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Last updated: 08 May 2006

Seashore Foraging & Fishing Study

Early Human Diet

African Lakes & Rivers

De Heinzelin's Map

The main catchment areas and drainage channels of the African continent have existed for an immense length of time. Except in the extreme north‑west (Atlas Mountains) and south (Cape Mountains) the continental crust has been little affected, at least for many millions of years, by the horizontal or orogenic compressions which have folded up the world's major mountain ranges (Himalayas, Alps, Andes and Rockies). Its surface has been shaped mainly by spasmodic earth movements (tectonics) in a vertical direction ‑ uplifting, faulting, subsidence and volcanic outpourings, as well as by the continuous forces of erosion. The presence of marine sediments dating from the Cretaceous (some 100 million years ago) show that much of what is now the Sahara, Ethiopia and Somalia was then inundated by the sea. But the rest of the continent has remained above sea‑level since the Precambrian, more than 600 million years ago, though large areas have from time to time been covered by lakes or swamps, most of which have now disappeared.

Uplifting and subsidence have moulded the surface to a pattern of large depressions separated by ridges (basins and swells), and it is this pattern which has determined the outlines of Africa's hydrology. Most of the basins which are the main catchment areas, now drain into the sea through gaps in their rims, via Zaire, Niger, Nile, Zambezi and Orange Rivers. Some are 'closed' and have no outlet. Lake Chad, which during part of the Pleistocene was larger than any of the world's present existing lakes, has no surface outlet, but seeps into the sandy soils to the northeast, rises to the surfaces by capillarity, evaporates and deposits salts. The lake thus remains fresh through the basin is 'closed'.

Though some of the northern edges of the Cubango and Kalahari basins in Angola and Botswana are drained by the Zambezi, the water of most of these areas finds no permanent outlet and collects in the swamps of the Okavango Delta and in the saltpans of the Makgadikgadi basin.

Leonard C. Beadle, The Inland waters of tropical Africa, 2nd ed., Longman Group, 1981. Chapter 3, Pages 20 to 25

But the outstanding point about de Heinzelin's map is the very stability (apart from the Great Rift Valley, that noisy, bumptious recent entrant to the stability of East Africa) of the African drainage basins, most of which are in exactly the same areas they occupied 25Mya, although many of them have now broken through to the sea as the great rivers of Africa (Niger, Congo, Zambesi, Nile, Orange).

Of course, those rivers haven't 'broken through' at all. It's not as if there was a great river, pent-up and trying to get out. What really happened was that a tiny trickle on the sea side of the basin quietly eroded, bit by little bit, under its stream bed, and back through the barrier, until it backed, perhaps reluctantly, into the basin's regular seasonal flood, and let a little bit out, which next year, became a little bit more, and so on.... 

And, just so, the nil became the Nile.

The alternating glacial/pluvial cycles of just the last 10% of that 25 My time (2.5My) have seen the waxing and waning of these great drainage basins.

Lake Chad is now a mere smear of the great lake or inland sea it was until a mere 6000ya.

[a Landsat image]

January 1973, Landsat 1 MSS bands 4 2 1

January 1987, Landsat 5 MSS bands 4 2 1

Indeed, it's disappearing before our very eyes.  I have changed the colour of the actual water surface to make the disaster more obvious, for disaster it is, both for the local micro-climate, and for the local people.

Chad is not suffering from massive over-extraction, for irrigation, of incoming river waters, like the similarly afflicted Aral Sea in Kazakhstan, so its shrinkage must largely be from natural causes. The Sahel area went through a very dry climate cycle, during the early 80s, that led to widespread famine.

Sure enough, though, by such a huge lake area, Toumäi, one of the very earliest hominid fossils, has recently been found there, and Australopithecus bahrelghazali, from somewhat later (about 3My) was also found nearby.

Remember, from Beadle, The Inland waters of tropical Africa (above): "Lake Chad, which during part of the Pleistocene was larger than any of the world's present existing lakes, has no surface outlet, but seeps into the sandy soils to the northeast...

Colonel Gaddafi of Libya is, right now, draining the underground waters of the Fezzan basin, with his 'Great Man-Made River Project'. The Fezzan basin is NE of Lake Chad. Perhaps the crafty old devil is sucking it all away.

Much the same type of ancient lake system applies to the now arid Arabian Peninsula, although, to my knowledge, no maps like de Heinzelin's have been produced for that area. Certainly, there were pluvial-period lakes or playas scattered about throughout the majority of the Pleistocene, during the development stages of Early Humans.

North-west of Riyadh, they're mining old water for irrigation. Huge circular fields, constantly watered by rotating hose lines, must be producing the world's most expensive vegetables.

Acheulian handaxes and other evidence of the presence of Homo erectus can be found, even by a casual tourist like me, scattered on the surface all over what are now searingly hot and dry salt flats.

Jordan has two well-known sites, Azraq (once Lawrence of Arabia's HQ), that still has scattered ponds, and is a major stopover for migratory water birds, and Jafr, now in the heart of the desert. Further south, the stored underground fossil waters of yet another great Pleistocene lake are now being mined to sustain the growing city of Amman. They won't get much more of it when it's done for.

Extensive East African Lakes

By examining soil layers at seven sites throughout East Africa, (Dr Martin Trauth of the University of Potsdam and his team) were able to identify three distinct periods during which extensive lakes covered the region and grew to depths of hundreds of metres.

They argue that the growth of these lakes resulted from a moist local climate. The regional wet periods, which may have persisted for up to 100,000 years, occurred as much of Africa became increasingly dry.

The periods of wet weather in East Africa might reflect fluctuations of the Earth's climate as a whole. At the time when the lakes grew - roughly 2.6, 1.8, and 1 million years ago - glaciers and the atmosphere were also going through major transformations.

Climate change marks dawn of man

Those three 'rough' dates: 2.6, 1.8, and 1 million years ago, are very significant in Early Human history

- 2.6 Mya - Emergence of Homo habilis - first human and first tools in Ethiopia

- 1.8 Mya - Emergence of Homo Erectus

- 1 Mya - Emergence of first 'archaic Homo'

Now ain't that a coincidence?

Freshwater or sea, the origin of humankind was deeply reliant on the shorelines of large bodies of water, and you can take your pick of the entire eastern coastline of Africa, no less than a dozen great primeval African drainage basins, or even the latecomers, the great lakes of the Rift Valley itself.

Algis Kuliukas, a leading scholar of the Aquatic Ape Theory, favours the saltpans of the Makgadikgadi basin as the site where bipedalism, the first hominid 'marker' began. Marc Verhaegen prefers a rather earlier time period with aquarboreal Miocene apes, while many adherents to the theory, including its main proponent, Elaine Morgan, prefer island isolation on a continental block fragment, the Danakil Alps, once, and often, cut off from the mainland by the onetime Afar Sea.

The 'Shoreline Diet' group (Broadhurst, Cunnane, Crawford, et al) have probably the strongest circumstancial evidence of all of early hominids' reliance on shoreline foods, but play it safe by plumping for Rift Valley lakes.

With his Delta Hypothesis, Richard Wrangham is now coming round to a new perspective:

- and has picked one of the proposed drainage basins that de Heinzelin proposed for pre-Rift Valley Africa, the Okavango 'delta', as as an example of the 'divergence site' of humans from apes.

Wrangham says:

If the first hominin evolved from a chimpanzee-like species, it could in theory have done so in the rainforest or in the savanna. Here I follow the conventional assumption that hominins began in the savanna. Accordingly, the old question, about how savanna apes became savanna hominins, has been replaced by a new problem: how did forest apes become savanna hominins? Specifically, how and why did the earliest hominins colonize the savanna, given that they came from a knuckle-walking, fruit-eating chimpanzee-like ape that depended on rainforest?

The proposal in this paper is that the LCA (the last common ancestor of Homo and Pan) must have relied initially on a chimpanzee-like diet in its new habitat.

The Okavango delta, I suggest, provides a suitable model for a transitional habitat between rainforest and other savanna habitats, because:

1) it is a (rare) example of a savanna region containing year-round access to foods that would be edible by chimpanzees, and providing sources of safety from predators;

2) such a habitat allows easy allopatric speciation, such as would be expected if chimpanzees were currently introduced to the Okavango delta; and

3) it is sufficiently large to allow a viable population.

The Delta Hypothesis: Hominoid Ecology and Hominin Origins - Richard W. Wrangham 2005 (PDF on internet?)

And then steps hesitantly into the Rubicon...

Water-crossings would doubtless have been ... alarming for the LCA: chimpanzees do not normally like to enter water. Under some circumstances, however, chimpanzees may spontaneously wade bipedally in water up to 1m deep (Gabon, C. M. Hladik personal communication; Congo, M. Ancrenaz personal communication). If the LCA were able to wade like chimpanzees, they would have been able to negotiate the waters of the Okavango delta at least as well as baboons. They would also have been able to reach Nymphaea stems growing more than an arm’s reach from the bank. Facultative bipedal wading would therefore have been a useful adaptation for the LCA occupying an inland delta.

Wrangham 2005

But others have also dipped their toes in the Rubicon:

‘One of the strong points about the aquatic theory is in explaining the origin of bipedality. If our ancestors did go into the water, that would forced them to walk upright’. Stringer, 1997

For example Verhaegen et al. (2002) suggested that hominin ancestors “fed partly on hardshelled fruits and molluscs”, on the basis of evidence such as dental similarities to mollusc-eating sea otters (Enhydra lutra), the human capacity for voluntary breath control, and the expectation that bipedalism would be associated with wading. They considered that the ancestor of australopiths could have come from a Miocene ape ancestral to chimpanzees and gorillas, so they did not expect the LCA to be chimpanzee-like.

It wasn't Marc Verhaegen who first suggested that a human's teeth were remarkably like those of a sea otter, but Alan Walker, very much a 'savannah' man. 'This species possesses small anterior teeth, and large, flat molars with thick enamel'.

 

As noted by Verhaegen et al. (2002) and many other authors, fossil hominins are frequently associated with wet habitats, doubtless partly a taphonomic bias*.

Wrangham 2005

 

(*That is, you find dead bones in wet places, because mud's a good medium for preservation. But then, you find stone tools in wet places, too. Mud does nothing very much for them).

 

Kathy Schick points out that "the majority of known Acheulean sites from anywhere in the world are found in fluvial contexts

Kathy Schick An Examination of Kalambo Falls Acheulean Site B5 from a Geoarchaeological Perspective. In Kalambo Falls Prehistoric Site Vol III The Earlier Cultures: Middle and Earlier Stone Age. edited by J. Desmond Clark. Cambridge: Cambridge University Press 2001. Pp. 463-480.

 

This scenario also raises the possibility that the composition of the Okavango as a network of islands could favor the evolution of bipedalism. For those who envisage bipedalism as facilitated by the need to traverse or exploit aquatic environments, an inland delta that generates low islands termitogenically¹ or hydrodynamically² offers rich scenarios.

The Delta Hypothesis: Hominoid Ecology and Hominin Origins - Richard W. Wrangham 2005 (PDF on internet?)

(¹ ² - ie, made by termites or by running water)

Harrummph!!

Sounds a bit like old Dick is going down that barmy 'Wet Ape Theory' path!

Although he does it circumspectly, by ritually invoking the Holy Assumption that Hominins Began in the Savanna. He's not quite ready to be an iconoclast yet.

That sort of thing is only allowed for the really Grand Old Men of palaeoanthropology, like Philip Tobias.

Philip Tobias's Repudiation of the Savannah Hypothesis

"My disavowal of SH was based in the first place on evidence which had been coming forth from excavations in South and East Africa. From Sterkfontein, suggestions of greater woodland cover at the time when Australopithecus was deposited in Member 4, had emerged from studies on fossil pollen, but these were not compelling. Then Wits team member Marian Bamford identified fossil vines or lianas of Dichapetalum in the same Member 4: such vines hang from forest trees and would not be expected in open savannah. The team at Makapansgat found floral and faunal evidence that the layers containing Australopithecus reflected forest or forest margin conditions. From Hadar, in Ethiopia, where "Lucy" was found, and from Aramis in Ethiopia, where Tim White's team found Ardipithecus ramidus, possibly the oldest hominid ever discovered, well-wooded and even forested conditions were inferred from the fauna accompanying the hominid fossils.

All the fossil evidence adds up to the small-brained, bipedal hominids of four to 2.5 million years ago having lived in a woodland or forest niche, not savannah. The evidence for the presence of big forest trees supports the idea we had gleaned from the bones of "Little Foot" that tree-climbing had been a part of the lifeways of these early African hominids. At least, one could conclude, there had been trees big enough to bear the weight of the Australopithecines (for which stunted acacias of the savannah would have been unsuitable).

To a large London audience in 1995 I said: "All the former savannah supporters (including myself) must now swallow our earlier words in the light of the new results from the early hominid deposits... Of course, if savannah is eliminated as a primary cause, or selective advantage of bipedalism, then we are back to square one."

Humans are not savannah-adapted animals

In rejecting the SH, I was moved primarily by the evidence unearthed in South Africa and East Africa. Meanwhile, Elaine Morgan had been piecing together a number of other arguments against the SH, based on some anatomical, biochemical and physiological data of modern humans, much of which was collected by Belgium's Dr Marc Verhaegen, which contrast sharply with the traits in present-day animals that are truly adapted to savannah life.

As examples, modern humans lack sun-reflecting fur and are virtually hairless. The cooling system in our skin is quite unfit for hot, dry, exposed environments: we have numerous sweat glands and we waste water and sodium - not very suitable for life on the savannah. Our ability to concentrate our urine is poor and too low and if ever our earliest ancestors were savannah dwellers, we must have been the worst, the most profligate urinators there.

Adapted savannah-dwellers need to drink more water at a time, but most humans are not able to drink much at a time. The quantity of our subcutaneous fat, which would insulate us against heat loss, is never found in truly savannah-adapted animals.

In our bodily functions, chemistry and microscopical anatomy, we should be hopeless as savannah-dwellers. So Marc Verhaegen and Elaine Morgan, in her remarkable book, The Scars of Evolution, came to the same conclusion that we had reached from quite different lines of evidence: the old Savannah Hypothesis was not tenable. All former savannah supporters must recant ­ and this I did in London. It was an exciting moment - living through a change of paradigm.

Max Planck, the German physicist and Nobel laureate, once wrote these words on the replacement of an outworn paradigm: "A new scientific truth does not triumph by convincing its opponents and making them see the light, but rather because its opponents eventually die, and a new generation grows that is familiar with it."

That must be one of the masterpieces of cynicism on the scientific process. Paradigm changes, I like to think, flow overwhelmingly from new evidence and, where the evidence is sound and even irresistible, they should be embraced just as lief by the old as by the young. It was three weeks after my 70th birthday and I went on to declare, "A change of paradigm shakes us up; it rejuvenates us; and, this above all, it prevents mental fossilisation - and that is good for all of us."

Philip Tobias

De Heinzelin's Map

Lake Chad

Extensive East African Lakes

Delta Hypothesis

Philip Tobias's Repudiation

East African Climate

Where were human fossils found ?

African Lake and River 'Seafood'

African freshwater fish

African freshwater shellfish

African freshwater flora

Conclusions

 

 

 

East African Climate

Three million years ago the Northern hemisphere climate was generally warmer, with sea levels at least 25 m higher than present levels. The most significant warming was in the high latitudes.

Equatorial East Africa was actually cooler than at present, but was wetter (Dowsett et al. 1994), and had evergreen forests (Bonnefille et al. 1987).

 

Major Climate Change 2.5 to 2 million years ago

From 2.5 to 2 million years ago, coincident with the onset of major northern hemisphere glaciation (mostly growth of polar ice caps), the climate became cooler and drier (Shackelton et al. 1984; Versteegh et al. 1996).

The environment was more similar to that of the present (Bonnefille, 1983), but was not yet dominated by savanna grassland (Cerling, 1992).

 

There was a mosaic of forest, bush, savanna and patchy wooded grassland, with a general trend towards a more open, arid, grassland-dominated environment (Vrba et al. 1995).

Mammalian generic diversity remained high and relatively unchanged, but guilds deepened (a guild being a group of closely related but distinct species that have very similar ecological requirements and also occur together in particular habitats; deepening of a guild indicating that the number of species in the guild is generally increasing), and some extant genera appeared for the first time (Harris 1993; Vrba et a1. 1995; including especially grazers such as Equus and Oryx (horse, oryx), camivore-omnivores such as Vulpes and Ichneumia (fox, mongoose), and the browser Loxodonta adaurora (modern elephant)).

Homo was one of these new genera, appearing in East African deposits dating to 2.3-2.5 million years ago, and South African deposits dating to approximately two million years ago (Conroy, 1990; Wood, 1993; Foley, 1994; Schwarz et al. 1994; Johansen & Edgar, 1996). Also approximately 2.3 to 2 million years ago, the gracile Australopithecines A. africanus and A. aethiopicus were replaced by the robust species A. robustus and A. boisei. Robust australopithecines coexisted with H. habilis, and later H. erectus, for over one million years, so there must have been subtle ecological differences between genera (Conroy 1990; Wood, 1992; Johansen & Edgar, 1996).

Rift Valley lake fish and shellfish provided brain-specific nutrition for early Homo
C. Leigh Broadhurst, Stephen C. Cunnane and Michael A. Crawford
British Journal of Nutrition (1998), 79, 3-21

But fluctuated wildly between pluvial (wet) and interpluvial (dry) periods

Serious study of past climates in tropical Africa, as revealed in exposed alluvial and lake sediments and raised beaches with their fossils and human artifacts, was begun in the 1920s. This led to the formulation by L. S. B. Leakey of a climatic scheme for the Pleistocene in sub‑Saharan Africa, based on work in East Africa, involving a series of alternating pluvial (wet) and interpluvial (dry) periods ....related to glacial and interglacial periods in the northern hemisphere. There were certainly great climatic fluctuations during the Pleistocene, especially in rainfall, but more recent research has disclosed a number of difficulties in the way of finding a universal timetable of climatic events applicable to the whole of tropical Africa. A popular account of East African prehistory, based on the pluvial‑interpluvial climate scheme, is to be found in Coles (1954). 

Leonard C. Beadle, The Inland waters of tropical Africa, 2nd ed., Longman Group, 1981. Chapter 3, Pages 20 to 25

Since Leakey's time, some doubt has been cast on the coincidence of tropical pluvial periods and northern glaciation, but, very roughly, in East Africa, at least, they correspond, more or less.

Where were human fossils found ?

Homo erectus at Olorgesailie - by Maurice Wilson, who made wonderful watercolours of primitive humans out for an amble.

Compare this style with the French one at:

Skull & Bones Club

and then tell me that palaeoanthropologists aren't nationalistic

East African sites are associated with watercourses, mostly ancient lake margins, but also riverine forests. Every site contains both sedimentary and igneous strata which record continual uplift, faulting, and volcanic activity (Baker et al. 1972; Dawson, 1992; Sikes, 1994). The Miocene to Pleistocene lakes were typically 10 000- 100 000 km2 in area.

Numerous hominid fossils have been recovered in Ethiopia (e.g. Hadar and Omo River), Kenya (e.g. Lake Turkana Basin) and Tanzania (e.g. Olduvai and Laetoli). H. habilis and H. erectus have been found at Omo, Turkana and Olduvai. (Fossils from Koobi Fora, Turkana, classified as H. habilis may represent another species H. rudolfensis, but this is not generally accepted (Wood, 1993).)

Hadar was mainly a marshy lake margin with rivers flowing in from the Ethiopian escarpment; Paleo Lake Hadar periodically filled the whole basin. However, there was a mosaic of microenvironments, including bush, grassland and wooded areas.

Omo River had both riverine fluvial environments and swampy lakes. Allia Bay records evidence of the proto-Omo river system flowing into the Turkana basin, with bordering gallery forest (Bonnefille et al. 1987; Leakey et al. 1995; Vrba et al. 1995).

Turkana was an enormous (> 15000 km’) lake basin with wide marshy lake margins, and extensive mud flats which were covered with grasses in the dry season. Lake levels fluctuated significantly during the Plio-Pleistocene and Lake Turkana was a closed, alkaline lake for at least part of the time (Abell, 1982).

Olduvai was also on the margins of a fluctuating lake, probably with no outlet. The perennial lake was alkaline and saline, but there was periodic flooding of the lake basin. Alluvial-fan and plain deposits are also present, indicating significant sedimentation derived from continual Rift fault uplift and associated river downcutting (Leakey, 1971, 1979; Plummer & Bishop, 1994; Behrensmeyer et al. 1995).

 

And the earliest known fish dinner was found there. It is not known whether Early Humans used crude choppers or bifacial handaxes to process the chips. Newspaper wrapping was unknown at the time.

See: Where is the Evidence?

Laetoli (exceptionally) was more arid, upland savanna, not necessarily near a permanent water course (Leakey & Harris, 1987; Andrews, 1989; Cerling, 1992).

Localities under development include Manoga Valley, Tanzania (Harrison, 1994), and Semliki Valley, Zaire (Boaz et al. 1994) both of which were also large lake basins.

Chad - At 2500 km west of the Rift Valley, A. afarensis fossils (actually A. bahrelghazi) dating to 3 to 3-4 million years have been found in Chad (Brunet et al. 1995). The paleoenvironment was also lakeside, with both perennial and permanent streams and a mosaic of gallery forest, wooded savanna, and open grassland.  

Behrensmeyer (1975) was one of the first to propose that H. habilis may have been more restricted ecologically to the lake margin than was A. boisei. At Turkana, Behrensmeyer (1975) assigned eighty-four hominids to major depositional environments, thirty-nine to fluvial, and forty-five to lake-margin deposits. A. boisei was more abundant in fluvial environments, while H. habilis was rare there. Both are represented in comparable numbers in lake- margin environments; however A. boisei fossils are more common than Homo in both channel and flood-plain deposits. The fluvial channels were probably bordered with gallery forest, as is the case today, while the lake margins had wide mudflats, swampy in the rainy season and grass- covered in the dry season.

Rift Valley lake fish and shellfish provided brain-specific nutrition for early Homo
C. Leigh Broadhurst, Stephen C. Cunnane and Michael A. Crawford
British Journal of Nutrition (1998), 79, 3-21


Olorgesailie - "Aha, I said, drawing it to the attention of the expatriate cousin.  We are, I announced, in the midst of another former lake bed. Lakes shrink and expand as droughts come and go, so shorelines migrate.  There’s another kind of change, too:  most shallow lakes silt up eventually, if something doesn’t pull the plug before then. 

We’re on our way to visit Olorgesailie, which is right on the edge of a basin that held a lake until it lost part of its rim to earth settling.  About a million years ago, it contained Lake Olorgesailie (a quite large freshwater lake, over a hundred km2, now vanished).

Olorgesailie shows the Acheulian toolkit that appeared about 1.8 million years ago.  It didn’t change very much for a million years thereafter.  In toolmaking, there didn’t seem to be any steady progress, contrary to our “Man the Toolmaker” expectations of what drove things.  The initial toolkit seen about 2.6 million years ago in Ethiopia had no more than a half-dozen tool types, and the Acheulian toolkit has no more than a dozen.  But in contrast to what came earlier, the Acheulian toolkit has at least one tool that looks “designed” (though for what isn’t clear)."

William H. Calvin, A Brain for All Seasons

Rick Potts, who's been digging Olorgesailie since the year dot, but still has strange ideas about 1Mya Homo erectus coming down to the lakeside for food, and commuting back to the hills for safety at night, has a very interesting site diary at:

Meet Our Expedition Team

This layer was formed when the lake that filled the basin dried up abruptly and completely. Above and below this layer are layers of diatomite, showing the presence of a large, fresh-water lake in the valley. Animals that relied on the lake would have had a hard time when it disappeared, and would have either died off or simply migrated away from Olorgesailie. But then, later, as the lake returned, a new grouping of species would have repopulated the area.

Rick Potts - Olorgesailie 23 July 2004

A lake than can leave layers as thick as that is a lake is a lake is a lake, not a savannah.

Earlier hominoid finds

Consider the 3.9–4.2 Mya beds at Lothagam, an Australopithecus anamensis site from Kenya, for example, or the 2.5 Mya Hata member of the Bouri formation, an Australopithecus garhi site from Awash, Ethiopia. Both sites have a mixture of terrestrial and aquatic elements, and have therefore been reconstructed as paleolakes or lake margins (de Heinzelin et al. 1999, Walker 2002).

Take Brunet et al.’s (2002) finds of Sahelanthropus tchadensis in northern Chad from six to seven million years ago, which are particularly relevant to considering the adaptation of the LCA to savannas. Vignaud et al. (2002) described the paleoecology as including gallery forest and savanna together with numerous aquatic elements, and therefore suggested that S. tchadensis lived close to a lake.

The Delta Hypothesis: Hominoid Ecology and Hominin Origins - Richard W. Wrangham 2005 (PDF on internet?)

Two early hominid species were even named after the wet places where they were found:

Australopithecus anamensis - from Anam  - local Turkana word for 'lake

Australopithecus bahrelghazali - from Bahr el Ghazal - Arabic for 'Sea of the Gazelles'

A  longer and more detailed list of  26 early hominid sites related to water (again with the sole exception of Laetoli) is given in:

Hominid Lifestyle and Diet Reconsidered  Marc Verhaegen, Pierre-François Puech

Human Evolution 15, 151-162, 2000

The standard Skull & Bones Club   answer to this is 'taphonomic bias'. So recall:

"That is, you find dead bones in wet places, because mud's a good medium for preservation. But then, you find stone tools in wet places, too. Mud does nothing very much for them".

African Lake and River 'Seafood'

Erlandson points out:

...the almost daily need for drinking water tethered our ancestors to aquatic habitats for most of human history.

...it seems unlikely that hominid hydrophobia would have prevented similar opportunistic harvesting of shallow water fauna by some of our earliest ancestors living along the shores of African lakes. With general similarities between many of the animals (fish, shellfish, birds, etc.) that live in lakes, rivers, estuaries, and marine habitats, it also seems unlikely that a significant learning curve would have been required to transfer such skills between aquatic habitats. Erlandson

African Lake & River Fish

African lakes and rivers have an abundance of sizeable fish and shellfish, in contrast to the somewhat impoverished freshwater fauna of North American and European ones.

Africa's lakes and rivers have certainly waxed and waned  over the past few million years, but they've stayed in more or less the same positions, and they haven't been scoured clean by glaciers or sudden glacial meltwaters.

True, Africa's fresh waters lack salmon, trout and sturgeon, but you can't have everything.

The fish shown below come from Lake Turkana, right beside the famous archaeological site of Koobi Fora.

tn_Babyn_u0.jpg

Barbus bynni bynni

tn_Mokan_u0.jpg


Mormyrus kannume 

tn_Albar_u0.jpg


Alestes baremoze

tn_Clgar_u1.jpg

 


Clarias gariepinus

tn_Henil_u1.jpg

 


Heterotis niloticus

tn_Maele_j0.jpg


Malapterurus electricus

African freshwater shellfish are very like their marine cousins

Photos from: http://members.aol.com/Mkohl2/Afropleuros.html and http://members.aol.com/savetheclams/AfroUnios.html


Iridina (Cameronia) spekei
LakeTanganyika

American Unionid cousins of these have largely disappeared - over-hunted for freshwater pearls.


Etheria eliptica.
Throughout Congo Basin, but only in rapids. Widely used by native peoples for food, and as a source of lime by early Belgian settlers.

 


Egeria Congica
Large heavy triangular clams may grow to over 120 mm in size.


Parreysia bakeri Lake Albert

French marine cousins of these are known as 'Praires', much sought after by gourmets who know their shellfish.

When Stanley met Livingstone, in the darkest heart of Africa, they probably shared a couple of dozen Congo oysters.


Spekia zonata  


Potadoma alutacea
 


Potadoma alutacea
 


Pachymelania aurita

A common or garden winkle. A fiddly little appetiser.

Close cousins of these three live in my local Philippines mangroves, 6000 miles away from Africa. I don't find them very tasty, but I still get offered quarts of  them every other day, always with the tips knocked off, just like the ones above. You have to blow through the tips to push the shellfish out of the other end. I suspect the collector of these never went near the lake swamps, but got them from a native who'd eaten them.

African Lake & River Flora

I'm not going to say too much about African lake algae (seaweeds) because I know sweet FA about them, and I somehow suspect no one else really knows very much either. But I could quite imagine some Kenyan lakeside villager sitting down, about now, enjoying a fresh, delicious salad of lato, or guso, or whatever Lake Bongo-bongo yields.

See: Philippine Caviare

 

Corms and roots from sedges and rushes, such as papyrus, would be much easier to harvest from a muddy substrate than from hard dry earth, like their terrestrial cousins.

Gorillas are particularly fond of them.

 

Lew Binford, whose analysis of early hominids at Olduvai Gorge turned them from mighty hunters into marginal scavengers, has only a slightly higher view of their Middle Paleolithic descendants. The main staple of the Neandertals at Combe Grenal, according to Binford, was not flesh at all. Judging from the traces of pollen left on flake tools at the site, it was aquatic plants plucked from the canyon stream. Cattails, to be exact.

The Neandertal Enigma - James Shreeve

It's very possible that the flake tools at the site were not used primarily for meat processing at all, but for stripping the furry heads of cattails (bulrushes), that would make fine bedding material.

Richard Wrangham is also very much in favour of aquatic or aquatic-margin foods:

The LCA would have required daily access to a class of preferred foods that would have been dominated by ripe fruits, but could also include honey, meat, social insects and immature seeds. It would also have required daily access to a class of fallback foods that would have included soft leaves (herbaceous or arboreal) and herbaceous piths.

1)      Dietary composition can be usefully dissected into preferred and fallback foods (e.g., Lambert et al. 2004) Fallback foods, i.e., abundant items that are not preferred but are acceptable when ripe fruits cannot be found.

2)      Great Apes smaller than gorillas require both preferred and fallback foods (e.g., Yamagiwa 1999)..

Isolated in the delta, they would be forced to survive on a restricted range of fruit, leaf and pith species...such as the superabundant Cyperus papyrus and Nymphaea spp.

Okavango tree species producing fleshy fruit is low (about 20 species) (but) the availability of ripe fruits is high for all or most of the year. The period of highest food availability appears to be the time of highest rainfall, when the majority of baboon conceptions occur (Cheney et al. 2004). But even during three months with no rainfall in one year (June–August) the ground was well watered, trees continued producing fruit, and baboons ate fruits and seeds from 11 species of woody plants (Hamilton et al. 1976). This prolonged availability of fleshy fruit at high density may be unique in a 'savanna' environment.

...several species that are so high in quality that they are also harvested enthusiastically and eaten raw by people, notably Diospyros mespiliformis, Garcinia livingstonei (“African mangosteen”), Phoenix reclinata (wild dates), and various Grewia species. The Okavango also has figs that are eaten by chimpanzees (Ficus verruculosa, Ficus natalensis, and Ficus sycamorus), and fruit-producing species in genera that in forest regions are eaten by chimpanzees (e.g., Syzigium cordatum).

Wrangham 2005

Lotus Eaters?
The roots of Okavango’s Nymphaea nouchali provide human food during times of scarcity and can be eaten either cooked or raw. People obtain them either by reaching or by wading into the water. The work is easy because a pull on the stems dislodges the root from the soft mud. People can likewise eat the leaves of Nymphaea spp. raw, and Nymphaea stems provide major fallback foods for four river tribes in the Okavango

Wrangham 2005

Wrangham avoids the problem of progressing to other forms of aquatic food, very simply:

Verhaegen et al. (2002) suggested that hominin ancestors “fed partly on hardshelled fruits and molluscs”, on the basis of evidence such as dental similarities to mollusc-eating sea otters (Enhydra lutra) ... such proposals are incomplete unless they can explain how the posited foods can be found in sufficient abundance all year.

Molluscs and fish are available throughout the year, and fish are especially 'fat' at the end of the dry season, as they spawn and are caught more easily during the very first rains, when other foods may not be available.

See: Olduvai Fish

Then goes on to say:

In my own experience, savanna lakes sustain few or no trees that produce year round fruits edible by primates (e.g., Rift Valley lakes in Kenya and Tanzania). This raises the possibility that for fruit-eating hominins lake margins would normally have been impoverished habitats unless they included deltaic areas receiving year-round water.

All the more reason to try fish and molluscs.

Then he gets on his favourite hobby-horse, USOs:

It would then presumably rapidly evolve in the direction of a hominin diet by incorporating underground storage organs. Appropriate changes in teeth and guts would follow. This scenario conforms to the fact that the molars of Sahelanthropus are rounder and have thicker enamel than those of chimpanzees, suggesting a greater use of underground storage organs (Brunet et al. 2002). (Or molluscs)

Be thankful for small mercies - at least he's not saying they'd off across the savannah to bag a brace of bucks with their bifacials.

The Delta Hypothesis: Hominoid Ecology and Hominin Origins - Richard W. Wrangham 2005 (PDF on internet?)

Conclusions

I don't subscribe to the convention that humanity necessarily developed in close proximity to the classic fossil sites of the East African Rift Valley, just because so many of them have been found there, although I have no hard, incontrovertible evidence to show that they didn't.

Although they certainly seem to have been messing around in Chad.

see: Why are so many early human fossils found in East Africa?

or even that Homo habilis and Homo erectus originated there.

My reason? - the missing essential mineral ingredients of the diet: Iodine, iron, copper, zinc and selenium for human brain development and maintenance, only available in any useful quantities from a sea shoreline diet. Without these, and particularly iodine, intellectual capacities can be reduced by an overall average of about 15%, or endemic cretinism may be prevalent throughout the population. Fat chance of growing clever Early Humans.

see: Iodine - The Missing Ingredient

Kenya, especially the interior of the country, is one of the world's most notorious iodine-deficient territories.

To be fair, this may be due to the majority of poor Kenyan subsistence farmers eating a modern, post-agricultural (and post-Columban) diet rich in cassava, maize, and other goitrogenic grains that positively inhibit iodine absorption

or it may be due to the usual dire shortage of such minerals far inland from the sea shore.

It may well be that the African Rift Valley lakes, subjected to continuous volcanic and tectonic disturbances, with regular flooding and desiccation cycles, themselves generate and concentrate such essential minerals in their edible fauna and flora, but, so far as I know, no one has studied or demonstrated this.

For that reason, I tend to favour the

Indo-Pacific Shoreline Ecotone

as the theatre where our ancestors developed their humanity.

New Pages as at May 2006

Skull & Bones Club  Oldest Beads Were Sea Shells
Brain Development The Indo-Pacific Shoreline Ecotone
Fats & The Brain 1 - Why DHA matters African Lakes & Rivers
Fats & The Brain 2 - Born Fat Shoreline Mammals
Iodine - Missing Ingredient Shoreline Reptiles
Iodine - Evolution's Catalyst Shoreline Diet - Evidence?
Coconut Origins Shell Middens & Fish Bones
'Eco-Friendly' Poisons Insects as Food
Two unfortunate experiences of Filipino culture:
Perfectly Normal Burglary Fishing Expedition

  Back to Coconut Studio Index Page

 

Richard Parker  - Siargao Island - April 2006  (Last updated Monday, May 08, 2006)  

 

I welcome comments or corrections on my site and opinions, so please feel free to email me at:  richardparker01@yahoo.com