7 research outputs found
Acineta nitocrae: A new suctorian epizooic on nonindigenous harpacticoid copepods, Nitocra hibernica and N. incerta, in the Laurentian Great Lakes
Sessile Ciliates (Ciliophora) from Extreme Habitats
Π‘ΡΠ°ΡΡΡ ΠΏΡΠ΅Π΄ΡΡΠ°Π²Π»ΡΠ΅Ρ ΡΠΎΠ±ΠΎΠΉ ΠΎΠ±Π·ΠΎΡ ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
ΡΠΈΠΏΠΎΠ² ΡΠΊΡΡΡΠ΅ΠΌΠ°Π»ΡΠ½ΡΡ
ΠΌΠ΅ΡΡΠΎΠΎΠ±ΠΈΡΠ°Π½ΠΈΠΉ, Π² ΠΊΠΎΡΠΎΡΡΡ
Π±ΡΠ»ΠΈ Π½Π°ΠΉΠ΄Π΅Π½Ρ ΡΠΈΠ΄ΡΡΠΈΠ΅ ΠΈΠ½ΡΡΠ·ΠΎΡΠΈΠΈ. ΠΡΠ½ΠΎΠ²Π½ΠΎΠ΅ Π²Π½ΠΈΠΌΠ°Π½ΠΈΠ΅ Π² ΡΠ°Π±ΠΎΡΠ΅ ΡΠ΄Π΅Π»Π΅Π½ΠΎ ΠΌΠ΅ΡΡΠΎΠΎΠ±ΠΈΡΠ°Π½ΠΈΡΠΌ, ΠΈΠ· ΠΊΠΎΡΠΎΡΡΡ
Π±ΡΠ»ΠΈ ΠΏΠΎΠ»ΡΡΠ΅Π½Ρ ΠΎΡΠΈΠ³ΠΈΠ½Π°Π»ΡΠ½ΡΠ΅ ΠΌΠ°ΡΠ΅ΡΠΈΠ°Π»Ρ: Π³ΠΈΠΏΠ΅ΡΠ³Π°Π»ΠΈΠ½Π½ΡΠΌ Π²ΠΎΠ΄ΠΎΠ΅ΠΌΠ°ΠΌ, Π³Π»ΡΠ±ΠΎΠΊΠΎΠ²ΠΎΠ΄Π½ΡΠΌ ΠΌΠ΅ΡΡΠΎΠΎΠ±ΠΈΡΠ°Π½ΠΈΡΠΌ ΡΠ°Π·Π½ΠΎΠ³ΠΎ ΡΠΈΠΏΠ°, Π° ΡΠ°ΠΊΠΆΠ΅ ΠΏΠ΅ΡΠ΅ΡΠ½ΡΠΌ ΠΈ ΠΏΠΎΠ΄Π·Π΅ΠΌΠ½ΡΠΌ Π²ΠΎΠ΄Π°ΠΌ. ΠΠ½Π°Π»ΠΈΠ·ΠΈΡΡΡΡΡΡ Π½Π°Ρ
ΠΎΠ΄ΠΊΠΈ ΡΡΠΊΡΠΎΡΠΈΠΉ Acinetides infundibuliformis, Acineta harpacticicola ΠΈ ΠΏΠ΅ΡΠΈΡΡΠΈΡ
ΠΈ Cothurnia maritima Π² Π³ΠΈΠΏΠ΅ΡΠ³Π°Π»ΠΈΠ½Π½ΡΡ
Π²ΠΎΠ΄ΠΎΠ΅ΠΌΠ°Ρ
(ΠΏΡΠΈ ΡΠΎΠ»Π΅Π½ΠΎΡΡΠΈ ΠΎΡ 38 Π΄ΠΎ 60 β°), ΡΡΠΊΡΠΎΡΠΈΠΉ Corynophrya abyssalis ΠΈΠ· ΡΠΎΠΎΠ±ΡΠ΅ΡΡΠ²Π° Π³ΠΈΠ΄ΡΠΎΡΠ΅ΡΠΌΠΎΠ² (Π³Π»ΡΠ±ΠΈΠ½Π° 4095 ΠΌ) ΠΈ Thecacineta calix, Π½Π°ΠΉΠ΄Π΅Π½Π½ΠΎΠΉ Π² ΠΠ½Π΄Π°ΠΌΠ°Π½ΡΠΊΠΎΠΌ ΠΌΠΎΡΠ΅ (Π³Π»ΡΠ±ΠΈΠ½Π° 1301 ΠΌ), ΡΡΠΊΡΠΎΡΠΈΠΉ Paracineta livadiana, C. lyngbyi ΠΈ ΠΏΠ΅ΡΠΈΡΡΠΈΡ
ΠΈ C. maritima ΠΈΠ· ΡΠ΅ΡΠΎΠ²ΠΎΠ΄ΠΎΡΠΎΠ΄Π½ΠΎΠΉ Π·ΠΎΠ½Ρ Π§Π΅ΡΠ½ΠΎΠ³ΠΎ ΠΌΠΎΡΡ (Π³Π»ΡΠ±ΠΈΠ½Ρ 80-300 ΠΌ), Π° ΡΠ°ΠΊΠΆΠ΅ ΡΡΠΊΡΠΎΡΠΈΠΉ Tokophrya niphargi ΠΈ Spelaeophrya troglocaridis ΠΈ Π°ΠΏΠΎΡΡΠΎΠΌΠ°Ρ Gymnodinioides sp. Π² ΠΏΠ΅ΡΠ΅ΡΠ½ΡΡ
ΠΈ ΠΏΠΎΠ΄Π·Π΅ΠΌΠ½ΡΡ
Π²ΠΎΠ΄Π°Ρ
. ΠΠ±ΡΡΠΆΠ΄Π°ΡΡΡΡ Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΡΠ΅ Π°Π΄Π°ΠΏΡΠ°ΡΠΈΠΈ ΠΏΠ΅ΡΠ΅ΡΠΈΡΠ»Π΅Π½Π½ΡΡ
ΠΈΠ½ΡΡΠ·ΠΎΡΠΈΠΉ ΠΊ ΡΡΠ»ΠΎΠ²ΠΈΡΠΌ ΡΠΊΡΡΡΠ΅ΠΌΠ°Π»ΡΠ½ΡΡ
ΠΌΠ΅ΡΡΠΎΠΎΠ±ΠΈΡΠ°Π½ΠΈΠΉ. ΠΠΎΠΊΠ°Π·Π°Π½ΠΎ, ΡΡΠΎ Π΄Π»Ρ ΠΈΠ½ΡΡΠ·ΠΎΡΠΈΠΉ-ΡΠΊΡΡΡΠ΅ΠΌΠΎΡΠΈΠ»ΠΎΠ² Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠ½Ρ ΡΠΈΠ·ΠΈΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠ΅ Π°Π΄Π°ΠΏΡΠ°ΡΠΈΠΈ ΠΊ ΡΠΊΡΡΡΠ΅ΠΌΠ°Π»ΡΠ½ΡΠΌ ΡΠ°ΠΊΡΠΎΡΠ°ΠΌ. ΠΠΌΠ΅ΡΡΠΈΠ΅ΡΡ Ρ ΡΠ°ΠΊΠΈΡ
Π²ΠΈΠ΄ΠΎΠ² ΠΌΠΎΡΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΡΡΡΡΠΊΡΡΡΡ ΠΈ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠΈ ΡΠ°Π·ΠΌΠ½ΠΎΠΆΠ΅Π½ΠΈΡ ΡΠ²Π»ΡΡΡΡΡ Π°Π΄Π°ΠΏΡΠ°ΡΠΈΡΠΌΠΈ ΠΊ Π½Π΅Π±Π»Π°Π³ΠΎΠΏΡΠΈΡΡΠ½ΡΠΌ ΡΠ°ΠΊΡΠΎΡΠ°ΠΌ Π² ΡΠ΅Π»ΠΎΠΌThe present article addresses an overview of different types of extreme habitats in which sessile ciliates were found. Ciliates were found in different extreme habitats (marine deep waters, hypersaline, caves, and subterranean waters). Authors registered 11 species of sessile ciliates in extreme environments: suctorians Corynophrya abyssalis in a hydrothermal vent field (4090 m depth), Thecacineta calix in the Andaman Sea (1301 m depth), Paracineta livadiana, C. lyngbyi and peritrichous ciliate Cothurnia maritima in hypoxic/anoxic conditions of the Black Sea (80-300 m depth), suctorian ciliates Tokophrya niphargi and Spelaeophrya troglocaridis and apostome ciliate Gymnodinioides sp. in cave and subterranean waters, as well as suctorians Acinetides infundibuliformis, Acineta harpacticicola and peritrichous ciliate C. maritima in hypersaline waters (salinity from 38 β° to 60 β°). The possible adaptations of listed ciliates to extreme habitats are discussed. It is difficult to identify any morphological adaptations of these ciliate species to life in extreme conditions. There are the physiological adaptations to extreme factors in extremophile ciliates. Some morphological structures and breeding characteristics, which are presented in ciliates living in extreme environments, may be adaptations to such conditions in genera
New reports of sessile ciliates from Amsterdam, The Netherlands
The aim of this contribution is to present some ciliate reports from Amsterdam, the Netherlands. They are: Acineta nitocrae Dovgal, 1984, Metacineta micraster (Penard, 1914), Opercularia sp., Campanella sp., Platycola decumbens Ehrenberg, 1830, Thuricola folliculata Kent, 1881, and Stentor sp. The systematic position of the several finds of these species are given along with the related information in the study. To the best of our knowledge, this is the first time that A. nitocrae has been reported in Northern European freshwaters, which is the third region after Ukraine and Canada where the species was found.Celem pracy jest doniesienie dotyczΔ
ce stwierdzenia orzΔskΓ³w z Amsterdamu w Holandii. SΔ
to: Acineta nitocrae Dovgal, 1984, Metacineta micraster (Penard, 1914), Opercularia sp., Campanella sp., Platycola decumbens Ehrenberg, 1830, Thuricola folliculata Kent, 1881 i Stentor sp. Podano pozycjΔ systematycznΔ
wybranych gatunkΓ³w. WedΕug naszej najlepszej wiedzy jest to pierwszy przypadek wystΔpowania A. nitocrae w sΕodkowodnych wodach Europy PΓ³Εnocnej, ktΓ³re sΔ
trzecim regionem po Ukrainie i Kanadzie, gdzie ten gatunek zostaΕ znaleziony
Sessile Ciliates (Ciliophora) from Extreme Habitats
Π‘ΡΠ°ΡΡΡ ΠΏΡΠ΅Π΄ΡΡΠ°Π²Π»ΡΠ΅Ρ ΡΠΎΠ±ΠΎΠΉ ΠΎΠ±Π·ΠΎΡ ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
ΡΠΈΠΏΠΎΠ² ΡΠΊΡΡΡΠ΅ΠΌΠ°Π»ΡΠ½ΡΡ
ΠΌΠ΅ΡΡΠΎΠΎΠ±ΠΈΡΠ°Π½ΠΈΠΉ, Π² ΠΊΠΎΡΠΎΡΡΡ
Π±ΡΠ»ΠΈ Π½Π°ΠΉΠ΄Π΅Π½Ρ ΡΠΈΠ΄ΡΡΠΈΠ΅ ΠΈΠ½ΡΡΠ·ΠΎΡΠΈΠΈ. ΠΡΠ½ΠΎΠ²Π½ΠΎΠ΅ Π²Π½ΠΈΠΌΠ°Π½ΠΈΠ΅ Π² ΡΠ°Π±ΠΎΡΠ΅ ΡΠ΄Π΅Π»Π΅Π½ΠΎ ΠΌΠ΅ΡΡΠΎΠΎΠ±ΠΈΡΠ°Π½ΠΈΡΠΌ, ΠΈΠ· ΠΊΠΎΡΠΎΡΡΡ
Π±ΡΠ»ΠΈ ΠΏΠΎΠ»ΡΡΠ΅Π½Ρ ΠΎΡΠΈΠ³ΠΈΠ½Π°Π»ΡΠ½ΡΠ΅ ΠΌΠ°ΡΠ΅ΡΠΈΠ°Π»Ρ: Π³ΠΈΠΏΠ΅ΡΠ³Π°Π»ΠΈΠ½Π½ΡΠΌ Π²ΠΎΠ΄ΠΎΠ΅ΠΌΠ°ΠΌ, Π³Π»ΡΠ±ΠΎΠΊΠΎΠ²ΠΎΠ΄Π½ΡΠΌ ΠΌΠ΅ΡΡΠΎΠΎΠ±ΠΈΡΠ°Π½ΠΈΡΠΌ ΡΠ°Π·Π½ΠΎΠ³ΠΎ ΡΠΈΠΏΠ°, Π° ΡΠ°ΠΊΠΆΠ΅ ΠΏΠ΅ΡΠ΅ΡΠ½ΡΠΌ ΠΈ ΠΏΠΎΠ΄Π·Π΅ΠΌΠ½ΡΠΌ Π²ΠΎΠ΄Π°ΠΌ. ΠΠ½Π°Π»ΠΈΠ·ΠΈΡΡΡΡΡΡ Π½Π°Ρ
ΠΎΠ΄ΠΊΠΈ ΡΡΠΊΡΠΎΡΠΈΠΉ Acinetides infundibuliformis, Acineta harpacticicola ΠΈ ΠΏΠ΅ΡΠΈΡΡΠΈΡ
ΠΈ Cothurnia maritima Π² Π³ΠΈΠΏΠ΅ΡΠ³Π°Π»ΠΈΠ½Π½ΡΡ
Π²ΠΎΠ΄ΠΎΠ΅ΠΌΠ°Ρ
(ΠΏΡΠΈ ΡΠΎΠ»Π΅Π½ΠΎΡΡΠΈ ΠΎΡ 38 Π΄ΠΎ 60 β°), ΡΡΠΊΡΠΎΡΠΈΠΉ Corynophrya abyssalis ΠΈΠ· ΡΠΎΠΎΠ±ΡΠ΅ΡΡΠ²Π° Π³ΠΈΠ΄ΡΠΎΡΠ΅ΡΠΌΠΎΠ² (Π³Π»ΡΠ±ΠΈΠ½Π° 4095 ΠΌ) ΠΈ Thecacineta calix, Π½Π°ΠΉΠ΄Π΅Π½Π½ΠΎΠΉ Π² ΠΠ½Π΄Π°ΠΌΠ°Π½ΡΠΊΠΎΠΌ ΠΌΠΎΡΠ΅ (Π³Π»ΡΠ±ΠΈΠ½Π° 1301 ΠΌ), ΡΡΠΊΡΠΎΡΠΈΠΉ Paracineta livadiana, C. lyngbyi ΠΈ ΠΏΠ΅ΡΠΈΡΡΠΈΡ
ΠΈ C. maritima ΠΈΠ· ΡΠ΅ΡΠΎΠ²ΠΎΠ΄ΠΎΡΠΎΠ΄Π½ΠΎΠΉ Π·ΠΎΠ½Ρ Π§Π΅ΡΠ½ΠΎΠ³ΠΎ ΠΌΠΎΡΡ (Π³Π»ΡΠ±ΠΈΠ½Ρ 80-300 ΠΌ), Π° ΡΠ°ΠΊΠΆΠ΅ ΡΡΠΊΡΠΎΡΠΈΠΉ Tokophrya niphargi ΠΈ Spelaeophrya troglocaridis ΠΈ Π°ΠΏΠΎΡΡΠΎΠΌΠ°Ρ Gymnodinioides sp. Π² ΠΏΠ΅ΡΠ΅ΡΠ½ΡΡ
ΠΈ ΠΏΠΎΠ΄Π·Π΅ΠΌΠ½ΡΡ
Π²ΠΎΠ΄Π°Ρ
. ΠΠ±ΡΡΠΆΠ΄Π°ΡΡΡΡ Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΡΠ΅ Π°Π΄Π°ΠΏΡΠ°ΡΠΈΠΈ ΠΏΠ΅ΡΠ΅ΡΠΈΡΠ»Π΅Π½Π½ΡΡ
ΠΈΠ½ΡΡΠ·ΠΎΡΠΈΠΉ ΠΊ ΡΡΠ»ΠΎΠ²ΠΈΡΠΌ ΡΠΊΡΡΡΠ΅ΠΌΠ°Π»ΡΠ½ΡΡ
ΠΌΠ΅ΡΡΠΎΠΎΠ±ΠΈΡΠ°Π½ΠΈΠΉ. ΠΠΎΠΊΠ°Π·Π°Π½ΠΎ, ΡΡΠΎ Π΄Π»Ρ ΠΈΠ½ΡΡΠ·ΠΎΡΠΈΠΉ-ΡΠΊΡΡΡΠ΅ΠΌΠΎΡΠΈΠ»ΠΎΠ² Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠ½Ρ ΡΠΈΠ·ΠΈΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠ΅ Π°Π΄Π°ΠΏΡΠ°ΡΠΈΠΈ ΠΊ ΡΠΊΡΡΡΠ΅ΠΌΠ°Π»ΡΠ½ΡΠΌ ΡΠ°ΠΊΡΠΎΡΠ°ΠΌ. ΠΠΌΠ΅ΡΡΠΈΠ΅ΡΡ Ρ ΡΠ°ΠΊΠΈΡ
Π²ΠΈΠ΄ΠΎΠ² ΠΌΠΎΡΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΡΡΡΡΠΊΡΡΡΡ ΠΈ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠΈ ΡΠ°Π·ΠΌΠ½ΠΎΠΆΠ΅Π½ΠΈΡ ΡΠ²Π»ΡΡΡΡΡ Π°Π΄Π°ΠΏΡΠ°ΡΠΈΡΠΌΠΈ ΠΊ Π½Π΅Π±Π»Π°Π³ΠΎΠΏΡΠΈΡΡΠ½ΡΠΌ ΡΠ°ΠΊΡΠΎΡΠ°ΠΌ Π² ΡΠ΅Π»ΠΎΠΌThe present article addresses an overview of different types of extreme habitats in which sessile ciliates were found. Ciliates were found in different extreme habitats (marine deep waters, hypersaline, caves, and subterranean waters). Authors registered 11 species of sessile ciliates in extreme environments: suctorians Corynophrya abyssalis in a hydrothermal vent field (4090 m depth), Thecacineta calix in the Andaman Sea (1301 m depth), Paracineta livadiana, C. lyngbyi and peritrichous ciliate Cothurnia maritima in hypoxic/anoxic conditions of the Black Sea (80-300 m depth), suctorian ciliates Tokophrya niphargi and Spelaeophrya troglocaridis and apostome ciliate Gymnodinioides sp. in cave and subterranean waters, as well as suctorians Acinetides infundibuliformis, Acineta harpacticicola and peritrichous ciliate C. maritima in hypersaline waters (salinity from 38 β° to 60 β°). The possible adaptations of listed ciliates to extreme habitats are discussed. It is difficult to identify any morphological adaptations of these ciliate species to life in extreme conditions. There are the physiological adaptations to extreme factors in extremophile ciliates. Some morphological structures and breeding characteristics, which are presented in ciliates living in extreme environments, may be adaptations to such conditions in genera
Determining Stability Conditions for Haulage Drifts Protected by Coal Pillars
The aim of this research is to study the stability of haulage drifts and the manifestations of rock pressure in them lengthwise the working area when protecting them with coal pillars.To assess the stability of workings, field experiments were conducted to study the manifestations of rock pressure in the haulage drifts of a steep coal seam. It has been registered that as the breakage face progresses, the displacement of roof rocks on the contour of the drift linearly increases with an increase in the length of the working area.The deformation properties of coal pillars were studied taking into consideration the extent of the convergence of the roof and soil. This paper reports a theoretical model that describes the destruction of the above-drift coal pillars when unloading the coal-bearing massif that hosts the workings.It has been determined that the equilibrium state of coal pillars is ensured when the specific deformation and stress potentials are equal before the occurrence of main cracks of destruction. As the relative deformation of coal pillars increases at compression, when this equality is broken, the specific energy intensity of destruction increases. It is noted that at a distance exceeding l>10 m behind the breakage face, the occurrence of the main cracks of destruction is followed by a stability loss in the coal pillars. As a result of external forces, the change in the volume and shape of the coal pillars causes the intensification of the process of convergence of lateral rocks on the contour of haulage drifts lengthwise the working area and leads, with a certain degree of probability, to a deterioration in the stability of workings.The results of this study could be used to justify the choice of technique to protect haulage drifts. This would allow the timely development of minefield reserves thereby improving the safety of operations. It is recommended that the technique of protecting haulage drifts by coal pillars should be abandone
Determining Stability Conditions for Haulage Drifts Protected by Coal Pillars
The aim of this research is to study the stability of haulage drifts and the manifestations of rock pressure in them lengthwise the working area when protecting them with coal pillars.To assess the stability of workings, field experiments were conducted to study the manifestations of rock pressure in the haulage drifts of a steep coal seam. It has been registered that as the breakage face progresses, the displacement of roof rocks on the contour of the drift linearly increases with an increase in the length of the working area.The deformation properties of coal pillars were studied taking into consideration the extent of the convergence of the roof and soil. This paper reports a theoretical model that describes the destruction of the above-drift coal pillars when unloading the coal-bearing massif that hosts the workings.It has been determined that the equilibrium state of coal pillars is ensured when the specific deformation and stress potentials are equal before the occurrence of main cracks of destruction. As the relative deformation of coal pillars increases at compression, when this equality is broken, the specific energy intensity of destruction increases. It is noted that at a distance exceeding l>10 m behind the breakage face, the occurrence of the main cracks of destruction is followed by a stability loss in the coal pillars. As a result of external forces, the change in the volume and shape of the coal pillars causes the intensification of the process of convergence of lateral rocks on the contour of haulage drifts lengthwise the working area and leads, with a certain degree of probability, to a deterioration in the stability of workings.The results of this study could be used to justify the choice of technique to protect haulage drifts. This would allow the timely development of minefield reserves thereby improving the safety of operations. It is recommended that the technique of protecting haulage drifts by coal pillars should be abandone