Vô sinh là gì? Các công bố khoa học về Vô sinh

The raised coral reef sequences at Kish Island provide a rare window into the depositional setting and paleoenvironment of a high-latitude, shallow-water coral reef that developed under turbid conditions in the Persian Gulf during Marine Isotope Stage 7 (~200 to 250 ka). Six sedimentary facies and eight foraminiferal assemblages can be identified throughout the sequence. A ninth assemblage can be defined for the modern subtidal realm. At the base of the sequence is a marl rich in hyaline foraminifera (Elphidium, Ammonia, Asterorotalia, Bulimina, Nonion, and Quinqueloculina) and ostracods, which was deposited in about 30–40 m water depth in a turbid deltaic setting. Shallowing resulted in the marl becoming sandy, and changing to a mollusc-rich facies with rare foraminifera (mostly smaller miliolid taxa) that formed the substrate for coral recruitment. The coral marl layer contains many large corals embedded in situ in an aggregate and coralline algae-rich marl. Two abundance peaks in the foraminifera occur at the base and mid-way through this layer, which also correspond to a change from Murrayinella-dominated to Placopsilina-dominated assemblages, indicating deepening and more open-marine conditions, but elevated turbidity. Towards the top of the layer, abundance of foraminifera decreases and miliolid foraminifera become dominant. The top-most layer is dominated by coral and mollusc fragments and has an Amphistegina-rich reef-related assemblage. Of the Late Pleistocene foraminiferal assemblages, the Murrayinella-, Pararotalia-, and Placopsilina-dominated assemblages are no longer present in the modern gulf for unknown reasons. Of the other five assemblages, only the Amphistegina assemblage is found within proximity to the modern Kish Island. The Elphidium and Asterorotalia-Bulimina assemblages are from deeper areas of the gulf. The Ammonia and Quinqueloculina assemblages occur in lagoonal sediments on the Arabian side of the gulf. Like the modern Persian Gulf, the diversity of foraminifera was low (~80 common species) during the Pleistocene and does not correlate with foraminiferal abundance.

We construct Laplace invariants for an equation with a dominating fourth partial derivative. The determining equations are written out in terms of the Laplace invariants. We single out classes of equations admitting four-dimensional Lie algebras.

To derive a more precise estimation of the relationship between miR-499 rs3746444 polymorphism (A>G) and cancer risk, a meta-analysis was performed. A total of 9 studies including 6,077 cases and 7,199 controls were involved in this meta-analysis. Overall, no significantly elevated cancer risk was associated with miR-499 G allele when all studies were pooled into the meta-analysis (AG vs. AA: OR = 1.14, 95 % CI = 0.98–1.32; GG vs. AA: OR = 1.12, 95 % CI = 0.95–1.33; dominant model: OR = 1.13, 95 % CI = 0.99–1.29; recessive model: OR = 1.05, 95 % CI = 0.83–1.33). In the subgroup analysis by ethnicity, significantly increased risk was only found for Asians (dominant model: OR = 1.22, 95 % CI = 1.02–1.46). When stratified by study design, no statistically significantly elevated risks were found in hospital-based studies or population-based studies. In the subgroup analysis by cancer type, significant cancer risk change was only found for breast cancer when miR-499 G allele was included (dominant model: OR = 1.13, 95 % CI = 1.01–1.26). In conclusion, this meta-analysis suggests that the miR-499 rs3746444 polymorphism (A>G) is a low-penetrant risk factor for cancer development among Asians and may contribute to breast cancer susceptibility.