The Different Artificial Sweeteners and Their Effects on Endothelial Cell/Blood Vessel Health: Possible Implications for Ringing in the Ear

Abstract: Background: Tinnitus, a condition whose remarkable symptom is ringing in the ear (RIE), is a problem plaguing people all around the world in varying degrees of severity, though it is most common and severe in older populations. Literature is lacking on its etiology. Therefore, it is difficult to diagnose and treat. Several possible components could play a role in the development of tinnitus including neurological, physiological, traumatic, dietary and vascular factors. No factor has yet been definitively linked to the development of tinnitus. Vascular health can be significantly impacted by diet- especially in regard to sugars. As artificial sweeteners are used widely in the American diet, they may play a significant role in vascular health. Objective: This project aims to investigate a possible connection between artificial sugars’ impact on vascular health and complaints of RIE among age groups through a patient survey and laboratory experiments. Methods: A survey assessing individuals’ demographic information, subjective severity of RIE and reported artificial sweetener consumption will be distributed to audiologists’ offices in major Ohio cities, via Qualtrics, where patients will complete them. Data collected will be analyzed for interrelationships among sugar intake, age and severity of RIE. In the laboratory, an ELISA assay will evaluate the effects of artificial sweeteners on endothelial cells- the same cells that comprise blood vessels- through quantifying stimulation of the Tie-2 survival and angiogenesis pathway via the cellular messenger pAKT

A Mississippian black shale record of redox oscillation in the Craven Basin, UK

Early diagenetic redox oscillation processes have been rarely recognised in the ancient rock record but potentially exert an important control on mineral authigenesis, hydrocarbon prospectivity and supply of metals and/or reduced S as part of associated mineral systems. The upper unit of the Mississippian Bowland Shale Formation is a candidate record of diagenetic redox oscillation processes because it was deposited under a relatively high sediment accumulation rate linked to a large delta system, and under dominantly anoxic and intermittently sulphidic bottom-water conditions. In order to characterise the syngenetic and early diagenetic processes, sedimentological and geochemical data were integrated through the Upper Bowland Shale at three sites in the Craven Basin (Lancashire, UK). Organic matter (OM) comprises a mixture of Type II, II-S, II/III and III OM. ‘Redox zones’ are defined by patterns of Fe-speciation and redox-sensitive trace element enrichment and split into two groups. ‘Sulphidic’ zones (EUX, AN-III, AN-I and AN-IT) represent sediments deposited under conditions of at least intermittently active sulphate-reduction in bottom-waters. ‘Non-sulphidic’ zones (OX-RX, OX-F and OX) represent sediments deposited under non-sulphidic (oxic to ferruginous anoxic) bottom-waters. Operation of a shelf-to-basin ‘reactive Fe’ (FeHR) shuttle, moderated by sea level fluctuation and delta proximity, controlled the position and stability of redoxclines between zones of Fe and sulphate reduction, and methanogenesis. Early diagenetic redoxclines were capable of migration through the shallow sediment column relatively quickly, in response to sea level fluctuation. Preservation of syngenetic and early diagenetic geochemical signals shows redoxclines between Fe and sulphate reduction, and the upper boundary of sulphate-methane transition zone, were positioned within decimetres (i.e., 10 s cm) of seabed. Falling sea level and increasing FeHR supply is recognised as a switch from zones EUX (high sea level), AN-III and ultimately AN-I and AN-IT (low sea level). Zone AN-I defines the operation of ‘redox oscillation’, between zones of Fe and sulphate reduction in shallow porewaters, associated with enhanced degradation of OM and complete dissolution of primary carbonate. Preservation of OM and carbonate, in this system, was a function of changing bottom and pore water redox processes. Redox oscillation operated in a siliciclastic, prodeltaic environment associated with a relatively high sediment accumulation rate and high loadings of labile organic matter and metal oxides. These findings are important for understanding Late Palaeozoic black shales in the context of hydrocarbon and mineral systems