29 research outputs found

    Cannabinoid receptors expression in bone marrow trephine biopsy of chronic lymphocytic leukaemia patients treated with purine analogues

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    Background: Cannabinoid receptors CB1 and CB2 are part the endocannabinoid system that plays an important role in the process of proliferation and apoptosis of different neoplastic cells. B-cell chronic lymphocytic leukaemia is one of the diseases in which these processes are altered. Aim: The aim of our study was the assessment of cannabinoid receptor expression on the B-lymphocytes in bone marrow trephine biopsy from leukaemic patients at diagnosis and after purine analogue treatment. Methods: The biopsy was taken routinely and standard immunohistochemical staining procedure for paraffin embedded sections was applied. The cannabinoid receptors were detected using specific primary polyclonal antibody anti-CB1 and anti-CB2. Additionally, an existence of cannabinoid receptors was confirmed by flow cytometry. Results: The results showed that the expression of CB1 receptor on the surface of neoplastic cells was lower than that of CB2 (17.0 Β± 3.1% and 92.1 Β± 1.7% respectively, p < 0.001). Nine of the patients responded to applied treatment with a reduction in leukaemic infiltration (77.2 Β± 6.9% to 30.2 Β± 6.5%, p = 0.007) and CB1 receptor expression (24.4 Β± 4.8% to 8.6 Β± 2.9%, p = 0.01), but there was no change in CB2 expression (91.7 Β± 2.7% vs 90.9 Β± 2.8%, p = 0.69). Four patients without remission expressed even greater number of the receptors. In all of the cases both cannabinoid receptor types antibodies gave positive reaction. Furthermore, the existence of cannabinoid receptors on neoplastic lymphocytes was confirmed by flow cytometry. Conclusion: The study provides original evidence for the existence of cannabinoid receptors on B-lymphocytes in chronic lymphocytic leukaemia patients. The receptors are thought to be a new structure that can modify the course of the disease and may be considered as a new target in leukaemia treatment.ОбоснованиС: Ρ€Π΅Ρ†Π΅ΠΏΡ‚ΠΎΡ€Ρ‹ ΠΊΠ°Π½Π½Π°Π±ΠΈΠ½ΠΎΠΈΠ΄ΠΎΠ² CB1 ΠΈ CB2 яв Π»ΡΡŽΡ‚ΡΡ Ρ‡Π°ΡΡ‚ΡŒΡŽ систСмы эндоканнабиноидов, которая ΠΈΠ³Ρ€Π°Π΅Ρ‚ Π²Π°ΠΆΠ½ΡƒΡŽ Ρ€ΠΎΠ»ΡŒ Π² процСссах ΠΏΡ€ΠΎΠ»ΠΈΡ„Π΅Ρ€Π°Ρ†ΠΈΠΈ ΠΈ Π°ΠΏΠΎΠΏΡ‚ΠΎΠ·Π° Ρ€Π°Π·Π»ΠΈΡ‡Π½Ρ‹Ρ… нСопластичСских ΠΊΠ»Π΅Ρ‚ΠΎΠΊ. Одним ΠΈΠ· Π·Π°Π±ΠΎΠ»Π΅Π²Π°Π½ΠΈΠΉ, ΠΏΡ€ΠΈ ΠΊΠΎΡ‚ΠΎΡ€Ρ‹Ρ… происходит Π½Π°Ρ€ΡƒΡˆΠ΅Π½ΠΈΠ΅ этих процСссов, являСтся Π’-ΠΊΠ»Π΅Ρ‚ΠΎΡ‡Π½Ρ‹ΠΉ хроничСский Π»ΠΈΠΌΡ„Π»Π΅ΠΉΠΊΠΎΠ·. ЦСль: ΠΎΡ†Π΅Π½ΠΊΠ° экспрСссии Ρ€Π΅Ρ†Π΅ΠΏΡ‚ΠΎΡ€ΠΎΠ² ΠΊΠ°Π½Π½Π°Π±ΠΈΠ½ΠΎΠΈΠ΄ΠΎΠ² Π½Π° Π’-Π»ΠΈΠΌΡ„ΠΎΡ†ΠΈΡ‚Π°Ρ… Π² Ρ‚Ρ€Π΅ΠΏΠ°Π½ΠΎΠ±ΠΈΠΎΠΏΡ‚Π°Ρ‚Π°Ρ… Ρƒ Π±ΠΎΠ»ΡŒΠ½Ρ‹Ρ… Π»Π΅ΠΉΠΊΠΎΠ·ΠΎΠΌ Π΄ΠΎ ΠΈ послС провСдСния лСчСния с использованиСм ΠΏΡƒΡ€ΠΈΠ½ΠΎΠ²Ρ‹Ρ… Π°Π½Π°Π»ΠΎΠ³ΠΎΠ². ΠœΠ΅Ρ‚ΠΎΠ΄Ρ‹: Π±ΠΈΠΎΠΏΡ‚Π°Ρ‚Ρ‹ ΠΏΠΎΠ»ΡƒΡ‡ΠΈΠ»ΠΈ Ρ€ΡƒΡ‚ΠΈΠ½Π½Ρ‹ΠΌΠΈ ΠΌΠ΅Ρ‚ΠΎΠ΄Π°ΠΌΠΈ; иммуногистохимичСскоС исслСдованиС Π΄Π΅ΠΏΠ°Ρ€Π°Ρ„ΠΈΠ½ΠΈΠ·ΠΈΡ€ΠΎΠ²Π°Π½Π½Ρ‹Ρ… срСзов ΠΏΡ€ΠΎΠ²ΠΎΠ΄ΠΈΠ»ΠΈ ΠΏΠΎ стандартной ΠΏΡ€ΠΎΡ†Π΅Π΄ΡƒΡ€Π΅. Π Π΅Ρ†Π΅ΠΏΡ‚ΠΎΡ€Ρ‹ ΠΊΠ°Π½Π½Π°Π±ΠΈΠ½ΠΎΠΈΠ΄ΠΎΠ² опрСдСляли с использованиСм спСцифичСских ΠΌΠΎΠ½ΠΎΠΊΠ»ΠΎΠ½Π°Π»ΡŒΠ½Ρ‹Ρ… Π°Π½Ρ‚ΠΈΡ‚Π΅Π» Π°Π½Ρ‚ΠΈ-CB1 ΠΈ Π°Π½Ρ‚ΠΈ-CB2. ΠšΡ€ΠΎΠΌΠ΅ Ρ‚ΠΎΠ³ΠΎ, Π½Π°Π»ΠΈΡ‡ΠΈΠ΅ Ρ€Π΅Ρ†Π΅ΠΏΡ‚ΠΎΡ€ΠΎΠ² ΠΏΠΎΠ΄Ρ‚Π²Π΅Ρ€ΠΆΠ΄Π΅Π½ΠΎ ΠΏΡ€ΠΈ ΠΏΠΎ- ΠΌΠΎΡ‰ΠΈ ΠΏΡ€ΠΎΡ‚ΠΎΡ‡Π½ΠΎΠΉ Ρ†ΠΈΡ‚ΠΎΡ„Π»ΡƒΠΎΡ€ΠΈΠΌΠ΅Ρ‚Ρ€ΠΈΠΈ. Π Π΅Π·ΡƒΠ»ΡŒΡ‚Π°Ρ‚Ρ‹: ΠΏΠΎΠΊΠ°Π·Π°Π½ΠΎ, Ρ‡Ρ‚ΠΎ экспрСссия Ρ€Π΅Ρ†Π΅ΠΏΡ‚ΠΎΡ€Π° CB1 Π½Π° повСрхности ΠΎΠΏΡƒΡ…ΠΎΠ»Π΅Π²Ρ‹Ρ… ΠΊΠ»Π΅Ρ‚ΠΎΠΊ Π½ΠΈΠΆΠ΅, Ρ‡Π΅ΠΌ экспрСссия CB2 (17,0Β  Β± 3,1% ΠΈ 92,1 1,7% Ρ‚Π²Π΅Π½Π½ΠΎ, p < 0,001). ПослС ΠΏΡ€ΠΎΠ²Π΅Π΄Π΅Π½Π½ΠΎΠ³ΠΎ лСчСния Ρƒ 9 ΠΏΠ°Ρ†ΠΈΠ΅Π½Ρ‚ΠΎΠ² ΠΎΡ‚ΠΌΠ΅Ρ‡Π°Π»ΠΎΡΡŒ ΡƒΠΌΠ΅Π½ΡŒΡˆΠ΅Π½ΠΈΠ΅ Π»Π΅ΠΉΠΊΠΎΠ·Π½ΠΎΠ³ΠΎ ΠΈΠ½Ρ„ΠΈΠ»ΡŒΡ‚Ρ€Π°Ρ‚Π° (77,2 6,9% Π΄ΠΎ 30,2 6,5%, p = 0,007) ΠΈ сниТСниС экспрСссии Ρ€Π΅Ρ†Π΅ΠΏΡ‚ΠΎΡ€Π° CB1 (24,4 4,8% Π΄ΠΎ 8,6 2,9%, p = 0,01), ΠΎΠ΄Π½Π°ΠΊΠΎ Ρ€Π°Π·Π»ΠΈΡ‡ΠΈΠΉ Π² экспрСссии CB2 Π½Π΅ ΠΎΡ‚ΠΌΠ΅Ρ‡Π°Π»ΠΈ (91,7 2,7% ΠΏΡ€ΠΎΡ‚ΠΈΠ² 90,9 2,8%, p = 0,69). Π£ 4 ΠΏΠ°Ρ†ΠΈΠ΅Π½Ρ‚ΠΎΠ², Ρƒ ΠΊΠΎΡ‚ΠΎΡ€Ρ‹Ρ… Π½Π΅ ΡƒΠ΄Π°Π»ΠΎΡΡŒ Π΄ΠΎΡΡ‚ΠΈΡ‡ΡŒ рСмиссии, опрСдСляли Π΄Π°ΠΆΠ΅ ΠΏΠΎΠ²Ρ‹ΡˆΠ΅Π½ΠΈΠ΅ экспрСссии Ρ€Π΅Ρ†Π΅ΠΏΡ‚ΠΎΡ€ΠΎΠ². Π’ΠΎ всСх случаях ΠΌΠ°Ρ€ΠΊΠΈΡ€ΠΎΠ²ΠΊΠΈ Π°Π½Ρ‚ΠΈΡ‚Π΅Π»Π°ΠΌΠΈ ΠΊ ΠΎΠ±ΠΎΠΈΠΌ Ρ‚ΠΈΠΏΠ°ΠΌ Ρ€Π΅Ρ†Π΅ΠΏΡ‚ΠΎΡ€ΠΎΠ² ΠΊΠ°Π½Π½Π°Π±ΠΈΠ½ΠΎΠΈΠ΄ΠΎΠ² ΠΎΡ‚ΠΌΠ΅Ρ‡Π°Π»ΠΈ ΠΏΠΎΠ»ΠΎ- ΠΆΠΈΡ‚Π΅Π»ΡŒΠ½ΡƒΡŽ Ρ€Π΅Π°ΠΊΡ†ΠΈΡŽ. Π‘ΠΎΠ»Π΅Π΅ Ρ‚ΠΎΠ³ΠΎ, присутствиС Ρ€Π΅Ρ†Π΅ΠΏΡ‚ΠΎΡ€ΠΎΠ² ΠΊΠ°Π½Π½Π°Π±ΠΈΠ½ΠΎΠΈΠ΄ΠΎΠ² Π½Π° злокачСствСнных ΠΊΠ»Π΅Ρ‚ΠΊΠ°Ρ… ΠΏΠΎΠ΄Ρ‚Π²Π΅Ρ€ΠΆΠ΄Π°Π»ΠΈ ΠΏΡ€ΠΈ ΠΏΠΎΠΌΠΎΡ‰ΠΈ ΠΏΡ€ΠΎΡ‚ΠΎΡ‡Π½ΠΎΠΉ Ρ†ΠΈΡ‚ΠΎΠΌΠ΅Ρ‚Ρ€ΠΈΠΈ. Π’Ρ‹Π²ΠΎΠ΄Ρ‹: Π² Ρ…ΠΎΠ΄Π΅ исслСдования ΠΏΠΎΠΊΠ°Π·Π°Π½ΠΎ ΠΈΠ·Π½Π°Ρ‡Π°Π»ΡŒΠ½ΠΎΠ΅ Π½Π°Π»ΠΈΡ‡ΠΈΠ΅ Ρ€Π΅Ρ†Π΅ΠΏΡ‚ΠΎΡ€ΠΎΠ² ΠΊΠ°Π½Π½Π°Π±ΠΈΠ½ΠΎΠΈΠ΄ΠΎΠ² Π½Π° Π’-Π»ΠΈΠΌΡ„ΠΎΡ†ΠΈΡ‚Π°Ρ… Ρƒ Π±ΠΎΠ»ΡŒΠ½Ρ‹Ρ… хроничСским Π»ΠΈΠΌΡ„ΠΎΠ»Π΅ΠΉΠΊΠΎΠ·ΠΎΠΌ. Π£ΠΊΠ°Π·Π°Π½Π½Ρ‹Π΅ Ρ€Π΅Ρ†Π΅ΠΏΡ‚ΠΎΡ€Ρ‹ ΠΌΠΎΠ³ΡƒΡ‚ Π±Ρ‹Ρ‚ΡŒ Π½ΠΎΠ²ΠΎΠΉ структурой, которая ΠΌΠΎΠΆΠ΅Ρ‚ Π±Ρ‹Ρ‚ΡŒ ΠΌΠΎΠ΄ΠΈΡ„ΠΈΡ†ΠΈΡ€ΠΎΠ²Π°Π½Π° Π² Ρ‚Π΅Ρ‡Π΅Π½ΠΈΠ΅ Π±ΠΎΠ»Π΅Π·Π½ΠΈ, ΠΈ ΠΌΠΎΠ³ΡƒΡ‚ ΡΡ‡ΠΈΡ‚Π°Ρ‚ΡŒΡΡ Π½ΠΎΠ²ΠΎΠΉ мишСнью ΠΏΡ€ΠΈ Π»Π΅Ρ‡Π΅Π½ΠΈΠΈ Π±ΠΎΠ»ΡŒΠ½Ρ‹Ρ… Π»Π΅ΠΉΠΊΠΎΠ·ΠΎΠΌ

    Rapid and highly variable warming of lake surface waters around the globe

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    In this first worldwide synthesis of in situ and satellite-derived lake data, we find that lake summer surface water temperatures rose rapidly (global mean = 0.34Β°C decadeβˆ’1) between 1985 and 2009. Our analyses show that surface water warming rates are dependent on combinations of climate and local characteristics, rather than just lake location, leading to the counterintuitive result that regional consistency in lake warming is the exception, rather than the rule. The most rapidly warming lakes are widely geographically distributed, and their warming is associated with interactions among different climatic factorsβ€”from seasonally ice-covered lakes in areas where temperature and solar radiation are increasing while cloud cover is diminishing (0.72Β°C decadeβˆ’1) to ice-free lakes experiencing increases in air temperature and solar radiation (0.53Β°C decadeβˆ’1). The pervasive and rapid warming observed here signals the urgent need to incorporate climate impacts into vulnerability assessments and adaptation efforts for lakes.Peer reviewe

    Rapid and highly variable warming of lake surface waters around the globe

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    Peer reviewed. Β©2015. The Authors.This is an open access article under theterms of the Creative CommonsAttribution-NonCommercial-N oDerivsLicense, which permits use and distri-bution in any medium, provided theoriginal work is properly cited, the use isnon-commerc ial and no modificationsor adaptations are made.In this first worldwide synthesis of in situ and satellite-derived lake data, we find that lake summer surface water temperatures rose rapidly (global mean = 0.34Β°C decade 1) between 1985 and 2009. Our analyses show that surface water warming rates are dependent on combinations of climate and local characteristics, rather than just lake location, leading to the counterintuitive result that regional consistency in lake warming is the exception, rather than the rule. The most rapidly warming lakes are widely geographically distributed, and their warming is associated with interactions among different climatic factors β€”from seasonally ice-covered lakes in areas where temperature and solar radiation are increasing while cloud cover is diminishing (0.72Β°C decade 1) to ice-free lakes experiencing increases in air temperature and solar radiation (0.53Β°C decade 1). The pervasive and rapid warming observed here signals the urgent need to incorporate climate impacts into vulnerability assessments and adaptation efforts for lakes

    Rapid and highly variable warming of lake surface waters around the globe

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    peer reviewedIn this first worldwide synthesis of in situ and satellite-derived lake data, we find that lake summer surface water temperatures rose rapidly (global mean = 0.34Β°C decade-1) between 1985 and 2009. Our analyses show that surface water warming rates are dependent on combinations of climate and local characteristics, rather than just lake location, leading to the counterintuitive result that regional consistency in lake warming is the exception, rather than the rule. The most rapidly warming lakes are widely geographically distributed, and their warming is associated with interactions among different climatic factors - from seasonally ice-covered lakes in areas where temperature and solar radiation are increasing while cloud cover is diminishing (0.72Β°C decade-1) to ice-free lakes experiencing increases in air temperature and solar radiation (0.53Β°C decade-1). The pervasive and rapid warming observed here signals the urgent need to incorporate climate impacts into vulnerability assessments and adaptation efforts for lakes. Β© 2015. American Geophysical Union. All Rights Reserved

    Global data set of long-term summertime vertical temperature profiles in 153 lakes

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    peer reviewedClimate change and other anthropogenic stressors have led to long-term changes in the thermal structure, including surface temperatures, deepwater temperatures, and vertical thermal gradients, in many lakes around the world. Though many studies highlight warming of surface water temperatures in lakes worldwide, less is known about long-term trends in full vertical thermal structure and deepwater temperatures, which have been changing less consistently in both direction and magnitude. Here, we present a globally-expansive data set of summertime in-situ vertical temperature profiles from 153 lakes, with one time series beginning as early as 1894. We also compiled lake geographic, morphometric, and water quality variables that can influence vertical thermal structure through a variety of potential mechanisms in these lakes. These long-term time series of vertical temperature profiles and corresponding lake characteristics serve as valuable data to help understand changes and drivers of lake thermal structure in a time of rapid global and ecological change. Β© 2021, The Author(s)

    The unique methodological challenges of winter limnology

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    Winter is an important season for many limnological processes, which can range from biogeochemical transformations to ecological interactions. Interest in the structure and function of lake ecosystems under ice is on the rise. Although limnologists working at polar latitudes have a long history of winter work, the required knowledge to successfully sample under winter conditions is not widely available and relatively few limnologists receive formal training. In particular, the deployment and operation of equipment in below 0 C temperatures pose considerable logistical and methodological challenges, as do the safety risks of sampling during the ice covered period. Here, we consolidate information on winter lake sampling and describe effective methods to measure physical, chemical, and biological variables in and under ice. We describe variation in snow and ice conditions and discuss implications for sampling logistics and safety. We outline commonly encountered methodological challenges and make recommendations for best practices to maximize safety and efficiency when sampling through ice or deploying instruments in ice-covered lakes. Application of such practices over a broad range of ice-covered lakes will contribute to a better understanding of the factors that regulate lakes during winter and how winter conditions affect the subsequent ice-free period

    Synchronous dynamics of zooplankton competitors prevail in temperate lake ecosystems

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    Although competing species are expected to exhibit compensatory dynamics (negative temporal covariation), empirical work has demonstrated that competitive communities often exhibit synchronous dynamics (positive temporal covariation). This has led to the suggestion that environmental forcing dominates species dynamics; however, synchronous and compensatory dynamics may appear at different length scales and/or at different times, making it challenging to identify their relative importance. We compiled 58 long-term datasets of zooplankton abundance in north-temperate and subtropical lakes and used wavelet analysis to quantify general patterns in the times and scales at which synchronous/compensatory dynamics dominated zooplankton communities in different regions and across the entire dataset. Synchronous dynamics were far more prevalent at all scales and times and were ubiquitous at the annual scale. Although we found compensatory dynamics in approximately 14% of all combinations of time period/scale/ lake, there were no consistent scales or time periods during which compensatory dynamics were apparent across different regions. Our results suggest that the processes driving compensatory dynamics may be local in their extent, while those generating synchronous dynamics operate at much larger scales. This highlights an important gap in our understanding of the interaction between environmental and biotic forces that structure communities. Β© 2014 The Author(s) Published by the Royal Society. All rights reserved
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