molecular thermometers
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2021 ◽  
pp. 2101870
Author(s):  
Albano N. Carneiro Neto ◽  
Ekaterina Mamontova ◽  
Alexandre M. P. Botas ◽  
Carlos D. S. Brites ◽  
Rute A. S. Ferreira ◽  
...  

2021 ◽  
pp. 45-108
Author(s):  
Sivakumar Vaidyanathan ◽  
Priyadarshini Pradhan

The Analyst ◽  
2021 ◽  
Author(s):  
Tianruo Shen ◽  
Xia Wu ◽  
Davin Tan ◽  
Zhaochao Xu ◽  
Xiaogang Liu

Fluorescent thermometers based on organic dyes play an important role in the visualization of dynamic temperature topography with high resolution. Many molecular thermometers contain two fluorophores with different temperature responses...


2018 ◽  
Vol 18 (12) ◽  
pp. 7383-7390 ◽  
Author(s):  
Yan-Jie Qi ◽  
Yong-Jiang Wang ◽  
Xin-Xiong Li ◽  
Dan Zhao ◽  
Yan-Qiong Sun ◽  
...  

2017 ◽  
Vol 56 (20) ◽  
pp. 12186-12192 ◽  
Author(s):  
Dong-Fei Lu ◽  
Zi-Feng Hong ◽  
Jing Xie ◽  
Xiang-Jian Kong ◽  
La-Sheng Long ◽  
...  

2017 ◽  
Vol 36 (1) ◽  
Author(s):  
Seiichi Uchiyama ◽  
Chie Gota

AbstractRecently, numerous luminescent molecular thermometers that exhibit temperature-dependent emission properties have been developed to measure the temperatures of tiny spaces. Intracellular temperature is the most interesting and exciting applications of luminescent molecular thermometers because this temperature is assumed to be correlated with all cell events, such as cell division, gene expression, enzyme reaction, metabolism, and pathogenesis. Among the various types of temperature-dependent emission parameters of luminescent molecular thermometers, the emission intensity ratio at two different wavelengths is suitable for accurate and accessible intracellular temperature measurements. In this review article, luminescent molecular thermometers that exhibit a temperature-dependent emission intensity ratio in living cells are summarized, and current progress in intracellular thermometry is outlined.


The Analyst ◽  
2017 ◽  
Vol 142 (18) ◽  
pp. 3388-3399 ◽  
Author(s):  
Frederik Lermyte ◽  
Frank Sobott

Traveling-wave-dependent ion ‘heating’ is observed during mass spectrometry experiments under both ion mobility and electron transfer dissociation conditions and investigated using novel molecular ‘thermometers’.


2015 ◽  
Vol 12 (1) ◽  
pp. 751-778
Author(s):  
T. Bauersachs ◽  
J. Rochelmeier ◽  
L. Schwark

Abstract. It has been demonstrated that the relative distribution of heterocyst glycolipids (HGs) in cultures of N2-fixing heterocystous cyanobacteria is largely controlled by growth temperature, suggesting a potential use of these components in paleoenvironmental studies. Here, we investigated the effect of environmental parameters (e.g. surface water temperatures, oxygen concentrations and pH) on the distribution of HGs in a natural system using water column filtrates collected from Lake Schreventeich (Kiel, Germany) from late July to the end of October 2013. HPLC-ESI/MS analysis revealed a dominance of 1-(O-hexose)-3,25-hexacosanediols (HG26 diols) and 1-(O-hexose)-3-keto-25-hexacosanol (HG26 keto-ol) in the solvent extracted water column filtrates, which were accompanied by minor abundances of 1-(O-hexose)-3,27-octacosanediol (HG28 diol) and 1-(O-hexose)-3-keto-27-octacosanol (HG28 keto-ol) as well as 1-(O-hexose)-3,25,27-octacosanetriol (HG28 triol) and 1-(O-hexose)-3-keto-25,27-octacosanediol (HG28 keto-diol). Fractional abundances of alcoholic and ketonic HGs generally showed strong linear correlations with surface water temperatures and no or only weak linear correlations with both oxygen concentrations and pH. Changes in the distribution of the most abundant diol and keto-ol (e.g., HG26 diol and HG26 keto-ol) were quantitatively expressed as the HDI26 (heterocyst diol index of 26carbon atoms) with values of this index ranging from 0.89 in mid-August to 0.66 in mid-October. An average HDI26 value of 0.79, which translates into a calculated surface water temperature of 15.8 ± 0.3 °C, was obtained from surface sediments collected from Lake Schreventeich. This temperature – and temperatures obtained from other HG indices (e.g., HDI28 and HTI28) – is similar to the one measured during maximum cyanobacterial productivity in early to mid-September and suggests that HGs preserved in Lake Schreventeich sediments record summer surface water temperatures. As N2-fixing heterocystous cyanobacteria are widespread in present-day freshwater and brackish environments, we conclude that the distribution of HGs in sediments may allow the reconstruction of surface water temperatures of modern and potentially ancient lacustrine settings.


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