Morphometric variation between populations of recent wild boar in Israel

Author(s):  
Goggy Davidowitz ◽  
Kolska Liora Horwitz

Today the wild boar (subspecies Sub scrofa lybica Gray, 1868) is the largest wild mammal found in Israel (Mendelssohn & Yom Tov 1999a). Sus scrofa has formed an integral part of the fauna of Israel since c.0.78 Mya, with the earliest skeletal remains derived from the Lower Palaeolithic site of Gesher Benot Ya’akov, Israel (Hooijer 1959; Geraads & Tchernov 1983). Remains of wild boar are commonly found in archaeological assemblages in this region (e.g. Davis 1982; Tchernov 1988), and according to 19th-century travellers, wild boar were abundant throughout Palestine, including the thickets of the Jordan river and the Dead Sea, and even extended into the arid regions of the northern Negev and Judean desert (Tristram 1866; Hart 1891; Bodenheimer 1958; Qumsiyeh 1996). However, during the period of the Mandate of Palestine (1923–48) the population size of wild boar was severely reduced by hunting, and as a consequence, their distribution was reduced to the Jordan valley, from the Hula Lake in the north to Sdom at the southern tip of the Dead Sea (Bodenheimer 1958; Mendelssohn & Yom-Tov 1999 a, 1999b). Since the creation of the State of Israel in 1948 they have been protected by legislation, which, coupled with the reduced numbers of predators, has resulted in a marked increase in their numbers. Nowadays, wild boar occupy most of their former habitats including the coastal region. The species has also been observed as far south as Nahal Besor in the northern Negev, but it has been proposed that these animals may represent hybrids of domestic pigs and wild boar (Mendelssohn & Yom-Tov 1999b). Four main concentrations of wild boar can be identified in Israel today: the Upper Galilee (especially in the national park of Mount Meiron), the Hula Nature Reserve, the Golan Heights, and Sdom. As shown in Table 12.1, these areas differ markedly in vegetation, altitude, and climate. A study of dental pathology in skeletal collections derived from these groups showed significant differences between the four areas (Horwitz & Davidowitz 1992). Specifically, the Sdom group was characterized by an unusually high frequency of hypodontia of the lower third incisor, indicative of inbreeding.

1984 ◽  
Vol 121 (6) ◽  
pp. 577-587 ◽  
Author(s):  
P. E. R. Lovelock

AbstractThe structure of the northern part of the Arabian platform is reviewed in the light of hitherto unpublished exploration data and the presently accepted kinematic model of plate motion in the region. The Palmyra and Sinjar zones share a common history of development involving two stages of rifting, one in the Triassic–Jurassic and the other during late Cretaceous to early Tertiary times. Deformation of the Palmyra zone during the Mio-Pliocene is attributed to north–south compression on the eastern block of the Dead Sea transcurrent system which occurred after continental collision in the north in southeast Turkey. The asymmetry of the Palmyra zone is believed to result from northward underthrusting along the southern boundary facilitated by the presence of shallow Triassic evaporites. An important NW-SE cross-plate shear zone has been identified, which can be traced for 600 km and which controls the course of the River Euphrates over long distances in Syria and Iraq. Transcurrent motion along this zone resulted in the formation of narrow grabens during the late Cretaceous which were compressed during the Mio-Pliocene. To a large extent, present day structures in the region result from compressional reactivation of old lineaments within the Arabian plate by the transcurrent motion of the Dead Sea fault zone and subsequent continental collision.


Subject The implications of the Red Sea-Dead Sea plan. Significance Israel and Jordan on February 26 signed an agreement to facilitate water-sharing and address the depletion of the Dead Sea, which is receding at a rate of about a metre per year. The 900 million dollar World Bank-sponsored 'Seas Canal' deal consists of two main aspects: local water exchange deals, with Jordan providing Israel with desalinated water from Aqaba in exchange for bluewater from the Sea of Galilee in the north; and saltwater transfer from the Red Sea to the Dead Sea. The Palestinian Authority is not party to the agreement, and awaits a separate deal with Israel. Impacts Prospects for Palestinian-Israeli water negotiations have drastically decreased. Jordan will still need to agree further desalination and cooperation deals in order to meet demand. Water saving efforts will be pushed aside in favour of much more costly desalination. Desalination powered by burning fossil hydrocarbons accelerates global warming.


1954 ◽  
Vol 1 (2) ◽  
pp. 137-141
Author(s):  
Bo Reicke

The Hebrew scrolls newly discovered near Qumran at the north-western shore of the Dead Sea, which are attracting more and more the attention of New Testament students, are also very important for the evolution of Jewish Gnosticism. One may think especially of the fact that in some of these manuscripts the Hebrew word for ‘knowledge’ and related terms occur with a striking frequency, and that the dualistic cosmology of the new texts seems to be rather like certain fundamental ideas of Gnosticism. Since the archaeological evidence now proves that the Qumran manuscripts are pre-Christian, or were at least written in the first Christian century, one may very well state that new light can now be thrown upon the much debated question of a pre-Christian, Jewish Gnosticism.


2016 ◽  
Vol 43 (6) ◽  
pp. 2494-2501 ◽  
Author(s):  
Yariv Hamiel ◽  
Oksana Piatibratova ◽  
Yaakov Mizrahi

1997 ◽  
Vol 24 (16) ◽  
pp. 2063-2066 ◽  
Author(s):  
Avihu Ginzburg ◽  
Zvi Ben-Avraham

1888 ◽  
Vol 5 (9) ◽  
pp. 387-395 ◽  
Author(s):  
Israel C. Russell

The occurrence of numerous terraces on the mountain slopes over-looking the Dead Sea has been reported by several observers, but no accurate measurements of their elevations or definite correlation of the terraces on the opposite slopes of the depression, seem to have been attempted. In the central part of the Wady Arabah on the west flank of the promontory known as Samrat el Fedan, a terrace, or perhaps more properly a gravel bar, has been observed by Hull at an elevation of about 1300 feet above the Dead Sea. This is apparently a definite record of the surface level of the Dead Sea during a former period. On the sides of the Jordan valley the terraces range in height from a few feet to 750 feet above the river. The measurements reported show great variation due principally to an inclination of the surfaces of the terraces, towards the centre of the valley, but indicating also that they are not horizontal in the direction of drainage.


Nature ◽  
1912 ◽  
Vol 90 (2241) ◽  
pp. 165-166
Author(s):  
T. G. B

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