Excessive amounts of melanin pigments may hamper histopathological assessments of melanocytic lesions by obscuring cellular morphology and hindering antibody-antigen interactions. To determine the optimal melanin-bleaching conditions for histopathological examination, heavily pigmented melanomas were treated with warm hydrogen peroxide (H2O2) diluted with various diluents (1% disodium hydrogen phosphate 12H2O (Na2 HPO4); phosphate buffer 0.05 M, pH 7.4 (PB); and PBS 0.05 M, pH 7.4) at varying temperatures (50°C, 55°C, and 60°C) and for varying incubation times (0.5, 1, 2, and 3 h). The effect of the sequential order of antigen retrieval and bleaching on preserving tissue morphology was then evaluated. Additionally, the effect of melanin bleaching using warm diluted H2O2 on the antigenicity of melanoma-related markers (HMB-45, MART-1, and S-100) and other markers used for histopathology was examined in amelanotic melanomas and tonsil tissue. Optimal and complete bleaching was achieved using warm 3% H2O2 in PB treatment at 55°C for 2 h following antigen retrieval with microwaving or digestion with trypsin. Under these conditions, the tissue morphology and antigenicity of various immunohistochemical markers were also well preserved. Bleaching with warm 3% H2O2 PB is a fast and efficient method of bleaching melanin pigments and performing immunohistochemical examination in heavily melanin-pigmented lesions.
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http://dx.doi.org/10.1111/j.1440-1827.2011.02667.x | DOI Listing |
Glob Chang Biol
December 2024
Department of Geography, University of British Columbia, Vancouver, British Columbia, Canada.
Warm-season marine heatwaves (MHWs) have greatly increased in frequency, severity, and extent over the last few decades, driving more frequent and severe coral bleaching episodes. Given the grave near-term threat to coral reefs imposed by MHWs, it is important to assess the mechanisms by which corals may acquire higher thermal tolerance. Recent field and laboratory studies have demonstrated that exposure to sublethal heat stress, known as "priming," can reduce bleaching susceptibility during a subsequent MHW.
View Article and Find Full Text PDFJ Sci Food Agric
January 2025
School of Science, Monash University Malaysia, Bandar Sunway, Malaysia.
Background: The present study evaluated the effects of temperature, pH, light and chemical oxidation on fucoxanthin changes in terms of colour, antioxidant activity and metabolomic profile. Additionally, the correlation between antioxidant activity and identified metabolites was analysed.
Results: It was found that colour change was significantly reduced at elevated heat (100 °C, *∆E = 0.
Sci Total Environ
November 2024
Climate Geochemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany.
Elevated sea surface temperatures are causing an increase in coral bleaching events worldwide, and represent an existential threat to coral reefs. Early studies of Mesophotic Coral Ecosystems (MCEs) highlighted their potential as thermal refuges for shallow-water coral species in the face of predicted 21 century warming. However, recent genetic evidence implies that limited ecological connectivity between shallow- and deep-water coral communities inhibits their effectiveness as refugia; instead MCEs host distinct endemic communities that are ecologically significant in and of themselves.
View Article and Find Full Text PDFMicrob Ecol
July 2024
Department of Biological Sciences, National University of Singapore, Singapore, Singapore.
PLoS One
March 2024
ENTROPIE, IRD, Université de la Réunion, CNRS, IFREMER, Université de Nouvelle-Calédonie, Nouméa, New Caledonia.
Widespread coral bleaching has generally been linked to high water temperatures at larger geographic scales. However, the bleaching response can be highly variable among individual of the same species, between different species, and across localities; what causes this variability remains unresolved. Here, we tracked bleached and non-bleached colonies of Acropora muricata to see if they recovered or died following a stress event inside the semi-enclosed lagoon of Bouraké (New Caledonia), where corals are long-term acclimatized to extreme conditions of temperature, pH and dissolved oxygen, and at a nearby control reef where conditions are more benign.
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