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Last
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|
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]](African Lakes & Rivers_files/lake chad 1973.jpg)
|

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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
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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. |
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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
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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. |
|

Barbus bynni bynni |

Mormyrus kannume
|

Alestes baremoze
|
|

Clarias gariepinus
|

Heterotis niloticus
|

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. |
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 |
|