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14 | A NCIENT BONES

The upper jawbone found by a Bavarian soldier in Pikermi and now in the collection of the Bavarian State Collection for Palaeontology and Geology in Munich. It was used by Johann Andreas Wagner in 1839 to document a species he named Mesopithecus pentelicus.

An almost complete skull of Mesopithecus pentelicus THE GREEK ADVENTURE | 17

Detail of bone fragments from Pikermi. Embedded in the fine-grained red sedimentary rock is a chaotic assemblage of bones, primarily from horses, antelopes, and giraffes. 30 | A NCIENT BONES the root tips of the two fuse into a single power- ful root. In many of us, you can tell that the pencil-shaped roots have fused together because there is more than one root canal. The molars of great apes and are not the same shape, because they have different demands made on them when the are chewing. Different diets mean great apes and hominins () have developed differently shaped teeth. (Hominin or Hominini is the term paleoanthro- pologists use for our species and for all our extinct ancestors who lived later than the common ancestor of humans and .)

DiGrafikfferen 1.1-b:ces in Unterschiede DeDifferencesntition an Menschenaffd T ooin thDentition Rooen-Menschts and Toothin Bezahnung Roots

Lower jaw of a modern

Molars

Premolars Human Canines Incisors with a single root

Lower jaw of a

Molars

Premolars Chimpanzee Canines premolar with a Incisors double root 32 | A NCIENT BONES between 5.8 million and 2 million years old. But when exactly had lived?

CT-Scan of the Lower Jawbone of Graecopithecus freybergi

Root canals

Roots

Comparison: Premolar with partially cross section of lower jaw fused roots

p3 p3

p4 p4

m1 m1

m2 m2

m3 m3

SahelanthropusGraecopithecus Inner view Outer view 34 | A NCIENT BONES calcite had formed above the sediment, as they had done in the finds from Pikermi that the Bavarian soldier thought were filled with diamonds back in 1838.

The Earth’s Magnetic Field and the Principles of Paleomagnetism

Earth’s magnetic field Earth's magnetic field showing normal polarity showing reverse polarity Geographic North Pole Geographic North Pole Magnetic Magnetic South North Pole Pole

N S

S N

Magnetic Magnetic South Pole North Pole Geographic South Pole Geographic South Pole

Reverse Normal Pattern Magnetized oceanic crust S N N S

N S S N

Lithosphere

Magma rises and cools. The prevailing direction of the Earth’s magnetic field is encoded in rocks as they form. MAGNETOMETERS AND MICROTOMOGRAPHY | 35

The alignment of the sediment surface gave us the infor- mation we needed to reconstruct the exact orientation of the giraffe bones in the sediment. Using these levels, we could deduce the Earth’s magnetic field at the time the in Pyrgos were deposited.

How a Fossil Level Works

1. Hollow bone 3 cm

Above: Cross-sections of two girae bones from Pyrgos with crystals 2. Bone half-filled with sediment The crystal/sediment boundary marks the and water horizontal level in ancient times.

Left: The formation of the paleo-horizontal line

3. Hardening of the sediment: crystals of calcite form in the hollow space.

We combined the paleomagnetic data from Pyrgos, Pi- kermi, and Azmaka with data harvested from three other chronological techniques. We could then date the Graecopithe- cus fossils and the other Pyrgos finds fairly accurately: they were 7.175 million years old.9 The premolar from Bulgaria 58 | A NCIENT BONES into lesser apes— and siamangs (Hylobatidae)—and great apes (). Great apes include all great apes living today and humans and their extinct ancestors. First, the () split from the lineage leading to , chimpanzees, and humans (). Then the gorillas (Gorillini) split off, and finally, the chimpanzees and (Panini), leaving the human line (Hominini). Over millions of years, early hominins (prehumans) evolved into species of early (early humans), and ultimately into us: Homo sapiens.

The Evolutionary Development and Diversification of Apes and Humans

Gibbons Orangutans Gorillas Bonobos Chimpanzees Humans

Panini Hominini 1.5–2.5 Gorillini 7–13

Ponginae 9–18

Hylobatidae Homininae 13–>20 Hominidae (Great apes)

>20 Time of split in millions years

Hominoidea (Apes)

The search for our roots, therefore, reaches way back into the evolutionary history of . The changes in body shape of the different species, which evolved as they settled in new habitats and adapted to changes in climate, are the cornerstones of human evolutionary history. 64 | A NCIENT BONES stretch of the southern edge of Europe rose as the ocean floor of Tethys slid beneath it, throwing up the European ranges of the , the Apennines, the , the Dinarides, and the Balkans. The Old World, as seafarers called Afro-Eurasia at the beginning of the modern era, was coming together. And in a future only a few million years away from our present, the Mediterranean will eventually disappear completely, buried under new mountain ranges, and a new supercontinent will be formed.

The Paleogeographic Evolution of the Earth

Glaciers Deserts 100 million years ago Vegetation

Eurasia NortNo th AmeAmmerica North Atlantic Pacific

Tethys South Africa AmericA a India South Auststrraalia Atlantic AAntarctica

50 million years ago

North Europe America Asia

North Pacific Atlantic Africa Indiandia Southth America Indian South Ocean Atlantic Australia

Antarctica

14 million years ago

NNorth Europeo Asia America North Atlantic Indiaa Pacific Africa South Ammericme a Indian South Ocean Atlantic AustrA raalil a

Antarcticc a

18,000 years ago (the last glacial period)

Euroopee NortNorth Asia America North Atlantic Africa Pacific South Indian AAmericAm a South Ocean Atlantic AAustustrraalia

AAntarctica

into the future Med North editerr rr NorthNor Atlantic ane an M Eurrasia AmericAmemerica ountauntains Africa South America Pacific

South Atlantic Austrstralia

Antarctica Glaciers Deserts 100 million years ago Vegetation

Eurasia NortNo th AmeAmmerica North Atlantic Pacific

Tethys South Africa AmericA a India South Auststrraalia Atlantic AAntarctica

50 million years ago

North Europe America Asia

North Pacific Atlantic Africa Indiandia Southth America Indian South Ocean Atlantic Australia

AntarcticaAFRICAN BEGINNINGS | 65

14 million years ago

NNorth Europeo Asia America North Atlantic Indiaa Pacific Africa South Ammericme a Indian South Ocean Atlantic AustrA raalil a

Antarcticc a

18,000 years ago (the last glacial period)

Euroopee NortNorth Asia America North Atlantic Africa Pacific South Indian AAmericAm a South Ocean Atlantic AAustustrraalia

AAntarctica

into the future Med North editerr rr NorthNor Atlantic ane an M Eurrasia AmericAmemerica ountauntains Africa South America Pacific

South Atlantic Austrstralia

Antarctica 70 | A NCIENT BONES soil were moved, leading to the discovery of thousands of fossils,28 including three genera of great apes (, , and ) from the middle phase of great ape evolution.29

Paleogeography 10 Million Years Ago and Great Ape Finds

1 Dryopithecus 2 Pierolapithecus 3 Danuvius 4 5 6 3 5 7 1 1 8 Graecopithecus Iberia Paratethys 8 9 7 6 10 Trachilos footprints 1 2 4 Anatolia 8 10 Mediterranean

Africa Arabia

9

Fat Reserves for Lean Times

During the middle phase of great ape evolution, deciduous trees such as and were crowding out their tropical counterparts in many parts of Europe and Asia. At the same time, animals that flourished in the heat, such as crocodiles, snakehead fish, and chameleons, were also disap- pearing. It took time for the apes from Africa to adjust to the new vegetation of Eurasia, and they found themselves fac- ing considerable challenges. For example, unlike in Africa, PROGRESS IN EUROPE | 77

Geological Epochs and Important Genera of Hominoids s ear y

f s ds

h Africa Europe ons o o i oc er Tarantian Milli P Ep y

e Chibanian n e oc

t Calabrian s i e uaternar l

Q Homo Homo P Gelasian olution Piacenzian e d phase n e oc eat ape ev

Pli Zanclian 5 The thir of gr Trachilos footprint Messinian Sahelanthropus Graecopithecus

Ouranopithecus Hispanopithecus Rudapithecus

10 olutio n ond phase of Danuvius eat ape ev gr

e Pierolapithecus The sec

en Dryopithecus g Serravalian Neo e

n Kenyapithecus e oc i M 15 Langhian

Afropithecus olution

Burdigalian eat ape ev

Ekembo The first phase of gr

20

Aquitanian

Paleogene 102 | A NCIENT BONES angle slightly inward so the knees end up directly beneath the body’s center of gravity.

Upright Gait

The human foramen magnum (the hole at the base of the skull through which the spinal cord passes) is centered under the skull. This balances the head more eciently over the neck. The human spine is S-shaped and acts like Great apes need strong neck muscles, because the a spring when we walk foramen magnum is located at the back of the skull upright. above the neck

In humans, the upper ribcage is wide, allowing the shoulder blades to move backward, which frees up the arms.

The human The longer shoulder blades of great thighbone is long apes lie to each side of their narrow and straight. upper ribcage, which makes it easier The knee, when for them to move their arms when they straightened, is are walking on all fours. below the body’s center of gravity.

In great apes, the knee is always bent and oset from the body’s center of gravity. The thighbone is short and curved.

The human pelvis is shallow, wide, and bowl-shaped. The lumbar spine bends, which leads to flexible and strong Humans have a compact walking foot. The back muscles so the upper body can be ball of the foot is pronounced and the big toe held upright. is elongated and aligns with the other toes. The great ape pelvis is long and Tree-climbing great apes have a flexible surrounds the lumbar region. This grasping foot that looks more like a hand with compactness lends stability while a short big toe splayed out to the side. climbing. THE PRIMAL ANCESTOR | 103

Comparison of a Human and Chimpanzee Foot

Chimpanzee Human

Chimpanzee

Human 104 | A NCIENT BONES

There were also profound evolutionary changes in the anatomy of the feet as great apes evolved into humans. Homi- nin feet are no longer appendages used for grasping things. They now facilitate a stable stance on two legs and, even more important, efficient, swift, balanced, forward locomo- tion. In contrast to the big toe of apes, the human big toe is no longer splayed out to the side. It is oriented forward, parallel to the other toes, which are considerably shorter in compari- son. At the base of the enormous big toe, the foot developed a ball, which has a new, extremely important function in the sequence of motion. The big toe, as the last toe in contact with the ground, works in concert with the ball of the foot to propel the body forward.

ChangesChanges in in F ootthe Shape offrom the Gr Footeat FromApe to Great Modern Ape Huma to Humann

5

Footprint of a modern human 4

3

Footprint of a great ape

2 1 The midfoot lengthens. 2 The heel widens. 3 The ball of the foot develops. 4 The big toe aligns with the other toes 1 and increases in size. 5 The second toe lengthens. FOSSIL FOOTPRINTS FROM CRETE | 113 could have been deposited at the mouth of a river. Perhaps the biped followed this river down to the sea. After all, ocean beaches and areas of brackish water offer the promise of plentiful food. Nutritious mussels, snails, and seaweed are there for the taking. All you have to do is bend over and scoop them up.

The Cretan SeaCretan 6 to 7 Million Sea 7 Million Years Ago to 6 Million Years Ago

Aegean

Mediterranean Cretan Sea Trrachilraa os

Coastline of modern Crete

The research results documenting the footprints from Trachilos were published in July 2017, only two months after the scientific paper on Graecopithecus freybergi. For our research group, the results were sensational, because they strongly rattled the cage of accepted thinking that the ear- liest ancestors of humans lived in Africa and nowhere else. The Trachilos find is the oldest direct evidence by far of upright gait. It shows a relatively modern foot anatomy that 122 | A NCIENT BONES detail using state-of-the-art tools at the University of Zurich. Their results were published on July 11, 2002.12 The key mes- sage of those results: The oldest known ancient ancestor of humans came out of North Africa and lived from 7 million to 6 million years ago. It was, therefore, “close to the diver- gence of hominids and chimpanzees.” The scientists named it Sahelanthropus tchadensis. Sahel is a geographic region at the southern edge of the Sahara, so the name translates as “the Sahel human from Chad.” They gave it the nickname Toumaï, which in the local Dazaga language means “hope of life.” The skull from Chad had small canines, a relatively flat face, heavy protuberances over the eye sockets that met in the middle, and medium —all features that sug- gest a humanlike creature.

The collection of bones at the site where Sahelanthropus tchadensis’s skull was found on July 19, 2001. The arrow points to the thighbone belonging to this species. This bone has since disappeared. A SKULL IN THE SAND AND A “SECRET” THIGHBONE | 123

The skull of Sahelanthropus tchadensis after it was cleaned

It was not long, however, before the first critical voices began to make themselves heard. A few months after Sahelanthropus tchadensis was initially described, a Franco- American team led by Milford Wolpoff chimed in with an open letter to Nature.13 The team included Brigitte Senut and Martin Pickford, who had discovered Orrorin tugenensis, which until the paper about Sahelanthropus was published was credited as being the earliest potential hominin. In this letter, the three scientists expressed doubts about how dis- tinctive the skull’s features really were. They argued that the features, although they looked as though they might belong A SKULL IN THE SAND AND A “SECRET” THIGHBONE | 125 the features in question were in no way sufficient to support the analysis, and that the back part of the skull and bone attachments for the neck muscles, in particular, did not fit the anatomy of a biped. Our El Graeco team compared Sahelanthropus tchaden- sis with the somewhat older Graecopithecus freybergi (see the diagram on page 32). We determined that the tooth roots on Toumaï’s lower jaw were much more primitive than El Grae- co’s. The root of Toumaï’s canine was longer and the roots of its two premolars were completely split and not grown together like those of Graecopithecus. These features of the roots also suggest that Sahelanthropus was not an early hominin.

The Nape of the Neck in Great Apes, Sahelanthropus, and Modern Humans

Where the neck musculature attaches to the back of the head in chimpanzees Where the neck musculature attaches to the back of the head in modern humans C Direction of force in the neck musculature of chimpanzees H Direction of force in the neck musculature of modern humans

C H C H

Chimpanzee Sahelanthropus Human

The human angle of attachment for the neck muscles (H) is unlikely for Sahelanthropus, because the angle this would create would be too tight for its neck muscles. The angle of the Sahelanthropus skull is more like that of a chimpanzee (C). FROM EARLY HOMININ TO PREHISTORIC HUMAN | 133 and a specific kind of arm and shoulder musculature that can be reconstructed using the bones that have been found. Based on the specific shape of the joint and pelvis, many experts agree that and others of her species had not yet committed entirely to walking on the ground and still spent at least some of their time up in the trees.26 Other research- ers, however, see no anatomical constraints to walking and running.27

The Hominid Tree e n uta a g l an n m ril ra O Go Chimpanze Hu

Australopithecus ArdipithecusA Ororrinn 5 Trrachilos footprint SahelanthrShS lth opus GrG aecopithecusith

  Ouranopithecusanopithecu Hispanpanopithecusanopithecus 10 Dananuviusnuvius Sivapithecusp us Pierorolapithecusl DryopithecusDry ih Kenyapithnyapiithecust 15 AfrAffropithecus Millions of years Ekembbo 20

25

The Advantages of Walking Upright

Australopithecus afarensis, when mature, had a brain volume of about 450 cubic centimeters. The relationship of its brain 138 | A NCIENT BONES

Great Ape Evolution, Global Climate, and Ecosystems

Glaciers Deserts Glaciers North Europe Asia Vegetation Deserts America North North Europe Asia Vegetation America Atlantic India Pacific North Africa Atlantic India Pacific South Africa America Indian South South Ocean Indian America Atlantic Australia South Ocean Atlantic Australia

First phase Antarctica

First phase Antarctica

ca. 21–14 million years ago Primitive apes arise Globally very humid Forests into the polar in Africa. and warm, 9°F (5°C) regions. Many ca. 21–14 million years ago Primitive apes arise Glwarmerobally verythan humidtoday. Foeverrestsgr eeninto trtheees polar in in Africa. Trandopic warm,al temperatur 9°F (5°C)es Euroregions.pe. First Many deserts inwarmer Europe thanand littl todae y.ic e everbegingr toeen appear trees in Trinopic easternal temperatur Antarcticaes. EuroCentralpe. First Asia. deserts in Europe and little ice begin to appear in in eastern Antarctica. Central Asia.

Europe North Asia America North Europe North Atlantic Asia America North Africa Pacific Atlantic South Africa Indian Pacific America South Ocean South Atlantic Indian Australia America South Ocean Atlantic Australia ond phase Antarctica Sec ond phase Antarctica Sec

ca. 14–7 million years ago Prime time for the Globally very warm, Forests yield to open hominids. They arrived 5.4°F (3°C) warmer than savannahs in many

ca. 14–7 million years ago in PrimeEurasia time and fo evolr theved Gltodaobaly.ly Subt veryro warm,pical Foarreeas.sts Desertsyield to openand hominids.into the grTheyoups arrived we 5.4°Ftemperatur (3°C) warmeres in central than steppessavannahs expand in manyin Asia. knowin Eurasia today: and - evolved latitudes.today. Subt Onlyro easternpical areas. Deserts and intolike, the -lik groups wee, Antatemperaturrctica ises co inmpl centraletely steppes expand in Asia. knowchimpanzee-lik today: orangutan-e, and latitudes.cover edOn inly easternice. thelik earlieste, gorilla-lik hominins.e, Antarctica is completely chimpanzee-like, and covered in ice. the earliest hominins.

Asia North Europe Asia America North Europe North Atlantic America North Africa Pacific Atlantic South Indian Pacific Africa America South Ocean South Atlantic Indian Australia America South Ocean Atlantic Australia

d phase Antarctica Thir d phase Antarctica Great apes died out in Highly variable climate Globally, grasslands Thir Europe and migrated to conditions. Fluctuations (savannahs, steppes) GrAfriceat apesa, wher diede ear outly in betweenHighly variabl warme climateperiods Gleobalxpand.ly, gras Desertsslands ca. 7 million years ago until today Eurhomininsope and flourished. migrated Atto coandnditions. glacial Fluctuations periods. dominate(savannahs, wide steppes) expanses Africa, where early between warm periods expand. Deserts

ca. 7 million years ago until today the beginning of the ice Antarctica and, of the Old World. homininsage, the flourished. first early At incrandeasing glacially, periods.the Arctic dominateAirborne dust wide incr expanseseases. thehumans beginning appear of theed atic e complAntaetelrcyti frcae ezeand, ove r. 5.5 millionof the Old years Wo ago,rld. the almostage, the e firstxactl eary thely increasingly, the Arctic AirborneMediterranean dust incr driedeases. up. humanssame time appear in bothed at completely freeze over. 5.5 million years ago, the Africalmosta and exactl Eurasia.y the Mediterranean dried up. same time in both Africa and Eurasia. Glaciers Deserts North Europe Asia Vegetation America North Atlantic India Pacific Africa South America Indian South Ocean Atlantic Australia

First phase Antarctica

ca. 21–14 million years ago Primitive apes arise Globally very humid Forests into the polar in Africa. and warm, 9°F (5°C) regions. Many warmer than today. evergreen trees in Tropical temperatures Europe. First deserts in Europe and little ice begin to appear in in eastern Antarctica. Central Asia.

Europe North Asia America North Atlantic Africa Pacific South Indian America South Ocean Atlantic Australia ond phase Antarctica Sec

ca. 14–7 million years ago Prime time for the Globally very warm, Forests yield to open hominids. They arrived 5.4°F (3°C) warmer than savannahs in many in Eurasia and evolved today. Subtropical areas. Deserts and into the groups we temperatures in central steppes expand in Asia. know today: orangutan- latitudes. Only eastern like, gorilla-like, Antarctica is completely chimpanzee-like, and covered in ice. the earliestFROM hominins. EARLY HOMININ TO PREHISTORIC HUMAN | 139

Asia North Europe America North Atlantic Pacific Africa South Indian America South Ocean Atlantic Australia

d phase Antarctica Thir Great apes died out in Highly variable climate Globally, grasslands Europe and migrated to conditions. Fluctuations (savannahs, steppes) Africa, where early between warm periods expand. Deserts ca. 7 million years ago until today hominins flourished. At and glacial periods. dominate wide expanses the beginning of the ice Antarctica and, of the Old World. age, the first early increasingly, the Arctic Airborne dust increases. humans appeared at completely freeze over. 5.5 million years ago, the almost exactly the Mediterranean dried up. same time in both Africa and Eurasia.

Out of Africa?

The finds of what appear to be early hominins in Europe, finds that fit with the timeline of savannahs appearing in Europe, clearly contradict the assumption that Africa is the cradle of humanity. In the 1980s, the idea that the human evolutionary line arose in Africa and that humans spread out all over the world from there was labeled the Out of Africa theory. The name comes courtesy of Günther Bräuer, a long- time professor of at the University of Hamburg, who was inspired by a film based on Karen Blixen’s memoir, Out of Africa. Today, proponents of this theory propose that there were two chronologically and geographically distinct migrations: Out of Africa I describes the spread of early humans more FROM EARLY HOMININ TO PREHISTORIC HUMAN | 147 and excavations can give us only fleeting snapshots of the time and place where these species lived. It is only when you have a large number of these fleeting moments that you can assemble the snapshots into an album that makes sense of the whole.

Oldowan Stone Tools and Acheulean Handaxes Oldowan Stone Tools and Acheulean Handaxes

Oldowan stone tools ca 2.6 million years old

Acheulean handaxes ca. 1.76 million years old 168 | A NCIENT BONES

Mediterranean, where they deposit about 7 ounces of dust from the desert per 100 square feet per year (20 grams per square meter). This makes dust from the Sahara one of the most important components of the red-colored soil in this region.12 Were conditions similar 7 million years ago?

Deep deposits of Saharan dust at Pikermi, , with an embedded layer of gravel indicating a stream bed

I began to doubt that the red sediments in the Basin were deposits from lakes and rivers when I visited the site of the dig at Pikermi in 2014. Closer inspection of the material of which the red rock was composed revealed that although the particles were fine, they were not fine enough to be lake sediments. Geologists in the field develop a good feel for the grain size in sediments. Here is the rule of thumb: If you cannot see the grain with a magnifying glass and the 172 | A NCIENT BONES particles to fragments visible to the naked eye. They are proof that in the dry phases, fires swept through this landscape on a regular basis, another feature typical of savannahs.

The Geology of

Parnitha

Triasson Basin Attic Divide Pendeli Poikilo PyrP rgos VaVasilissis Mountains

Egaleo Pikermi Athensns Basinsin AcrAc opolisopolliis

Mesogea Basin Mountains

Saronic Gulf Limestone Schist 3 mi (5 km) Marble and gneiss

The animals we met on our journey back in time also belong in this landscape and are the ones for which the site at Pikermi has been famous for almost two hundred years. They are strikingly similar to the modern-day inhabitants of the African savannah. The resemblance is so strong that one of the first people to dig at Pikermi, Albert Gaudry, spe- cifically compared the two.21 The results of our research 186 | A NCIENT BONES

Geologists detected the first traces of this extreme geolog- ical phase in the early 1970s. They were using the research vessel Glomar Challenger to drill deep into the bottom of the when, completely unexpectedly, they came across massive layers of salt.43 It was unexpected because salt usually dissolves in seawater and does not accu- mulate on the bottom of the sea. That is, unless the water evaporates so quickly that crystals form in the brine. Many researchers have been working on this discovery since then, but it has only been in the last ten years that they have devel- oped a better idea of what exactly might have led to the salinity crisis.44 So, what were the forces of nature that almost wiped out the Mediterranean at the end of the ?

The Messinian Salinity Crisis

The Mediterranean region in the Miocene, ca. 7 million years ago

Iberia

Mediterranean

Atlantic Africa

Deeper water Deepest water

1. 2.2.2 Iberia Iberia

Betic Corridor Strait of Strait of Mediterranean Gibraltar ? Gibraltar Mediterranean Atlantic Atlantic Rifian Corridor Africa Africa

3.3 Iberia 4.4.4 Iberia

Strait of Strait of Gibraltar Gibraltar Mediterranean Mediterranean

Atlantic Atlantic

Africa Africa

Dotted lines indicate modern coastlines. Arrows represent currents. 1. Late Tortonian ca. 7 million 2. Early Messinian ca. 6.3 million years ago years ago Two straits (corridors) connect the The Betic Corridor dries out. Atlantic and the Mediterranean. Water continues to flow through the Rifian Corridor.

3. Late Messinian ca. 5.6 million 4. Zanclean ca. 5.3 million years ago years ago The Rifian Corridor also closes. The Strait of Gibraltar is now the only connection between the Atlantic and the Mediterranean.

Isolated salty seas remain after the Mediterranean dries up, ca. 5.5 million years ago.

Atlantic

Iberia

Africa The Mediterranean region in the Miocene, ca. 7 million years ago

Iberia

Mediterranean

Atlantic Africa

Deeper water A GRAY-WHITE DESERT AND A SALTY SEA | 187 Deepest water

1. 2.2.2 Iberia Iberia

Betic Corridor Strait of Strait of Mediterranean Gibraltar ? Gibraltar Mediterranean Atlantic Atlantic Rifian Corridor Africa Africa

3.3 Iberia 4.4.4 Iberia

Strait of Strait of Gibraltar Gibraltar Mediterranean Mediterranean

Atlantic Atlantic

Africa Africa

Dotted lines indicate modern coastlines. Arrows represent currents. 1. Late Tortonian ca. 7 million 2. Early Messinian ca. 6.3 million years ago years ago Two straits (corridors) connect the The Betic Corridor dries out. Atlantic and the Mediterranean. Water continues to flow through the Rifian Corridor.

3. Late Messinian ca. 5.6 million 4. Zanclean ca. 5.3 million years ago years ago The Rifian Corridor also closes. The Strait of Gibraltar is now the only connection between the Atlantic and the Mediterranean.

Isolated salty seas remain after the Mediterranean dries up, ca. 5.5 million years ago.

Atlantic

Iberia

Africa 214 | A NCIENT BONES are considerably thicker than those of modern humans. The same could be said for the build of the shoulders, which look most like those of .24 The Hobbit’s arms are even longer than those of other early hominins and early humans, which makes it seem more apelike. had especially large feet, which was rather fitting, given its nickname. The Hobbit’s feet are, amazingly, 70 percent as long as its thigh. To put that in per- spective, modern humans’ feet are half as long as our thighs. A Homo floresiensis that stood 5 feet 7 inches (1.7 meters) tall would have had feet that were 12.6 inches (32 centimeters) long. That corresponds with a size 16 (European size 50) in shoes. People who wear shoes this large today are usually over 6 feet (2 meters) tall. With feet this size, Homo floresien- sis must have had to lift its legs higher than we do when it walked, and it could certainly not run nearly as fast as mod- ern humans. Yet, if you look at its teeth, tooth roots, and jaw shape, there are similarities once again with Australopithe- cus and other primitive early humans, such as those found at the world-renowned site of Dmanisi in Georgia that are still revealing their secrets today. All in all, the Hobbit appears to be a mosaic of numerous other finds from Africa and Eurasia.

The skeleton of LB1, Homo floresiensis, also known as the Hobbit WANDERLUST | 223

Africa. This second interpretation is in accord with finds of tools in India and China that have been dated to 2.6 million years ago, and with the almost 2.5-million-year-old “mystery ape” from the Yangtze River, Homo wushanensis. In this lat- ter scenario, Homo floresiensis would not even have been an especially small hominin, because many early hominins and early humans stood no more than 3 feet (1 meter) tall. That is the case for Lucy, for example, and also for whomever left the footprints in Crete. Small stature, up to only 5 feet (1.5 meters), is a characteristic of all early hominins. It was only with Homo erectus, 1.7 million years ago, that humans grew to be more than 6 feet (1.7 meters) tall.40

The Wallace Line and the Distribution of Extinct Species of Humans

LLuzLuuzzoono Homo luzonensis

Sundaland Philippineshilippin (e.g., Eurasian fauna

deer Direc the Austtion of (2.4–2.8 inches/6–7 cm per ye , pigs, and travel of fauna nd ralian una plate Borneo etc.) ar) Sumamatrmatatra Sulawesiawesi New Guinea Homo floresiensis Homo erectus

na Wallace Line una roughflow ond) lian faunapial Th Sahula ShelSh upialsupif )  per sec Austr marsup m Indonesian(4,000 US gallons/ (e.g., 300 mi (500 km) 15 million Australia A CONFUSING COMPLEXITY | 267 survived without them for years.4 It is impossible to imagine how this old man would have managed to stay alive over 1.8 million years ago without a social support network. Ethno- logical studies have shown that Indigenous people in similar situations are fed food chewed by other members of their group, an act that strengthens the resilience of seniors and demonstrates that the helpers possess a high level of social competence and a sense of empathy—a behavior that is truly human.

The skull of the early human Homo georgicus from Dmanisi, Georgia An artistic rendition by Velizar Simeonovski of Danuvius guggenmosi in its habitat The lower jawbone of Graecopithecus freybergi from Pyrgos Vasilissis Amalias above photographs of the premolar from Azmaka taken from various angles

The happy discoverer of Danuvius guggenmosi’s lower jawbone, May 17, 2016 → Reconstruction of the facial skull belonging to Udo, a male example of Danuvius guggenmosi

↓ Important bones from Udo, Danuvius guggenmosi (upper jaw, lower jaw, vertebrae, elbow, shin, thigh) The Foot of a Great Ape Compared With a Human Foot and a Footprint From Trachilos

Great ape Modern human Trachilos print

Analyzing the Footprint From Trachilos

Toes Footprint

BBaBalalllo of Displaced thet fooott sediment Adhering sediment

HeeHee l The left footprint from a human in sand compared to the left footprint of a chimpanzee in clay

The Grasping Foot of Ardipithecus ramidus

Upright gait, but big toe splayed to the side Homo neanderthalensis Danuvius guggenmosi, Udo

17 Ouranopithecus macedoniensis 18 1 Homo heidel- Graecopithecus bergensis freybergi, El Graeco

14 12 Homo 2 antecessor 3 5 Trachilos footprint

4 6 8 Sahelanthropus tchadensis, 9 10 Toumaï 11 13

10

Australopithecus africanus

7

Millions of years -20 -13 -10 -7 -6 -5 -4 -3

1 Danuvius guggenmosi, Udo Ardipithecus Australopithecus afr icanus ramidus 2 6 Ouranopithecus macedoniensis Australopithecus afarensis Graecopithecus 3 8 freybergi, El Graeco Orrorin tugenensis aethiopic us Sahelanthropus 4 tchadensis Paranth ropus boisei Ardipithecus kadabba Trachilos footprint 5 Australo pithecus robustus Ho mo habilis HOMINIDAE HOMININI GREAT APES EARLY HOMININS AUSTRALOPITHE CINES

Chimpanzees (Panini, 7–13 Ma) Gorillas (Gorillini , 9–18 Ma) Orangutans (Ponginae, 13–20 Ma) 16

Homo georgicus

Australopithecus Ardipithecus afarensis, Lucy ramidus, Ardi

Homo floresiensis, the Hobbit

9 Paranthropus aethiopicus

13 11 Paranthropus boisei 15

10 Homo habilis

Homo erectus

13

-3 -2 -1 Today

Australopithecus afr icanus 18 7 Homo neanderthalensis 17 Australopithecus afarensis Homo ergaster / erectus 13 Homo sapiens

Paranthropus aethiopic us 9 12 Homo georgicus Homo floresiensis 15

Paranth ropus boisei 11 Denisovans Australo pithecus robustus 16 Ho mo habilis 10 14 AUSTRALOPITHE CINES EARLY HOMO AND EARLY HUMANS MODERN HUMANS

Bonobos A reconstruction of El Graeco’s habitat. Although we do not really know what Graecopithecus freybergi looked like, the reconstruction of the landscape El Graeco inhabited is based on scientific data. Visible in the background are the limestone ranges of the Lycabettos and the Acropolis, along with giraffes (Bohlinia), elephants (Anancus), gazelles, Hipparion-horses, and a rhinoceros. Clouds heavy with dust from the Sahara darken the sky.