From Brittany to the Black Sea: Nicholas Sabraham and English Military Experience in the Fourteenth Century

Author(s):  
Andrew Ayton
Author(s):  
David Abulafia

The fall of Acre in 1291 shocked western Europe, which had in fact done little to protect the city in its last decades. Plans to launch new expeditions abounded, and among the greatest enthusiasts was Charles II of Naples, after his release from his Catalan gaol. But this was all talk; he was far too preoccupied with trying to defeat the Aragonese to be able to launch a crusade, nor did he have the resources to do so. The Italian merchants diversified their interests to cope with the loss of access to eastern silks and spices through Acre. Venice gradually took the lead in Egypt, while the Genoese concentrated more on bulky goods from the Aegean and the Black Sea, following the establishment of a Genoese colony in Constantinople in 1261. But the Byzantine emperors were wary of the Genoese. They favoured the Venetians as well, though to a lesser degree, so that the Genoese would not assume they could do whatever they wished. Michael VIII and his son Andronikos II confined the Genoese to the high ground north of the Golden Horn, the area known as Pera, or Galata, where a massive Genoese tower still dominates the skyline of northern Istanbul, but they also granted them the right to self-government, and the Genoese colony grew so rapidly that it soon had to be extended. By the mid-fourteenth century the trade revenues of Genoese Pera dwarfed those of Greek Constantinople, by a ratio of about seven to one. These emperors effectively handed control of the Aegean and the Black Sea to the Genoese, and Michael’s navy, consisting of about eighty ships, was dismantled by his son. It was assumed that God would protect Constantinople as a reward for the rejection of all attempts at a union of the holy Orthodox Church with the unholy Catholic one. The Genoese generally tolerated a Venetian presence, for war damaged trade and ate up valuable resources. Occasionally, as in 1298, pirate attacks by one side caused a crisis, and the cities did go to war.


1979 ◽  
Vol 40 (C2) ◽  
pp. C2-445-C2-448
Author(s):  
D. Barb ◽  
L. Diamandescu ◽  
M. Morariu ◽  
I. I. Georgescu

Author(s):  
Eleonora P. Radionova

The associations and ecological conditions of the existence of modern diatoms of the North-West (Pridneprovsky), Prikerchensky and Eastern regions of the subtidal zone of the Black Sea are considered. Based on the unity of the composition of the Present and Sarmatian-Meotian diatom flora, an attempt has been made to model some of the ecological c situation of the Late Miocene Euxinian basin.


2002 ◽  
Vol 8 (2-3) ◽  
pp. 231-238
Author(s):  
G.K. Korotaev ◽  
◽  
M.E. Li ◽  
G.A. Tolkachenko ◽  
◽  
...  

2020 ◽  
Vol 42 (4) ◽  
pp. 33-49
Author(s):  
O.V. CHEPIZHKO ◽  
V.V. YANKO ◽  
V.M. KADURIN ◽  
I.M. NAUMKO ◽  
S.M. SHATALIN

For the first time the importance of mineralogical and lithological-petrographical ranks in the line of geological information ranks is substantiated for implementation of long-term forecasts, standard and non-standard approaches to research of physical and geochemical parameters as a basis of creation of complex system of forecast criteria and prospecting indicators of hydrocarbons within the sedimentary cover of Black sea based on the theory of global fluid-flows derivation. These criteria have different sensitivity to the object (hydrocarbon deposits) and are therefore ranked. The ranking determined the following parameters: 1) seismic data within the object, obtained by the method of deep seismic sounding, RWM SDP; 2) parameters of tectono-geodynamic structures; 3) the main characteristics of sedimentary cover and bedrock; 4) geochemical characteristics; 5) parameters of mineral complexes and fluid inclusions in mineral neoformations; 6) the value of the distribution of meiobenthos. Based on modern views of oil and gas geology, structural-tectonic and lithological-facies criteria are among the main ones. The study of the mineralogical component of sediments is made with using mineralogical, thermobarogeochemical and X-ray spectral methods. Fixation of anomalies of fluid flow at the bottom of the Black Sea as to the distribution of abiotic parameters in order to assess the prospects of oil and gas is determined by structural and tectonic features and high permeability of fluid flow; parameters of mineral complexes (minerals, facies) and genetic connections; heterogeneity of geochemical characteristics of bottom sediments; the presence of hydrocarbon inclusions in authigenic minerals of bottom sediments.


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