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5-hydroxymethyluracil (hmU) is an oxidative DNA lesion and a potential intermediate in DNA repair–coupled DNA demethylation pathways. Isotopic labeling and MS reveal that hmU is produced directly by Tet-mediated oxidation of thymine in mouse embryonic stem cells, suggesting a functional role for hmU in stem cells. Ten eleven translocation (Tet) enzymes oxidize the epigenetically important DNA base 5-methylcytosine (mC) stepwise to 5-hydroxymethylcytosine (hmC), 5-formylcytosine and 5-carboxycytosine. It is currently unknown whether Tet-induced oxidation is limited to cytosine-derived nucleobases or whether other nucleobases are oxidized as well. We synthesized isotopologs of all major oxidized pyrimidine and purine bases and performed quantitative MS to show that Tet-induced oxidation is not limited to mC but that thymine is also a substrate that gives 5-hydroxymethyluracil (hmU) in mouse embryonic stem cells (mESCs). Using MS-based isotope tracing, we show that deamination of hmC does not contribute to the steady-state levels of hmU in mESCs. Protein pull-down experiments in combination with peptide tracing identifies hmU as a base that influences binding of chromatin remodeling proteins and transcription factors, suggesting that hmU has a specific function in stem cells besides triggering DNA repair.

Hypermethylation of the promoters of tumour suppressor genes represses transcription of these genes, conferring growth advantages to cancer cells. How these changes arise is poorly understood. Here we show that the activity of oxygen-dependent ten-eleven translocation (TET) enzymes is reduced by tumour hypoxia in human and mouse cells. TET enzymes catalyse DNA demethylation through 5-methylcytosine oxidation. This reduction in activity occurs independently of hypoxia-associated alterations in TET expression, proliferation, metabolism, hypoxia-inducible factor activity or reactive oxygen species, and depends directly on oxygen shortage. Hypoxia-induced loss of TET activity increases hypermethylation at gene promoters in vitro . In patients, tumour suppressor gene promoters are markedly more methylated in hypoxic tumour tissue, independent of proliferation, stromal cell infiltration and tumour characteristics. Our data suggest that up to half of hypermethylation events are due to hypoxia, with these events conferring a selective advantage. Accordingly, increased hypoxia in mouse breast tumours increases hypermethylation, while restoration of tumour oxygenation abrogates this effect. Tumour hypoxia therefore acts as a novel regulator of DNA methylation. Genes silenced by hypoxia Tumours are epigenetically distinct from their tissue of origin, frequently showing increased DNA methylation of tumour suppressor gene promoters, but how these changes arise is poorly understood. Here, Diether Lambrechts and colleagues report that tumour hypoxia, pervasive in many solid tumours, reduces the activity of the oxygen-dependent ten-eleven translocation (TET) enzymes, which catalyse DNA demethylation through 5-methylcytosine oxidation. They show that oxygen is an important co-factor for TET activity, and hypoxia-induced loss of TET activity increases hypermethylation at gene promoters in vitro and at tumour suppressor genes in hypoxic tumours. The authors propose that tumour hypoxia directly reduces TET activity, leading to changes in DNA methylation and silencing gene expression. Countering hypermethylation by inhibiting DNA methylation or by normalizing tumour blood supply may therefore be of therapeutic benefit.

Tet enzymes oxidize 5-methyl-deoxycytidine (mdC) to 5-hydroxymethyl-dC (hmdC), 5-formyl-dC (fdC) and 5-carboxy-dC (cadC) in DNA. It was proposed that fdC and cadC deformylate and decarboxylate, respectively, to dC over the course of an active demethylation process. This would re-install canonical dC bases at previously methylated sites. However, whether such direct C-C bond cleavage reactions at fdC and cadC occur in vivo remains an unanswered question. Here we report the incorporation of synthetic isotope- and (R)-2'-fluorine-labeled dC and fdC derivatives into the genome of cultured mammalian cells. Following the fate of these probe molecules using UHPLC-MS/MS provided quantitative data about the formed reaction products. The data show that the labeled fdC probe is efficiently converted into the corresponding labeled dC, most likely after its incorporation into the genome. Therefore, we conclude that fdC undergoes C-C bond cleavage in stem cells, leading to the direct re-installation of unmodified dC.

From the earliest observations of ozone in the lower atmosphere in the 19th century, both measurement methods and the portion of the globe observed have evolved and changed. These methods have different uncertainties and biases, and the data records differ with respect to coverage (space and time), information content, and representativeness. In this study, various ozone measurement methods and ozone datasets are reviewed and selected for inclusion in the historical record of background ozone levels, based on relationship of the measurement technique to the modern UV absorption standard, absence of interfering pollutants, representativeness of the well-mixed boundary layer and expert judgement of their credibility. There are significant uncertainties with the 19th and early 20th-century measurements related to interference of other gases. Spectroscopic methods applied before 1960 have likely underestimated ozone by as much as 11% at the surface and by about 24% in the free troposphere, due to the use of differing ozone absorption coefficients. There is no unambiguous evidence in the measurement record back to 1896 that typical mid-latitude background surface ozone values were below about 20 nmol mol–1, but there is robust evidence for increases in the temperate and polar regions of the northern hemisphere of 30–70%, with large uncertainty, between the period of historic observations, 1896–1975, and the modern period (1990–2014). Independent historical observations from balloons and aircraft indicate similar changes in the free troposphere. Changes in the southern hemisphere are much less. Regional representativeness of the available observations remains a potential source of large errors, which are difficult to quantify. The great majority of validation and intercomparison studies of free tropospheric ozone measurement methods use ECC ozonesondes as reference. Compared to UV-absorption measurements they show a modest (~1–5% ±5%) high bias in the troposphere, but no evidence of a change with time. Umkehr, lidar, and FTIR methods all show modest low biases relative to ECCs, and so, using ECC sondes as a transfer standard, all appear to agree to within one standard deviation with the modern UV-absorption standard. Other sonde types show an increase of 5–20% in sensitivity to tropospheric ozone from 1970–1995. Biases and standard deviations of satellite retrieval comparisons are often 2–3 times larger than those of other free tropospheric measurements. The lack of information on temporal changes of bias for satellite measurements of tropospheric ozone is an area of concern for long-term trend studies.