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1.
Molecular profiling of normal tissues is a regular and necessary step when developing systems for expression analyses in biological samples, including diagnostic panels for various diseases and conditions. Yet there are still no rigorous criteria to allow precise typing of normal tissues. A main problem is that the methods employed in diagnostic expression testing are difficult to standardize. While various technologies, instruments, and reagents are available, universal protocols of handling biological material are lacking, thus impairing the reproducibility of data from independent studies. The review describes a new approach to standardizing circulating microRNA studies in forensic biology, which has relatively recently (7–8 years ago) come to employ RNA markers in molecular typing of tissues and biological fluids. Forensic biology is now one of the few disciplines where several panels of tissue mRNA markers have been developed within a short period of time and a number of specific microRNA markers have been established and validated for several biological fluids. To allow their successful use, new protocols have been combined with the available, rigidly standardized system of genetic personal identification. Although a ready diagnostic product has still not been obtained with this well-working approach, the apparent efficiency of the standardization methods clearly demonstrates that the problem is possible to solve in other biomedical fields, including those where RNA-based diagnostic protocols are still under development.  相似文献   
2.

Uxmal and Tulum are two important Mayan sites in the Yucatan peninsula. The buildings are mainly composed of limestone and grey/black discoloration is seen on exposed walls and copious greenish biofilms on inner walls. The principal microorganisms detected on interior walls at both Uxmal and Tulum were cyanobacteria; heterotrophic bacteria and filamentous fungi were also present. A dark‐pigmented mitosporic fungus and Bacillus cereus, both isolated from Uxmal, were shown to be acidogenic in laboratory cultures. Cyanobacteria belonging to rock‐degrading genera Synechocystis and Gloeocapsa were identified at both sites. Surface analysis previously showed that calcium ions were present in the biofilms on buildings at Uxmal and Tulum, suggesting the deposition of biosolubilized stone. Apart from their potential to degrade the substrate, the coccoid cyanobacteria supply organic nutrients for bacteria and fungi, which can produce organic acids, further increasing stone degradation.  相似文献   
3.
DNA microchip technology is a rapid, high-throughput method for nucleic acid hybridization reactions. This technology requires random fragmentation and fluorescent labeling of target nucleic acids prior to hybridization. Radical-generating coordination complexes, such as 1,10-phenanthroline-Cu(II) (OP-Cu) and Fe(II)-EDTA (Fe-EDTA), have been commonly used as sequence nonspecific "chemical nucleases" to introduce single-strand breaks in nucleic acids. Here we describe a new method based on these radical-generating complexes for random fragmentation and labeling of both single- and double-stranded forms of RNA and DNA. Nucleic acids labeled with the OP-Cu and the Fe-EDTA protocols revealed high hybridization specificity in hybridization with DNA microchips containing oligonucleotide probes selected for identification of 16S rRNA sequences of the Bacillus group microorganisms.We also demonstrated cDNA- and cRNA-labeling and fragmentation with this method. Both the OP-Cu and Fe-EDTA fragmentation and labeling procedures are quick and inexpensive compared to other commonly used methods. A column-based version of the described method does not require centrifugation and therefore is promising for the automation of sample preparations in DNA microchip technology as well as in other nucleic acid hybridization studies.  相似文献   
4.
Perry  CT  Kench  PS  Smithers  SG  Riegl  BR  Gulliver  P  Daniells  JJ 《Coral reefs (Online)》2017,36(3):1013-1021

Low-lying coral reef islands are considered highly vulnerable to climate change, necessitating an improved understanding of when and why they form, and how the timing of formation varies within and among regions. Several testable models have been proposed that explain inter-regional variability as a function of sea-level history and, more recently, a reef platform size model has been proposed from the Maldives (central Indian Ocean) to explain intra-regional (intra-atoll) variability. Here we present chronostratigraphic data from Pipon Island, northern Great Barrier Reef (GBR), enabling us to test the applicability of existing regional island evolution models, and the platform size control hypothesis in a Pacific context. We show that reef platform infilling occurred rapidly (~4–5 mm yr−1) under a “bucket-fill” type scenario. Unusually, this infilling was dominated by terrigenous sedimentation, with platform filling and subsequent reef flat formation complete by ~5000 calibrated years BP (cal BP). Reef flat exposure as sea levels slowly fell post highstand facilitated a shift towards intertidal and subaerial-dominated sedimentation. Our data suggest, however, a lag of ~1500 yr before island initiation (at ~3200 cal BP), i.e. later than that reported from smaller and more evolutionarily mature reef platforms in the region. Our data thus support: (1) the hypothesis that platform size acts to influence the timing of platform filling and subsequent island development at intra-regional scales; and (2) the hypothesis that the low wooded islands of the northern GBR conform to a model of island formation above an elevated reef flat under falling sea levels.

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5.
The Peranakan Chinese are culturally unique descendants of immigrants from China who settled in the Malay Archipelago ∼300–500 years ago. Today, among large communities in Southeast Asia, the Peranakans have preserved Chinese traditions with strong influence from the local indigenous Malays. Yet, whether or to what extent genetic admixture co-occurred with the cultural mixture has been a topic of ongoing debate. We performed whole-genome sequencing (WGS) on 177 Singapore (SG) Peranakans and analyzed the data jointly with WGS data of Asian and European populations. We estimated that Peranakan Chinese inherited ∼5.62% (95% confidence interval [CI]: 4.76–6.49%) Malay ancestry, much higher than that in SG Chinese (1.08%, 0.65–1.51%), southern Chinese (0.86%, 0.50–1.23%), and northern Chinese (0.25%, 0.18–0.32%). A sex-biased admixture history, in which the Malay ancestry was contributed primarily by females, was supported by X chromosomal variants, and mitochondrial (MT) and Y haplogroups. Finally, we identified an ancient admixture event shared by Peranakan Chinese and SG Chinese ∼1,612 (95% CI: 1,345–1,923) years ago, coinciding with the settlement history of Han Chinese in southern China, apart from the recent admixture event with Malays unique to Peranakan Chinese ∼190 (159–213) years ago. These findings greatly advance our understanding of the dispersal history of Chinese and their interaction with indigenous populations in Southeast Asia.  相似文献   
6.
DNA/RNA methylation plays an important role in lung cancer initiation and progression. Liquid biopsy makes use of cells, nucleotides and proteins released from tumor cells into body fluids to help with cancer diagnosis and prognosis. Methylation of circulating tumor DNA (ctDNA) has gained increasing attention as biomarkers for lung cancer. Here we briefly introduce the biological basis and detection method of ctDNA methylation, and review various applications of methylated DNA in body fluids in lung cancer screening, diagnosis, prognosis, monitoring and treatment prediction. We also discuss the emerging role of RNA methylation as biomarkers for cancer.  相似文献   
7.
A high-resolution map for the arrangement of histones along DNA in the nucleosome core particles has been determined by a new sequencing procedure. The lysine groups of histones were crosslinked to partly depurinated DNA at neutral pH. One strand of DNA was split at the points of crosslinking, thus leaving the 5′-terminal DNA fragments bound to histones. The lengths of these crosslinked DNA fragments were measured to determine the position of histones on one strand of the core DNA from its 5′ end.The results demonstrate that histones are bound to regularly arranged, discrete DNA segments about six nucleotides long. These segments are separated by histone-free gaps about four nucleotides wide located at a distance of about 10n nucleotides from the 5′ end of DNA. The first 20 nucleotides from the 5′ ends of DNA seem to be free of histones. Histones appear to be arranged symmetrically and in a similar way on both DNA strands. Any one histone, being bound predominantly to discrete segments on one or other of the strands, can oscillate at the same time between the two strands across the major DNA groove. Two symmetrical models for the arrangement of two molecules of each core histone on linearized and folded DNA are proposed.  相似文献   
8.
The sequential arrangement of histones along DNA in nucleosomes containing all five histones and DNA about 165 and 175 base-pairs in length has been determined. The data provide evidence that core histones (H2A, H2B, H3 and H4) are arranged in nucleosomes and nucleosome core particles in a largely similar way with the following differences. (1) On nucleosomal DNA about 175 basepairs long core histones are probably shifted by 20 nucleotides on one DNA strand and by 10 nucleotides on the complementary DNA strand from the 5′ end. On nucleosomal DNA 165 base-pairs long, histones appear to be shifted by 10 nucleotides from the 5′ end of DNA on both the DNA strands. (2) Histone H3 is extended beyond core DNA and is bound to the 3′ end of DNA about 175 nucleotides long. Thus, core histones span the whole length of nucleosomal DNA. (3) Histone H2A seems to be absent from the central region of nucleosomal DNA. These results indicate that during the preparation of core particles, some rearrangement of histones or some of their regions occurs.Histone H1 has been shown to be bound mainly to the ends of nucleosomal DNA and, along the whole DNA length, to the gap regions that are free of core histones.  相似文献   
9.
10.
The sequential arrangement of histones along DNA in nucleosome core particles was determined between 0.5 and 600 mM salt and from 0 to 8 M urea. These concentrations of salt and urea up to 6 M had no significant effect on the linear order of histones along DNA but 8 M urea caused the rearrangement of histones. Conformational changes in cores have been identified within these ranges of conditions by several laboratories 8-21. Also, abrupt structural changes in the cores, apparently their unfolding, were found by gel electrophoresis to occur at urea concentration, between 4 and 5 M. 600 mM salt and 6 M urea were shown to relax the binding of histones to DNA in cores but do not however release histones or some part of their molecules from DNA. It appears therefore that nucleosomal cores can undergo some conformational transitions and unfolding whereas their primary organization remains essentially unaffected. These results are consistent with a model of the core particles in which the histone octamer forms something like a helical "rim" along the superhelical DNA and histone-histone interactions beyond the "rim" are rather weak in comparison with those within the "rim".  相似文献   
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