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Maltese Medical History
THE
INFLUENCE OF NEOLITHIC MAN ON MALTESE ENVIRONMENT
C. Savona-Ventura
The first known traces of man in Malta may
date from approximately
15000 years ago when Palaeolithic man followed the deer herd migration
south as a result of the advancing ice on the continent. At this stage
in his culture, man had a very limited effect of his surrounding
environment. Definite changes to the environment were only felt when
man learned to cultivate the fields and husband animals in the
Neolithic phase of his culture.
Definite evidence of Neolithic man on the Islands dates to about 7000
years ago. Excavations at Ghar Dalam and Skorba have shown that the
first colonisers were people at a Neolithic level of cultural
development: they were able to make stone implements, knew the art of
pottery making and lived by farming. Very little is known about the
vegetation of the Islands before the advent of man. Quaternary deposits
have indicated remains of the tree species Laurus nobilis
(Laurel) and Pinus halepensis
(Aleppio pine) [Zammit Maempel, 1977/1982]. The quaternary snail
species population excavated from the deposit at Mellieha (Malta)
suggest that the climate during the quaternary period was a
Mediterranean one similar to that prevailing today. The presence of the
calciphile snail species Orcula doliolum, now extinct on the
Islands, suggests that the climate was slightly more moist than the
present day [Thake, 1985].
Analysis of carbonized wood and seeds excavated from
Scorba - a
neolithic site datable to the Ghar Dalam phase (5200-4500 BC) - have
confirmed that the in the early Neolithic period the islands had tree
species like Cercis siliquastrum (Judas tree), Crataegus sp.
(Hawthorn) and Fraxinus sp. (Ash) [Metcalfe, 1966]. Two species
of wild plants Sherardia arvensis (Field Madder) and Scorpiurus
sp.
(Caterpillar plant) were also identified. The former may have been used
to extract dye [Helbaek, 1966], while many of the other species have
medicinal properties [Lanfranco, 1992].
The Early Neolithic farmers probably had a relatively simple
agriculture utilizing a system of shifting agriculture in which land
was roughly cleared of vegetation, cultivated for a few years and then
abandoned. Carbonized seed analysis have confirmed that Early Neolithic
man cultivated barley, wheat, leguminous plants - Lens esculenta
(Lentil of Neolithic Anatolian type), two types of wheat - Triticum
dicoccum (Emmer wheat) and Triticum compactum (Club wheat),
and a hulled variety of barley [Helbaek, 1966].
Early Neolithic man also intentionally and unintentionally introduced a
number of animal species to the Islands. He brought with him a number
of domesticated animal species including pigs, sheep and goats. He also
domesticated cattle. At Skorba with its Early - Late Neolithic phases,
cattle bones seemed to be more frequent in the deposits of the earlier
phases, though overall the commonest bones recovered belonged to goats
and sheep [Gandert, 1966]. The reason for the change in animal
husbandry is related to grazing patterns of the various species. Goats
and sheep, unlike cattle, graze very close to the ground thus requiring
poorer grazing grounds. In addition Early Neolithic man introduced the
two rat species (Rattus rattus and rattus norvegicus),
the House Mouse (Mus musculus), the Algerian Hedgehog (Erinaceus
algirus),
besides domesticated dogs and cats [Storch, 1970; Boessneck and Kuver,
1970]. Excavations at the Xemxija Tombs, dated to the beginning of the
Late Neolithic Period (the Temple Culture period), have revealed a
large number of bones belonging to a variety of domesticated and wild
animal species [Pike, 1971].
XEMXIJA TOMBS ANIMAL REMAINS
DOMESTICATED ANIMALS
1. Sheep/Goat: large range of sizes, biggest approximating the
modern Mediterranean sheep.
2. Bos sp.: Bone numbers less common than those of the
sheep/goat. Size smaller than those of modern Mediterranean cattle.
3. Pig: Not a large species
4. Horse: Size comparable to those of the Dartmoor pony.
5. Dog: Size of a small terrier.
6. Cat: Size smaller than those of the modern domestic cat. Cat
bones commoner than bones of dog.
WILD ANIMALS
1. Deer: Deer were common during the
Pliestocene period being excavated from a number of sites. They
apparently were existant even during the Early Neolithic Phase, but
became eventually extinct because of hunting and loss of habitat.
2. Rabbit: may have been introduced by man as food.
3. Rat
4. Hedgehog: may have been introduced by man as food.
5. Bird: same size as domestic fowl, but could be sea-birds.
The population on the Islands increased progressively, enough to enable
the development of a new culture requiring the building of a
significant number of large temples during a period of about 1500 years
(c. 4100 - 2500 BC). The increasing population was supported by a
higher agricultural production achieved mainly by utilising the land
more intensively, by the reduction of pasture land and woodland, and by
shortening the fallow periods in the shifting agricultural system. The
Temple Culture farmers relied basically on the same crops that were
utilised in the earlier Neolithic period, though there were probably
changes in emphasis. There may well have been more interest in crops
like the olive and the vine. Excavation at the Tarxien Phase level
(3300/3000-2500 BC) at Scorba revealed carbonised remains of the tree
species Pinus halepensis (Aleppio pine) and Olea europaea
(Olive) [Metcalfe, 1966].
The domesticated animals were much the same, but cattle
appear to have
become less important, possibly because the better land was used for
agriculture and there was less good pasture land available. Sheep and
goats could be grazed on poorer ground abandoned by the farmer. The
stresses placed on the soils made these liable to lose their fertility.
Over a period of time shifting cultivation and heavy grazing altered
the natural vegetation and resulted in the clearance of the woodland
areas. The woodland apparently disappeared as farming became more
intensive and the disturbed land was encroached by plant species best
suited for this environment. It appears from the land snail species
identified from deposits at Brochtorff Circle in Gozo that the area was
probably a garrique environment which forms on the barren Upper
Coralline Limestone and on which only a few hardy plant species survive
[Schembri, 1994].
The stresses placed on the environment by the increasing agricultual
efforts of Late Neolithic man contributed to the eventual decline of
the community. The Neolithic Temple culture of the Islands of Malta in
the Central Mediterranean disappeared around 2500 BC. Several attempts
have been made to unravel the mystery of how and why this splendid
civilization came to such an abrupt end after reaching heights of
artistic and architectural achievement, but none of the theories
suggested so far is entirely satisfactory. The most plausible one seems
to be that the population was compelled to abandon the islands
following a series of drought that ruined their triving, but sensitive,
agricultural economy. Scarcity of food, with accompanying deaths from
malnutrition and disease, broke down the social relationships of the
Temple Culture. The abrupt climatic change could very easily have been
caused by a series of volcanic eruptions in the region which gave rise
to the fall of a number of Old World Eastern Civilizations, all of
which apparently fell at about the same period [Weiss, 1996].
The direct and indirect effects of man and the continous efforts
required to enable him to compete in the continously changing
environment have resulted in the creation of a new group of stresses -
both mental and physical, besides the appearance of a new group of
disease conditions. During the Palaeolithic age, man was a
hunter-gatherer who lived in scattered groups of perhapds 50 to 100
individuals. The low numbers and low densities of the population
reduced the incidence of viral and bacterial infections so that people
were not troubled by contagious disease such as smallpox or measles,
where pathogens require large dense populations for survival. Moreover,
the lifestyle of hunter-gatherers spared them other illnesses. They
were often on the move and thus were not tied to a neighbourhood long
enough to pollute water sources with human wastes that transmit
disease, nor to pile up refuse that attracts disease-carrying insects
and animals. Fimally, hunter-gatherers had no domesticated animals.
Tamed animals helped to create civilizations with their meat, hides,
milk, eggs, and bones but also transmitted many disease. The situation
changed with the advent of the neolithic age when man group up into
larger communities, farmed the land and domesticated animals.
References
1. Boessneck J., Kuver M: Alluviale Tierknochenfunde aus der Ghar Dalam
- Hohle, Malta. Senckenbergiana Biol./i>, LI:p.147-158, 1970
2. Gandert O-F.: 1966: Preliminary report on the animal bones.
Appendix III. In: Trump D.H.: Skorba - excavations carried out on
behalf of the National Museum of Malta 1962-64. Report of the
Research Committee of the Society of Antiquaries of London, xxii, 1966
3. Helbaek H.: Report on carbonized grain from AFS (Ghar Dalam
Phase). Appendix IV. In: Trump D.H.: Skorba - excavations
carried out on behalf of the National Museum of Malta 1962-64.
Report of the Research Committee of the Society of Antiquaries of
London, xxii, 1966
4. Lanfranco, G.: Hxejjex Medicinali u ohrajn fil Gzejjer Maltin.
Media Centere, Malta, 1993, +132p.
5. Metcalfe C.R.: Report on the botanical determination of charcoal
samples. Appendix V. In: Trump D.H.: Skorba - excavations
carried out on behalf of the National Museum of Malta 1962-64.
Report of the Research Committee of the Society pf Antiquaries of
London, xxii, 1966
6. Pike G.: The Animal Bones from the Xemxija Tombs. Appendix
In: Evans J.D.: The prehistoric antiquities of the Maltese Islands:
A Survey. University of London, 1971
7. Schembri P.J.: Reconstructing the Palaeoenvironment of the
Maltese Islands. Brochtorff Circle Seminar - The Archaeological
Society, 10 September 1994 (lecture)
8. Storch G.: Holozane Kleinsaugerfunde aus der Ghar Dalam-Hohle, Malta
(Mammalia: Insectivora, Chiroptera, Rodentia). Senckenbergiana Biol.,
LI:135-145, 1970
9. Thake M.A.: Land snails from the Mellieha quaternary deposits. Potamon,
14:93, 1985
10. Weiss H.: Destert Storm. The Sciences, 36(3):30-36, 1996
11. Zammit Maempel G.: An outline of Maltese geology. Malta,
+44p., 1977
12. Zammit Maempel G.: A Maltese Pleistocene sequence capped by
volcanic tufa. Atti Soc. Tuscana Sci. Nat. Mem.,
ser.B(xliii):p225-240, 1982
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