7. MINERAL ELEMENTS RELATED to CARDIOVASCULAR HEALTH Leslie M
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Role of Trace Minerals in Animal Production
ROLE OF TRACE MINERALS IN ANIMAL PRODUCTION What Do I Need to Know About Trace Minerals for Beef and Dairy Cattle, Horses, Sheep and Goats? Connie K. Larson, Ph.D. Research Nutritionist, Zinpro Corporation Eden Praire, MN 55344 Presented at the 2005 Nutrition Conference sponsored by Department of Animal Science, UT Extension and University Professional and Personal Development The University of Tennessee. Introduction The role of trace minerals in animal production is an area of strong interest for producers, feed manufactures, veterinarians and scientists. Adequate trace mineral intake and absorption is required for a variety of metabolic functions including immune response to pathogenic challenge, reproduction and growth. Mineral supplementation strategies quickly become complex because differences in trace mineral status of all livestock and avian species is critical in order to obtain optimum production in modern animal production systems. Subclinical or marginal deficiencies may be a larger problem than acute mineral deficiency because specific clinical symptoms are not evident to allow the producer to recognize the deficiency; however, animals continue to grow and reproduce but at a reduced rate. As animal trace mineral status declines immunity and enzyme functions are compromised first, followed by a reduction in maximum growth and fertility, and finally normal growth and fertility decrease prior to evidence of clinical deficiency (Figure 1; Fraker, 1983; Wikse 1992). In order to maintain animals in adequate trace mineral status, balanced intake and absorption are necessary. Figure 1. Effect of declining trace mineral status on animal performance Mineral Status Immunity & Enzyme Function Adequate Maximum Growth/Fertility Normal Growth/Fertility Clinical Signs Subclinical Clinical Trace Mineral Function To better understand the role of trace minerals in animal production it is important to recognize that trace elements are functional components of numerous metabolic events. -
Effect of Captopril on Post-Infarction Remodelling Visualized by Light
www.nature.com/scientificreports OPEN Efect of captopril on post‑infarction remodelling visualized by light sheet microscopy and echocardiography Urmas Roostalu1*, Louise Thisted1, Jacob Lercke Skytte1, Casper Gravesen Salinas1, Philip Juhl Pedersen1, Jacob Hecksher‑Sørensen1, Bidda Rolin1,3, Henrik H. Hansen1, James G. MacKrell2, Robert M. Christie2, Niels Vrang1, Jacob Jelsing1 & Nora Elisabeth Zois1 Angiotensin converting enzyme inhibitors, among them captopril, improve survival following myocardial infarction (MI). The mechanisms of captopril action remain inadequately understood due to its diverse efects on multiple signalling pathways at diferent time periods following MI. Here we aimed to establish the role of captopril in late‑stage post‑MI remodelling. Left anterior descending artery (LAD) ligation or sham surgery was carried out in male C57BL/6J mice. Seven days post‑surgery LAD ligated mice were allocated to daily vehicle or captopril treatment continued over four weeks. To provide comprehensive characterization of the changes in mouse heart following MI a 3D light sheet imaging method was established together with automated image analysis workfow. The combination of echocardiography and light sheet imaging enabled to assess cardiac function and the underlying morphological changes. We show that delayed captopril treatment does not afect infarct size but prevents left ventricle dilation and hypertrophy, resulting in improved ejection fraction. Quantifcation of lectin perfused blood vessels showed improved vascular density in the infarct border zone in captopril treated mice in comparison to vehicle dosed control mice. These results validate the applicability of combined echocardiographic and light sheet assessment of drug mode of action in preclinical cardiovascular research. Although timely primary coronary percutaneous intervention has substantially improved patient survival post myocardial infarction (MI), the ofen-concomitant cardiac dysfunction and heart failure afect a signifcant num- ber of patients. -
Determination of Trace Element Levels in Patients with Burst Fractures
ORIGINAL ARTICLE Determination of trace element levels in patients with burst fractures Shahab Ahmed Salih Gezh, M.D.,1 Abdurrahman Aycan, M.D.,2 Halit Demir, M.D.,1 Cemal Bozlına, M.D.3 1Department of Chemistry, Yüzüncü Yıl University Faculty of Science and Literature, Van-Turkey 2Department of Neurosurgery, Yüzüncü Yıl University Faculty of Medicine, Van-Turkey 3Department of Neurosurgery, Van Training and Research Hospital, Van-Turkey ABSTRACT BACKGROUND: This study aimed to determine trace element levels (Zn, Fe, Mn, Mg, Cu, Cd, Co, and Pb) in patients with burst fractures in Van Province, Turkey. METHODS: The study included a total of 44 participants with no additional pathologies, including 22 patients with burst fractures aged over 18 years who were admitted to the neurosurgery departments at two hospitals between June 15, 2015 and January 20, 2016 and 22 healthy volunteers. Serum samples were obtained from all participants to measure the serum levels of trace and heavy elements, including Mn, Cd, Cu, Pb, Fe, Co and Zn, using atomic absorbance spectrophotometry. RESULTS: The trace element levels of Zn, Mn, Cu, Co, and Mg were significantly lower (p<0.001), whereas those of Fe, Cd, and Pb were significantly higher in the patient group than in the control group. In addition, the levels of Zn, Mn, Cu, Co, and Mg were lower and the levels of Fe, Cd, and Pb were higher in the patient group than in the control group. CONCLUSION: The probability of burst fracture and its causes leading to any injury may be considered as an indicator balance for the concentration of trace elements between the patient group and control group and may also be a risk factor associated with the bone exposed to burst fracture Significant changes in serum levels of Zn, Cd, Mn, Mg, Pb, Fe, Cu and Zn elements can be observed in patients with burst fractures. -
Essential Trace Elements in Human Health: a Physician's View
Margarita G. Skalnaya, Anatoly V. Skalny ESSENTIAL TRACE ELEMENTS IN HUMAN HEALTH: A PHYSICIAN'S VIEW Reviewers: Philippe Collery, M.D., Ph.D. Ivan V. Radysh, M.D., Ph.D., D.Sc. Tomsk Publishing House of Tomsk State University 2018 2 Essential trace elements in human health UDK 612:577.1 LBC 52.57 S66 Skalnaya Margarita G., Skalny Anatoly V. S66 Essential trace elements in human health: a physician's view. – Tomsk : Publishing House of Tomsk State University, 2018. – 224 p. ISBN 978-5-94621-683-8 Disturbances in trace element homeostasis may result in the development of pathologic states and diseases. The most characteristic patterns of a modern human being are deficiency of essential and excess of toxic trace elements. Such a deficiency frequently occurs due to insufficient trace element content in diets or increased requirements of an organism. All these changes of trace element homeostasis form an individual trace element portrait of a person. Consequently, impaired balance of every trace element should be analyzed in the view of other patterns of trace element portrait. Only personalized approach to diagnosis can meet these requirements and result in successful treatment. Effective management and timely diagnosis of trace element deficiency and toxicity may occur only in the case of adequate assessment of trace element status of every individual based on recent data on trace element metabolism. Therefore, the most recent basic data on participation of essential trace elements in physiological processes, metabolism, routes and volumes of entering to the body, relation to various diseases, medical applications with a special focus on iron (Fe), copper (Cu), manganese (Mn), zinc (Zn), selenium (Se), iodine (I), cobalt (Co), chromium, and molybdenum (Mo) are reviewed. -
Incomplete Versus Complete Myocardial Infarction
Henry Ford Hospital Medical Journal Volume 39 Number 3 Article 20 9-1991 Incomplete Versus Complete Myocardial Infarction Mihai Gheorghiade Sidney Goldstein Follow this and additional works at: https://scholarlycommons.henryford.com/hfhmedjournal Part of the Life Sciences Commons, Medical Specialties Commons, and the Public Health Commons Recommended Citation Gheorghiade, Mihai and Goldstein, Sidney (1991) "Incomplete Versus Complete Myocardial Infarction," Henry Ford Hospital Medical Journal : Vol. 39 : No. 3 , 263-264. Available at: https://scholarlycommons.henryford.com/hfhmedjournal/vol39/iss3/20 This Article is brought to you for free and open access by Henry Ford Health System Scholarly Commons. It has been accepted for inclusion in Henry Ford Hospital Medical Journal by an authorized editor of Henry Ford Health System Scholarly Commons. Incomplete Versus Complete Myocardial Infarction Mihai Gheorghiade, MD,* and Sidney Goldstein, MD* Incomplete myocardial infarction (MI), when compared with a complete Ml. is characterized by a small infarct size and a large mass of viable hut jeopardized myocardium within the perfusion zone of the infarct-related vessel that is manifested ctinicalty hy early recurrent infarction. The pathophysiology involves earty spontaneous or thrombolytic reperfusion. Clinical (i.e., residual ischemia), electrocardiographic, and echocardiographic findings and magnitude of serum cardiac enzyme elevatitms should be taken into account in diagnosing an incomplete Ml. (Heniy Ford Hosp MedJ 1991;39:263-4) he observation that the ischemic event associated with on the ECG may not properly identify patients with incomplete Tthrombotic occlusion of the coronary artery can be inter infarction. rupted with thrombolytic therapy has led to the recognition of a When applied to the individual patient, it is therefore more new ischemic syndrome, the incomplete myocardial infarction useful to divide postinfarction patients, regardless of whether or (MI) (1). -
Evidence for a Carbonatite-Influenced Source Assemblage for Intraplate
minerals Article Evidence for a Carbonatite-Influenced Source Assemblage for Intraplate Basalts from the Buckland Volcanic Province, Queensland, Australia Joshua J. Shea * and Stephen F. Foley Department Earth and Planetary Sciences and ARC Centre of Excellence for Core to Crust Fluid Systems, Macquarie University, North Ryde 2109, New South Wales, Australia * Correspondence: [email protected] Received: 20 June 2019; Accepted: 7 September 2019; Published: 10 September 2019 Abstract: Eastern Australia contains a widespread suite of primitive (MgO 7.5 wt.%) intraplate ≥ basaltic provinces, including those sited along the longest continental hotspot track on Earth ( 2000 km), the Cosgrove track. The Buckland volcanic province is the most southerly basaltic ≈ province on the Cosgrove track before a >1600 km stretch that contains only sparse leucitite volcanism. Buckland is also situated just northeast of the edge of thick cratonic lithosphere where it transitions to a thinner continental lithosphere (<110 km) to the east, which may influence the production of plume-derived melts. Here, analysis of minor and trace elements in olivines in alkali basalts and basanites from the Buckland Province are combined with whole-rock compositions to elucidate the mantle source assemblages, and to calibrate minor and trace element indicators in olivine for application to source mineralogy. Olivine xenocrysts show element concentration ranges typical for peridotites; Mn and Al concentrations indicate that the ambient mantle is spinel, rather than garnet, peridotite. High modal pyroxene content is indicated by high Ni, Zn/Fe, and Fe/Mn in olivines, while high Ti/Sc is consistent with amphibole in the source. Residual phlogopite in the source of the basanites is indicated by low K/Nb in whole rocks, while apatite contains high P2O5 and low Rb/Sr ( 0.015) and Sr/La ( 13). -
ST-Elevation Myocardial Infarction Due to Acute Thrombosis in an Adolescent with COVID-19
Prepublication Release ST-Elevation Myocardial Infarction Due to Acute Thrombosis in an Adolescent With COVID-19 Jessica Persson, MD, Michael Shorofsky, MD, Ryan Leahy, MD, MS, Richard Friesen, MD, Amber Khanna, MD, MS, Lyndsey Cole, MD, John S. Kim, MD, MS DOI: 10.1542/peds.2020-049793 Journal: Pediatrics Article Type: Case Report Citation: Persson J, Shorofsky M, Leahy R, et al. ST-elevation myocardial infarction due to acute thrombosis in an adolescent with COVID-19. Pediatrics. 2021; doi: 10.1542/peds.2020- 049793 This is a prepublication version of an article that has undergone peer review and been accepted for publication but is not the final version of record. This paper may be cited using the DOI and date of access. This paper may contain information that has errors in facts, figures, and statements, and will be corrected in the final published version. The journal is providing an early version of this article to expedite access to this information. The American Academy of Pediatrics, the editors, and authors are not responsible for inaccurate information and data described in this version. Downloaded from©202 www.aappublications.org/news1 American Academy by of guest Pediatrics on September 27, 2021 Prepublication Release ST-Elevation Myocardial Infarction Due to Acute Thrombosis in an Adolescent With COVID-19 Jessica Persson, MD1, Michael Shorofsky, MD1, Ryan Leahy, MD, MS1, Richard Friesen, MD1, Amber Khanna, MD, MS1,2, Lyndsey Cole, MD3, John S. Kim, MD, MS1 1Division of Cardiology, Department of Pediatrics, University of Colorado School of Medicine, Aurora, Colorado 2Division of Cardiology, Department of Medicine, University of Colorado School of Medicine, Aurora, Colorado 3Section of Infectious Diseases, Department of Pediatrics, University of Colorado School of Medicine, Aurora, Colorado Corresponding Author: John S. -
Myocardial Infarction Does Not Accelerate Atherosclerosis in a Mouse Model of Type 1 Diabetes
Diabetes Volume 69, October 2020 2133 Myocardial Infarction Does Not Accelerate Atherosclerosis in a Mouse Model of Type 1 Diabetes Farah Kramer,1 Amy M. Martinson,2 Thalia Papayannopoulou,3 and Jenny E. Kanter1 Diabetes 2020;69:2133–2143 | https://doi.org/10.2337/db20-0152 In addition to increasing the risk of an initial myocardial observed in response to the acute ischemic event was pos- infarction (MI), diabetes increases the risk of a recur- tulated to be driven by enhanced extramedullary hemato- rent MI. Previous work suggests that an experimental poiesis resulting in increased levels of circulating monocytes MI can accelerate atherosclerosis via monocytosis. To available for recruitment into the nascent atherosclerotic test whether diabetes and experimental MI synergize to lesion, thereby accelerating atherosclerosis (9). accelerate atherosclerosis, we performed ligation of Diabetes accelerates atherosclerosis lesion initiation and the left anterior descending coronary artery to induce progression and hinders lesion regression in response to experimental MI or sham surgery in nondiabetic and dramatic lipid lowering (10–13). Changes in monocyte and diabetic mice with preexisting atherosclerosis. All mice macrophage phenotype are believed to contribute to the COMPLICATIONS fi subjected to experimental MI had signi cantly reduced acceleration of atherosclerosis in diabetes. In both mouse left ventricular function. In our model, in comparisons and human studies, diabetes results in increased macro- with nondiabetic sham mice, neither diabetes nor MI phage accumulation within the artery wall (10,14,15). For resulted in monocytosis. Neither diabetes nor MI led to example, autopsy and atherectomy samples from humans increased atherosclerotic lesion size, but diabetes ac- celerated lesion progression, exemplified by necrotic have shown that lesions from subjects with diabetes have core expansion. -
NUTRIENTS in DRINKING WATER Manuel Olivares, MD Institute of Nutrition and Food Technology University of Chile Santiago, Chile
4. ESSENTIAL NUTRIENTS IN DRINKING WATER Manuel Olivares, MD Institute of Nutrition and Food Technology University of Chile Santiago, Chile Ricardo Uauy, MD, PhD Institute of Nutrition and Food Technology University of Chile Santiago, Chile London School of Hygiene and Tropical Medicine University of London London, United Kingdom ______________________________________________________________________________________________ I. INTRODUCTION Most of the inorganic chemicals in drinking water are naturally occurring. They are acquired by the contact of water with rocks and soil and the effects of the geological setting, including climate (1-4). However, the chemical composition of drinking water also depends on the contaminating effects of industry, human settlements, agricultural activities and water treatment and distribution (1-4). Depending on water quality at the source, filtration, coagulation, and addition of chemicals to adjust pH and/or control corrosion treatments are employed (1-5). In addition, chlorination or iodination may be used for disinfection and fluoridation for the prevention of dental caries (6-8). Leaching of minerals from metal components used in water treatment plants and plumbing materials occurs when pH and hardness of water are not adjusted. Some of the main sources of dissolved metals include: for Cu- copper or brass plumbing system; Fe- cast iron, steel, and galvanised plumbing system; Zn- zinc galvanised pipes; Ni- chromium- nickel stainless plumbing system; Pb- derived from tin-lead or lead solder; and for Cd- as an impurity in zinc galvanised pipes or cadmium containing solders (1-4,9). Recently, fortification of drinking water has been used in the prevention of iron deficiency in children (10) and to provide iodine in select populations (11). -
WM White Geochemistry Chapter 7: Trace Elements
W. M. White Geochemistry Chapter 7: Trace Elements Chapter 7: Trace Elements in Igneous Processes 7.1 INTRODUCTION n this chapter we will consider the behavior of trace elements, particularly in magmas, and in- troduce methods to model this behavior. Though trace elements, by definition, constitute only a I small fraction of a system of interest, they provide geochemical and geological information out of proportion to their abundance. There are several reasons for this. First, variations in the concentrations of many trace elements are much larger than variations in the concentrations of major components, of- ten by many orders of magnitude. Second, in any system there are far more trace elements than major elements. In most geochemical systems, there are 10 or fewer major components that together account for 99% or more of the system. This leaves 80 trace elements. Each element has chemical properties that are to some degree unique, hence there is unique geochemical information contained in the varia- tion of concentration for each element. Thus the 80 trace elements always contain information not available from the variations in the concentrations of major elements. Third, the range in behavior of trace elements is large and collectively they are sensitive to processes to which major elements are in- sensitive. One example is the depth at which partial melting occurs in the mantle. When the mantle melts, it produces melts whose composition is only weakly dependent on pressure, i.e., it always pro- duces basalt. Certain trace elements, however, are highly sensitive to the depth of melting (because the phase assemblages are functions of pressure). -
Trace Element Studies of the Origin of Igneous Rocks
Downloaded from http://jgs.lyellcollection.org/ by guest on September 29, 2021 Jl geol. Soc. Lond. Vol. 135, 1978, pp. 591-595, 1 table. Printed in Northern Ireland. Conference Report Trace element studies of the origin of igneous rocks W. J. Rea TRACE ELEMENT STUDIES are increasingly im- subject of a paper by Harrison & Wood. portant in igneous petrogenetic investigations in as Mathematical modelling, using geochemical data, much as they place constraints on possible modes of now allows the quantitative assessment of petrogenetic origin of igneous rocks and also give evidence of the processes such as closed and open system fractiona- nature and composition of the mantle/crust systems tion, progressive and single stage partial melting, within which magmas are generated and modified. crystal accumulation and magma mixing (Pearce). The The conference saw trace element studies applied to models, however require valid mineral-liquid partition a wide range of igneous rock compositions, occurring coefficients for the trace elements concerned and there within a wide range of environments. Four papers is sometimes a substantial range in the available litera- were concerned with areas in which basalt lavas pre- ture values. The problem arises mainly because parti- dominate, i.e. Mull (Beckinsale et al.), the islands tion coefficients vary with physical conditions such as associated with the axial trough of the Red Sea (Hen- temperature (Harrison & Wood) and are also heavily derson & Parry), the East Scotia Sea (Saunders & dependent on melt structure which in turn reflects Tarney) where basalts are generated within an intra- chemical parameters such as asio~ and Primo. In this oceanic marginal basin and the South Shetland Islands sense the experimental determination of partition and Antarctic Peninsula (Weaver et al.) where differ- coefficients (Harrison & Wood) is particularly wel- ent periods of magma genesis have been related to come as is any increase in the variety of natural rock subduction and extension. -
Trace-Element Contents of Some Plutonic Rocks of the Sierra Nevada Batholith
Trace-Element Contents of Some Plutonic Rocks of the Sierra Nevada Batholith GEOLOGICAL SURVEY BULLETIN 1114-F t "I A 4 - J Trace-Element Contents of Some Plutonic Rocks of the Sierra Nevada Batholith By F. C. W. DODGE CONTRIBUTIONS TO GEOCHEMISTRY GEOLOGICAL SURVEY BULLETIN 1 3 1 4 - F Summary of available trace-element data giving average data for 20 elements and other data for an additional 26 elements UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 72-600055 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 55 cents (paper cover) Stock Number 2401-2137 CONTENTS Page Abstract ...........-....--.....-.................................-. .......--..-...... Fl Introduction ........................................................................... 1 Abundance and variation of trace elements ................... 2 Changes in trace-element contents across the batholith 5 Discussion ................................................................................ 8 References cited ...................................................................... 12 ILLUSTRATIONS Page PLATE 1. Trace-element concentrations of plutonic rocks, central Sierra Nevada batholith .................................................... in pocket FIGURE 1. Map of central California and western Nevada showing distribution of granitic rocks of the Sierra