Acartia tonsa: a species new for the Black Sea fauna

1994 ◽  
pp. 9-15 ◽  
Author(s):  
Genuario Belmonte ◽  
Maria Grazia Mazzocchi ◽  
Ira Yu. Prusova ◽  
Nicola V. Shadrin
Keyword(s):  
Black Sea ◽  
Acartia Tonsa ◽  
The Black Sea

Oithona davisae: naturalization in the Black sea, inter-annual and seasonal dynamics, effect on the structure of the planktonic copepod community

2019 ◽  
Vol 59 (6) ◽  
pp. 1008-1015
Author(s):  
A. D. Gubanova ◽  
O. A. Garbazey ◽  
D. A. Altukhov ◽  
V. S. Mukhanov ◽  
E. V. Popova
Keyword(s):  
Black Sea ◽  
Coastal Waters ◽  
Native Species ◽  
Significant Decline ◽  
Acartia Tonsa ◽  
The Black Sea ◽  
Copepod Community ◽  
Oithona Davisae ◽  
Sevastopol Bay

Long-term (20032014) routine observations of zooplankton in Sevastopol Bay (the Black Sea) have allowed the naturalization of the invasive copepod Oithona davisae to be studied in the Black Sea coastal waters. Inter-annual and seasonal variability of the species and their impact on the native copepod community have been analyzed. The invasion of O. davisae and their undoubted dominance in terms of abundance were shown to alter the community structure but, at the same time, the abundances of the native species did not decrease, excepting the Black Sea earlier invader Acartia tonsa. A significant decline in A. tonsa numbers over the stages of O. davisae establishment and naturalization provided evidence of competition between the species. O. davisae have been demonstrated to gain competitive advantage over A. tonsa, that ensured their fast dispersal in the Black Sea, acclimatization in the new habitat and the successful competition over native species.

scholarly journals Occurrence of Acartia tonsa Dana in the Black Sea. Was it introduced from the Mediterranean?

2000 ◽  
Vol 1 (1) ◽  
pp. 105 ◽  
Author(s):  
A. GUBANOVA
Keyword(s):  
Black Sea ◽  
Seasonal Dynamics ◽  
Size Structure ◽  
World Ocean ◽  
Acartia Tonsa ◽  
The Black Sea ◽  
The World ◽  
The Mediterranean ◽  
First Time ◽  
Ship’S Ballast Water

It was reported for the first time that Acartia tonsa was present in the Black Sea as early as in 1976. A.tonsa was found in the Mediterranean Sea in 1985. So, this copepod was initially introduced to the Black Sea and did not invade here from the Mediterranean. Probably A.tonsa was transferred to the Black Sea with ship's ballast water from some other region of the World Ocean. Differences in seasonal dynamics and size structure of A.clausi and A.tonsa in the Bay of Sevastopol in 1976 are discussed.

Acartia tonsa: a species new for the Black Sea fauna

Hydrobiologia ◽  
1994 ◽  
Vol 292-293 (1) ◽  
pp. 9-15 ◽  
Author(s):  
Genuario Belmonte ◽  
Maria Grazia Mazzocchi ◽  
Ira Yu. Prusova ◽  
Nicola V. Shadrin
Keyword(s):  
Black Sea ◽  
Acartia Tonsa ◽  
The Black Sea

Fate of the Black Sea Acartia clausi and Acartia tonsa (Copepoda) penetrating into the Marmara Sea through the Bosphorus

2008 ◽  
Vol 76 (1) ◽  
pp. 131-140 ◽  
Author(s):  
Elena Hubareva ◽  
Leonid Svetlichny ◽  
Ahmet Kideys ◽  
Melek Isinibilir
Keyword(s):  
Black Sea ◽  
Acartia Tonsa ◽  
The Black Sea ◽  
Marmara Sea ◽  
Acartia Clausi

MÖSSBAUER AND CHEMICAL ANALYSES OF SOME SEDIMENTS FROM THE ROMANIAN SHORE OF THE BLACK SEA

1979 ◽  
Vol 40 (C2) ◽  
pp. C2-445-C2-448
Author(s):  
D. Barb ◽  
L. Diamandescu ◽  
M. Morariu ◽  
I. I. Georgescu
Keyword(s):  
Black Sea ◽  
The Black Sea ◽  
Chemical Analyses

Modeling of ecological conditions in the Euxine Basin in the Sarmatian and Maeotian by methods of diatom analysis

2019 ◽  
pp. 257-261
Author(s):  
Eleonora P. Radionova
Keyword(s):  
Black Sea ◽  
Late Miocene ◽  
The Black Sea ◽  
Subtidal Zone ◽  
Diatom Analysis ◽  
Diatom Flora ◽  
North West ◽  
Ecological Conditions ◽  
The North

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.

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