About 2 million years ago, the world climate underwent a series of cold-warm periods which gave rise to the Ice Ages. These climate fluctuations caused the periodic growth of ice sheets on land in high latitudes and mountains during the glacial periods, while the interglacial climate was similar to those prevailing today. The ice cap during the glacial periods advanced at a rate of 100 m/yr. and has been estimated to have been about 2500 m thick across Europe. The ice cap however never reached further than 400 latitude and thus the Maltese Islands were never covered with ice. The regions south to 40o latitude were affected by Pluvial periods which saw very unsettled weather with increasing rain precipitation. The Mediterreanean region may in fact have been rather arid during the glacials, increasing in humidity during the interglacial periods. The cool wetter climate of the Pluvial period allowed the southern extension of the Central European forests of pine, olive, juniper, cedar and fir. In addition the uptake of water in the increasing ice-cap resulted in a drop in the sea level, estimated at a total drop of 150 m in the Central Mediterranean during the last Ice Age. This sea level drop was sufficient to expose the submarine ridge of the Central Mediterranean thus connecting the Maltese Islands to mainland Europe. The advancing cold weather in Europe also forced the warm-loving animals to migrate southwards reaching the Maltese Islands. It is estimated that the Pleistocene period may have undergone a total of about 17 cold periods. This cycle of mainland connection of the Maltese Islands followed by a period of isolation allowed for the development of a number of endemic species which were generally characterised by dwarfism of the herbivore mammals and gigantism of rodent, reptilian and avian species. Similar species development has also been reported from other Mediterranean small islands.
During the Late Middle Pleistocene (c.130,000-180,000 years ago), the excavated fauna clearly suggest a wetter climate than that prevalent today. There is also evidence of a small lake in the west of Malta. However the presence of Laurel suggests a Mediterranean climate characterised by a hot dry season. The animals prevalent during this period included the dwarfed endemic hippopotamus and elephant species, besides extinct species of dormice, bats and avian remains. The deposits are generally referred to as Hippopotamus or Leithia cartei layer. No human remains or artefacts have been definitely associated with this stratigraphical layer.
The mainland connection was again re-established during the last Ice Age period during Late Upper Pleistocene (23,000 - 10,000 years ago). During this phase the climate in the Central Mediterranean was cooler than that prevailing today. A large number of species have been excavated from the various Late Upper Pleistocene deposits on the Maltese Islands, the prevalent animals appear to have been stunted forms of deer (Cervus elaphus), scanty remains of small sized carnivores (Ursus, vulpes, canis), and remains of bats, voles, birds, turtles and amphibians. Deposits of this period are typically referred to as Cervus or Pitymys melitensis layer. Stratification studies of trenches dug at Ghar Dalam suggest that the Cervus layer frequently had incorporated hippopotami and elephant remains in the lower layers, in association with Carnivores and Cervus. Human remains and artefacts were also found in this stratigraphical layer. The uppermost layer of the Cervus horizon was apparently devoid of carnivores and pacchyderms.
The recurrent land-links between the Maltese Islands and Sicily resulted
in similar faunal associations in both regions. The Pleistocene Sicilian
faunal repertiore have been grouped into four main stages dated by various
techniques. Several Maltese faunal associations have been described from
various sites in Malta - the most important sites being Ghar Dalam and
the Maghlaq Region with its caves and costal deposits. An attempt has been
made to correlate the Maltese faunal associations with those reported in
Sicily.
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MAGHLAQ/BENGHISA BEDS MAGHLAQ/MELLIEHA CAVE |
Microfauna: Erinaceus europaeus; Lepus europaeus Avian: various species |
Microfauna: Pitymys melitensis, Crocidura sp, Rhinolophus hipposideros, Rh. euryale, Rh. mehelyi, Rh. blasii, Miniopterus schreibersi Herpetofauna: Bufo bufo, Emys orbicularis, CHELONIA, (? Species) Avian: Passerine birds, Branta bernicla, Turdus sp; Scolopax ghardalamensis; Corvus cf frugilegus; Estrildidae |
(Maghlaq costal) |
200+/-40 ka Herpetofauna: Testudo sp. |
? 190 +/- 20 ka Herpetofauna: Testudo (?) graeca Avian: Corvus cf. frugilegus, ?Hawk Gliridae/Hippo Stage ? 190 +/- 20 ka Microfauna: Leithia cartei, Hypnomys gollcheri, Crocidura cf. russula, Rhinolophus hipposideros, Rh. mehelyi birzebbugensis, Rh. Blasii, Myotis exilis, M. bechsteini robustus, M. ghardalamensis, M. capaccini, Eptesicus praeglacialis, Pipistrelus pipistrellus, Minopterus schreibersi Avian: Anas acuta (?); Coturnix coturnix, Alectoris graeca (?); Scolopax ghardalamensis; Tyto alba; Otius scops; Hirundo sp; Turdus sp; Carduelis chloris; Coccothraustes coccothraustes; Sturnus vulgaris |
(Maghlaq Cave) Avian: large and small sp. _________________
Hippopotamus bed
Avian: large avian species |
455+/-90 ka Microfauna: Crocidura esui; Leithia melitensis; Leithia cartei; Rhinolophus hipposideros; Rh. mehelyi; Rh. cf blasii; Myotis bechsteini; M. capaccini; Minopterus schreibersi Herpetofauna: Discoglossus cf. pictus; Bufo viridis; Hyla sp.; Geochelone sp.; Testudo hermanni; Emys orbicularis; Lacerta viridis; L. siculomelitensis; Coluber cf viridiflavus; Natrix sp |
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Microfauna: Leithia melitensis; Leithia cartei, Maltamys gollcheri; a chiropteran species Herpetofauna: Geocelone robusta; Lacerta siculomelitensis Avian: Grus grus, Grus melitensis, Cygnus falconeri, Cygnus melitensis, and other small avian species remains |
Microfauna: Pellegrinia panormensis; Apodemus maximus; Leithia sp.; Hypolagus sp |
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