gregory Rift, tends to be geologically active with numerous volcanoes, hot springs, geysers and earthquakes (Figs. 5 & 6).

Figure 5. Geyser at Lake Bogoria, Kenya.

The geological processes driving the formation of the East African Rift System have greatly benefited the region. For instance, rift basins with steep 2000-3,000 ft (600-900 m) escarpments, solitary volcanoes, including Kilimanjaro and Meru, and 7,000-12,000 ft (2,134-3,658 m) volcanic highlands, provide a scenic and biological diversity that otherwise would not exist (Figs. 6&7). A rough measure of this diversity is the number of Kenyan and Tanzanian national parks (16) found in areas affected by rifting and volcanism.

Figure 6. Empakaai Crater (Embargi Crater in Fig. 1), an extinct, 10,569 ft. volcano in the Crater Highlands. Beyond, Kerimasi, another inactive volcano, rises from the arid rift floor where dry season dust devils swirl among leafless thorn trees. In contrast, temperatures at Empakaai Crater are lower, rainfall higher, and morning fogs drench evergreen forests and perennial grasslands.
Figure 7. Shallow lakes typical of the Eastern Rift are well known for their flamingoes. Lake Makat, Ngorongoro Crater.

In addition, highly fertile volcanic soils support dense populations of agriculturists, as on the well-watered slopes of Mt. Kenya and Mt. Kilimanjaro (see Mt. Kilimanjaro post). Livestock productivity of rangelands occurring on volcanic soils is up to twice (or sometime more) of that on soils derived from other geological materials.

Yet another benefit is that steam from hot springs and geysers can be harnessed to create geothermal energy. In 2015, geothermal energy generated nearly half of Kenya’s electricity (Fig. 8). And, it’s green energy, too!

Figure 8. Geothermal power station at Olkaria, near Lake Naivasha, Kenya.

Then, there’s this: The East African Rift System may even have influenced human evolution. Discovery of so many remains of early hominids within the rift (Fig. 9) has led to the idea that the processes of formation of the East African Rift System (uplifts of land thousands of feet in elevation, volcanoes spewing ash into the atmosphere, extensive lava flows . . . ) may have caused frequent alternations between wet and dry periods, thereby influencing the evolution of the human species by forcing our ancestors to adapt by becoming smarter and bipedal.

And, here I’d thought it was all about the scenery.

Figure 9. Oldupai Gorge, Ngorongoro Conservation Area, Tanzania. The concrete block marks the site where the remains of an early hominid species, Zinjanthropus boisei (since renamed Paranthropus boisei) were discovered in 1959.