15 research outputs found
New data on the large brown bear (Ursus Arctos l., 1758, Ursidae, Carnivora, Mammalia) from the pleistocene of Yakutia
ΠΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ Π³ΠΈΠΏΠΎΠΊΡΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΠΏΡΠ΅ΠΊΠΎΠ½Π΄ΠΈΡΠΈΠΎΠ½ΠΈΡΠΎΠ²Π°Π½ΠΈΡ Π΄Π»Ρ ΠΏΠΎΠ΄Π³ΠΎΡΠΎΠ²ΠΊΠΈ Π°ΡΡΠΎΠ΄Π΅ΡΠΌΠΎΡΡΠ°Π½ΡΠΏΠ»Π°Π½ΡΠ°ΡΠ° Ρ Π±ΠΎΠ»ΡΠ½ΡΡ ΡΠΎ ΡΠΊΠΎΠΌΠΏΡΠΎΠΌΠ΅ΡΠΈΡΠΎΠ²Π°Π½Π½ΠΎΠΉ ΠΌΠΈΠΊΡΠΎΡΠΈΡΠΊΡΠ»ΡΡΠΈΠ΅ΠΉ
Objective: to study the impact of the concentration of cytokine HIF-1Ξ± in the donor area on the processes of reparative regeneration in free autodermografting by split-thickness skin graft for patients with disorders of the microvasculature and to improve results of autodermografting by local stimulation of HIF-1Ξ± to prepare skin graft to hypoxia conditions.Materials and methods. The hypothesis of the influence of the local circulatory hypoxia on the concentration of HIF-1Ξ± was checked in the experiment with 18 white outbred male rats weighing 250β300 g. The microcirculation level was controlled by laser doppler flowmetry method. The indications to appraise the correctness of the hypothesis were analytical data of Enzyme Multiplied Immunoassay. This method of treatment was used in the clinic, where 18 patients with diabetic foot infections syndrome needed dermatoplastic surgery, and compared with the results of treatment of 22 patients with free autodermografting performed by traditional way.Results. It is identified the significant difference in concentration of cytokine HIF-1Ξ± in the donor skin area in preparation it for hypoxia conditions by proposed method. The experimental data are confirmed in the clinic. After the free autodermografting based on developed technique in the main group the viability of grafter was preserved on Me (Q1; Q3) 84 (78; 93) % of its area. In the control group graft acceptance is registered on Me (Q1; Q3) 72 (65; 79) % of grafter area (p = 0.012).Π¦Π΅Π»Ρ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ β ΠΈΠ·ΡΡΠ΅Π½ΠΈΠ΅ Π²Π»ΠΈΡΠ½ΠΈΡ ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΠΈ Π² Π΄ΠΎΠ½ΠΎΡΡΠΊΠΎΠΉ ΠΎΠ±Π»Π°ΡΡΠΈ ΡΠΈΡΠΎΠΊΠΈΠ½Π° HIF-1Ξ± Π½Π° ΠΏΡΠΎΡΠ΅ΡΡΡ ΡΠ΅ΠΏΠ°ΡΠ°ΡΠΈΠ²Π½ΠΎΠΉ ΡΠ΅Π³Π΅Π½Π΅ΡΠ°ΡΠΈΠΈ ΠΏΡΠΈ ΡΠ²ΠΎΠ±ΠΎΠ΄Π½ΠΎΠΉ Π°ΡΡΠΎΠ΄Π΅ΡΠΌΠΎΠΏΠ»Π°ΡΡΠΈΠΊΠ΅ ΡΠ°ΡΡΠ΅ΠΏΠ»Π΅Π½Π½ΡΠΌ ΠΊΠΎΠΆΠ½ΡΠΌ ΡΡΠ°Π½ΡΠΏΠ»Π°Π½ΡΠ°ΡΠΎΠΌ Ρ Π±ΠΎΠ»ΡΠ½ΡΡ
Ρ ΠΏΠ°ΡΠΎΠ»ΠΎΠ³ΠΈΠ΅ΠΉ ΠΌΠΈΠΊΡΠΎΡΠΈΡΠΊΡΠ»ΡΡΠΎΡΠ½ΠΎΠ³ΠΎ ΡΡΡΠ»Π° ΠΈ ΡΠ»ΡΡΡΠ΅Π½ΠΈΠ΅ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΠΎΠ² Π°ΡΡΠΎΠ΄Π΅ΡΠΌΠΎΠΏΠ»Π°ΡΡΠΈΠΊΠΈ ΠΏΡΡΠ΅ΠΌ Π»ΠΎΠΊΠ°Π»ΡΠ½ΠΎΠΉ ΡΡΠΈΠΌΡΠ»ΡΡΠΈΠΈ Π²ΡΡΠ°Π±ΠΎΡΠΊΠΈ HIF-1Ξ± Π² ΡΠ΅Π»ΡΡ
ΠΏΠΎΠ΄Π³ΠΎΡΠΎΠ²ΠΊΠΈ ΡΡΠ°Π½ΡΠΏΠ»Π°Π½ΡΠ°ΡΠ° ΠΊ ΡΡΠ»ΠΎΠ²ΠΈΡΠΌ Π³ΠΈΠΏΠΎΠΊΡΠΈΠΈ.ΠΠ°ΡΠ΅ΡΠΈΠ°Π»Ρ ΠΈ ΠΌΠ΅ΡΠΎΠ΄Ρ. Π ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ΅ Π³ΠΈΠΏΠΎΡΠ΅Π·Ρ Π²Π»ΠΈΡΠ½ΠΈΡ Π»ΠΎΠΊΠ°Π»ΡΠ½ΠΎΠΉ ΡΠΈΡΠΊΡΠ»ΡΡΠΎΡΠ½ΠΎΠΉ Π³ΠΈΠΏΠΎΠΊΡΠΈΠΈ Π½Π° ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΡ HIF-1Ξ± ΠΏΡΠΎΠ²Π΅ΡΠΈΠ»ΠΈ Π½Π° 18 Π±Π΅Π»ΡΡ
Π±Π΅ΡΠΏΠΎΡΠΎΠ΄Π½ΡΡ
ΠΊΡΡΡΠ°Ρ
-ΡΠ°ΠΌΡΠ°Ρ
ΠΌΠ°ΡΡΠΎΠΉ ΡΠ΅Π»Π° 250β300 Π³. Π£ΡΠΎΠ²Π΅Π½Ρ ΠΌΠΈΠΊΡΠΎΡΠΈΡΠΊΡΠ»ΡΡΠΈΠΈ ΠΊΠΎΠ½ΡΡΠΎΠ»ΠΈΡΠΎΠ²Π°Π»ΠΈ ΠΌΠ΅ΡΠΎΠ΄ΠΎΠΌ Π»Π°Π·Π΅ΡΠ½ΠΎΠΉ Π΄ΠΎΠΏΠΏΠ»Π΅ΡΠΎΠ²ΡΠΊΠΎΠΉ ΡΠ»ΠΎΡΠΌΠ΅ΡΡΠΈΠΈ. ΠΡΠΈΡΠ΅ΡΠΈΡΠΌΠΈ, ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡΡΠΈΠΌΠΈ ΠΎΡΠ΅Π½ΠΈΡΡ ΠΏΡΠ°Π²ΠΈΠ»ΡΠ½ΠΎΡΡΡ Π³ΠΈΠΏΠΎΡΠ΅Π·Ρ, ΡΠ²ΠΈΠ»ΠΈΡΡ Π΄Π°Π½Π½ΡΠ΅ ΠΈΠΌΠΌΡΠ½ΠΎΡΠ΅ΡΠΌΠ΅Π½ΡΠ½ΠΎΠ³ΠΎ Π°Π½Π°Π»ΠΈΠ·Π°. Π ΠΊΠ»ΠΈΠ½ΠΈΠΊΠ΅ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π»ΠΈ ΠΏΡΠ΅Π΄Π»ΠΎΠΆΠ΅Π½Π½ΡΠΉ ΡΠΏΠΎΡΠΎΠ± ΠΏΡΠΈ Π»Π΅ΡΠ΅Π½ΠΈΠΈ 18 Π±ΠΎΠ»ΡΠ½ΡΡ
Ρ ΡΠΈΠ½Π΄ΡΠΎΠΌΠΎΠΌ Π΄ΠΈΠ°Π±Π΅ΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΡΠΎΠΏΡ, ΡΡΠ΅Π±ΠΎΠ²Π°Π²ΡΠΈΠΌ Π²ΡΠΏΠΎΠ»Π½Π΅Π½ΠΈΡ ΠΊΠΎΠΆΠ½ΠΎ-ΠΏΠ»Π°ΡΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΉ, ΡΡΠ°Π²Π½ΠΈΠ²Π°Ρ Ρ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΠ°ΠΌΠΈ Π»Π΅ΡΠ΅Π½ΠΈΡ 22 Π±ΠΎΠ»ΡΠ½ΡΡ
, Ρ ΠΊΠΎΡΠΎΡΡΡ
ΡΠ²ΠΎΠ±ΠΎΠ΄Π½ΡΡ Π°ΡΡΠΎΠ΄Π΅ΡΠΌΠΎΠΏΠ»Π°ΡΡΠΈΠΊΡ Π²ΡΠΏΠΎΠ»Π½ΡΠ»ΠΈ ΡΡΠ°Π΄ΠΈΡΠΈΠΎΠ½Π½ΡΠΌ ΡΠΏΠΎΡΠΎΠ±ΠΎΠΌ.Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ. ΠΡΡΠ²Π»Π΅Π½Π° ΡΡΠ°ΡΠΈΡΡΠΈΡΠ΅ΡΠΊΠΈ Π·Π½Π°ΡΠΈΠΌΠ°Ρ ΡΠ°Π·Π½ΠΈΡΠ° Π² ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΠΈ ΡΠΈΡΠΎΠΊΠΈΠ½Π° HIF-1Ξ± Π² ΠΊΠΎΠΆΠ΅ Π΄ΠΎΠ½ΠΎΡΡΠΊΠΎΠΉ ΠΎΠ±Π»Π°ΡΡΠΈ ΠΏΡΠΈ ΠΏΠΎΠ΄Π³ΠΎΡΠΎΠ²ΠΊΠ΅ Π΅Π΅ ΠΊ ΡΡΠ»ΠΎΠ²ΠΈΡΠΌ Π³ΠΈΠΏΠΎΠΊΡΠΈΠΈ ΠΏΡΠ΅Π΄Π»ΠΎΠΆΠ΅Π½Π½ΡΠΌ ΡΠΏΠΎΡΠΎΠ±ΠΎΠΌ. ΠΠ°Π½Π½ΡΠ΅ ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ° ΠΏΠΎΠ΄ΡΠ²Π΅ΡΠΆΠ΄Π΅Π½Ρ Π² ΠΊΠ»ΠΈΠ½ΠΈΠΊΠ΅. Π ΠΎΡΠ½ΠΎΠ²Π½ΠΎΠΉ Π³ΡΡΠΏΠΏΠ΅ ΠΏΠΎΡΠ»Π΅ Π²ΡΠΏΠΎΠ»Π½Π΅Π½ΠΈΡ ΡΠ²ΠΎΠ±ΠΎΠ΄Π½ΠΎΠΉ Π°ΡΡΠΎΠ΄Π΅ΡΠΌΠΎΠΏΠ»Π°ΡΡΠΈΠΊΠΈ ΠΏΠΎ ΡΠ°Π·ΡΠ°Π±ΠΎΡΠ°Π½Π½ΠΎΠΉ ΠΌΠ΅ΡΠΎΠ΄ΠΈΠΊΠ΅ ΠΆΠΈΠ·Π½Π΅ΡΠΏΠΎΡΠΎΠ±Π½ΠΎΡΡΡ ΡΡΠ°Π½ΡΠΏΠ»Π°Π½ΡΠ°ΡΠ° ΡΠΎΡ
ΡΠ°Π½ΡΠ»Π°ΡΡ Π½Π° Me (Q1; Q3) 84 (78; 93) % Π΅Π³ΠΎ ΠΏΠ»ΠΎΡΠ°Π΄ΠΈ. Π ΠΊΠΎΠ½ΡΡΠΎΠ»ΡΠ½ΠΎΠΉ Π³ΡΡΠΏΠΏΠ΅ ΠΏΡΠΈΠΆΠΈΠ²Π»Π΅Π½ΠΈΠ΅ ΠΎΡΠΌΠ΅ΡΠ΅Π½ΠΎ Π½Π° Me (Q1; Q3) 72 (65; 79) % ΠΏΠ»ΠΎΡΠ°Π΄ΠΈ ΡΡΠ°Π½ΡΠΏΠ»Π°Π½ΡΠ°ΡΠ° (Ρ = 0,012)
New data on the large brown bear (Ursus Arctos l., 1758, Ursidae, Carnivora, Mammalia) from the pleistocene of Yakutia
Hydrological modeling of green roofs runoff by nash cascade model
Green roofs (GRs) technology has gained increasing interest in recent years since it offers multiple benefits to urban environments, citizens and buildings. Eco-covers can capture some water nutrient pollutants, filter air pollutants and moderate the urban heat island effect. Beyond these benefits, abundant literature stresses the role played by the GRs from the hydrological perspective. They allow to face the increasing stress on the traditional urban drainage systems by reducing the annual stormwater runoff. In light of this, the hydrological behavior prediction of a vegetated cover is essential for urban planners, policy makers and engineers in order to quantify runoff mitigation potential so as to optimize their application. Objective: The aim of the present research is to meet this need by testing the accuracy of Nash cascade model in predicting the stormwater production of GR systems. Materials and Methods: The proposed model has been calibrated against hourly data of thirteen rainfall-runoff events observed at two experimental sites, both located within the campus of the University of Salerno, southern Italy. Event scale model calibration, aimed at the identification of the storage coefficient parameter, has been based on the optimization of a number of error statistics. Results and Conclusion: Despite its simplicity, the investigated model appears adequately to be able to predict the runoff production from the experimental green roofs with a good degree of accuracy, as described by the Nash-Sutcliffe Efficiency index, which ranges between 0.54 and 0.94
New data on mammoth fauna mammals in the central Lena River basin (Yakutia, Lenskie Stolby National Nature Park and adjacent areas)
This paper considers the data on new findings of mammoth fauna remains in the Middle Lena basin used to specify the species composition of large Late Neopleistocene mammals represented by eleven species. The obtained range of radiocarbon dates made it possible to state that mass burials of Pleistocene mammal remains were formed in the region during the Karginsk Interstadial (24 000-55 000 years ago)
New data on the large brown bear (Ursus Arctos l., 1758, Ursidae, Carnivora, Mammalia) from the pleistocene of Yakutia
A study of a frozen mummy of a wild horse from the Holocene of Yakutia, East Siberia, Russia
The paper presents a description of a rare finding of the partial frozen corpse of the Yukagir horse. Discovered from thawing deposits in northern East Siberia (Yakutia, Russia), its age is confirmed to be Mid-Holocene (about 4600 BP). The mummy had a preserved head with the neck and the back of the torso with the legs and tail. The Yukagir horse was relatively short, with short ears and tail. Compared to the modern breeds, including the Yakutian domestic horse, wild Przewalski's horse, and extinct Lena horse, Equus lenensis, the Yukagir horse was closest to the latter, which was also confirmed by studies of the hair microstructure. The pollen and plant remains from the horse's intestines indicated a preference to grasses. The late geological age of the Yukagir horse is an indication that this species survived the Pleistocene-Holocene crisis and lived through the Mid-Holocene in northern Eastern Siberia
New Data on Large Brown Bear (Ursus arctos L., 1758, Ursidae, Carnivora, Mammalia) from the Pleistocene in Yakutia
New finds of brown bear (Ursus arctos L., 1758) fossil remains from the territory of Yakutia, namely, skulls and mandibular bones, have been investigated. The new finds are exceptionally large: most dimensions of these specimens exceed those of the present-day brown bears of Yakutia and even the maximal parameters of the largest individuals of the present-day Eurasian subspecies U. a. beringianus and U. a. piscator. Analysis of various data showed that giant brown bears had inhabited northern Yakutia during the Karginian interstadial in the Late Pleistocene