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Erratum to: The Accumulation of the REE by Bacterial Fe Oxyhydroxide 细菌氧化铁对稀土元素的富集
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-11-15 DOI: 10.1134/S0016702923210036
S. Felitsyn, N. Alfimova, E. Bogomolov
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引用次数: 0
On the Lithogeochemical Reconstruction of Possible “Geodynamic” Types of Granites-Sources of Arkose Clastic Material 花岗岩可能“地球动力学”类型的岩石地球化学重建——砂岩碎屑物质来源
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-11-15 DOI: 10.1134/S0016702923110071
A. V. Maslov, V. N. Podkovyrov

Abstract—A number of examples are considered in which modern arkose sands as well as arkose and compositionally similar sandstones (all of the above rocks are sediments of the first sedimentation cycle) of different ages have definite provenances composed of granitoids of different “geodynamic” types. The main goal of the work is to analyze how the geochemical characteristics of granitoids are translated into petrogenic sedimentary rocks. The comparison of 245 analyses of sands and sandstones with ~375 analyses of the inferred prototype sources of clastic material showed that the lithogeochemical characteristics of arkose and subarkose sands and sandstones (mainly the HFS element content and ratio) makes it possible in most cases to confidently judge the “geodynamic nature” of source felsic igneous rocks.

摘要:本文考虑了许多不同时代的现代粗砂、粗砂和成分相似的砂岩(以上岩石均为第一次沉积旋回的沉积物)具有由不同“地球动力学”类型的花岗岩组成的明确物源的例子。工作的主要目的是分析花岗岩类的地球化学特征如何转化为成岩沉积岩。245份砂、砂岩分析与375份碎屑物质原型源分析对比表明,粗砂和亚粗砂、砂岩的岩石地球化学特征(主要是HFS元素含量和比值)在大多数情况下可以自信地判断烃源岩长英质火成岩的“地球动力学性质”。
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引用次数: 0
Erratum to: Composition of Phenocrysts in Lamproites of Gaussberg Volcano, East Antarctica 南极东部高斯堡火山煌斑岩中斑晶成分的勘误
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-11-15 DOI: 10.1134/S0016702923210024
N. A. Migdisova, N. M. Sushchevskaya, M. V. Portnyagin, T. A. Shishkina, D. V. Kuzmin, V. G. Batanova
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引用次数: 0
Erratum to: A Stepwise Dissolution Method Applied to Isotopic Chemostratigraphic and Geochronological Studies of Riphean Carbonate Rocks of the Baykit Uplift 逐级溶蚀法应用于巴基特隆起里芬碳酸盐岩同位素化学地层学和年代学研究
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-11-15 DOI: 10.1134/S0016702923200016
I. M. Gorokhov, I. M. Vasil’eva, A. B. Kuznetsov, N. G. Rizvanova, G. V. Konstantinova
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引用次数: 0
Role of Biogeochemical Processes during Groundwater Deferrization 生物地球化学过程在地下水去铁过程中的作用
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-11-15 DOI: 10.1134/S0016702923100075
Z. N. Litvinenko, L. M. Kondratyeva

Abstract—The paper is devoted to the biogeochemical aspects of the treatment of iron-bearing groundwater, which are associated with the formation of biofouling in the pore space around wells after aeration of the aquifer and on technological equipment. Structure and activity characteristics of microbial complexes as a result of pumping groundwater from production and observation wells under changing redox conditions are presented. Scanning electron microscopy was used to study the microstructure and elemental composition of biofilm growths. It has been established that the accumulation of iron and manganese by microbial biomass occurs due to the encrustation of the surface of bacterial cells immersed in a polymer matrix represented by a constant base of three elements: Al, Si, and Ca. The survival of microbial complexes in biofouling is due to the high natural potential and ability to carry out biogeochemical processes in a wide range of oxygen concentrations (aerobic and anaerobic conditions).

摘要:本文从生物地球化学的角度对含铁地下水的处理进行了研究。含铁地下水与含水层曝气后井周围孔隙空间中生物污垢的形成有关,并在工艺设备上进行了探讨。本文介绍了在不同氧化还原条件下从生产井和观测井抽取地下水所产生的微生物复合物的结构和活性特征。利用扫描电子显微镜研究了生物膜生长的微观结构和元素组成。已经确定,微生物生物量对铁和锰的积累是由于细菌细胞表面的结壳,这些细菌细胞浸泡在由三种元素(Al, Si和Ca)组成的恒定碱的聚合物基质中。微生物复合物在生物污垢中的生存是由于其高自然电位和在大范围的氧浓度(好氧和厌氧条件)下进行生物地球化学过程的能力。
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引用次数: 0
Theoretical and Methodological Approaches to the Analysis of the Spatial Distribution of Endemic Diseases of Geochemical Nature 地球化学性质地方病空间分布分析的理论和方法论途径
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-10-25 DOI: 10.1134/S0016702923100063
E. M. Korobova, V. S. Baranchukov, L. I. Kolmykova

Throughout millions of years of geological history (in the Phanerozoic), the coevolution of all living organisms took place in a fierce competition for resources and opportunities for the maximum reproduction. Due to the geochemical heterogeneity of the primary (pre-Quaternary) biosphere, this resulted in a self-regulating system of ecological niches, within which all local biocenoses and their animal and plant species were maximally adapted to the parameters of the habitat. However, with the emergence of reason, the situation changed fundamentally. Human beings became the dominant species and began the conscious development of new territories, including geochemically unfavorable ones, which led to the formation of zones of stable endemic diseases. Based on this premise, for all existing species, there should be areas with physiologically optimal habitat conditions, i.e., those under which the species has evolved to its present state. It follows that, by being able to record the geochemical parameters of the undisturbed biosphere, it is possible to obtain characteristics that are ecologically ideal for local animal and plant species. In theoretical terms, this allowed us to put forward the hypothesis that by fixing the difference between observed and ideal geochemical conditions, it is possible to build maps of risk of diseases of geochemical nature, including in areas subjected to anthropogenic pollution. The paper outlines the methodology and gives examples of construction of such maps. The obtained results can have an important practical value in organizing the system of sanitary–epidemiological service, in solving the problems of liquidation of the consequences of anthropogenic pollution, and in carrying out preventive measures to minimize the risk of diseases of geochemical nature.

在数百万年的地质历史中(显生宙),所有生物的共同进化都是在争夺资源和最大繁殖机会的激烈竞争中进行的。由于原生(前第四纪)生物圈的地球化学异质性,这导致了生态位的自我调节系统,在该系统中,所有当地生物群落及其动植物物种都能最大限度地适应栖息地的参数。然而,随着理性的出现,情况发生了根本性的变化。人类成为优势物种,并开始有意识地开发新的领土,包括地球化学上不利的领土,这导致了稳定的地方病区域的形成。基于这一前提,对于所有现有物种,都应该有生理上最佳的栖息地条件,即物种进化到目前状态的区域。因此,通过能够记录未受干扰生物圈的地球化学参数,就有可能获得对当地动植物物种生态理想的特征。从理论上讲,这使我们能够提出这样一个假设,即通过确定观测到的和理想的地球化学条件之间的差异,可以绘制地球化学性质疾病的风险地图,包括在遭受人为污染的地区。本文概述了这种地图的构建方法并举例说明。所获得的结果在组织卫生-流行病学服务系统、解决人为污染后果的清理问题以及采取预防措施将地球化学性质疾病的风险降至最低方面具有重要的实际价值。
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引用次数: 0
Local Biogeochemical Cycles of Trace Elements in Agroecosystems of Western Siberia 西伯利亚西部农业生态系统中微量元素的局部生物地球化学循环
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-10-25 DOI: 10.1134/S0016702923100129
A. V. Sindireva

Abstract

The article presents results of long-term (2005–2022) field experiments on studying the distribution and migration of trace elements in the soil–plant–animal system as exemplified by agrocenoses of the southern forested steppe of Western Siberia. A biogeochemical assessment is presented for contents of trace elements (Pb, Cu, Zn, Ni, Cd, Cr, and Se) in the trophic chains under certain agroecological conditions, and geochemical factors affecting the accumulation of trace elements in various types of soils and plants growing on them are analyzed. Normative quantitative characteristics are determined for the effects of trace elements on the chemical composition of the soil, the productivity and quality of the plants of grain and of the fodder and vegetable crops. Relationships between major and trace elements when they enter plants are demonstrated to depend on the levels and ratios of the concentrations of the chemical elements in the soil and the physiological needs of the plant organism during its different ontogenesis stages. The parameters of the intake of trace elements into the body of animals with plant fodder under the conditions of model experiments are established. Structural and functional changes in the animal organs during feeding on crop products grown with different contents of trace elements are analyzed.

摘要——本文介绍了研究微量元素在土壤-植物-动物系统中分布和迁移的长期(2005-2022)田间试验结果,以西西伯利亚南部森林草原的农牧交错带为例。对一定农业生态条件下营养链中微量元素(Pb、Cu、Zn、Ni、Cd、Cr和Se)的含量进行了生物地球化学评价,并分析了影响微量元素在不同类型土壤及其上生长的植物中积累的地球化学因素。确定了微量元素对土壤化学成分、粮食、饲料和蔬菜作物的生产力和质量的影响的规范性定量特征。当主要元素和微量元素进入植物时,它们之间的关系被证明取决于土壤中化学元素浓度的水平和比例,以及植物有机体在其不同个体发生阶段的生理需求。建立了模型实验条件下植物饲料对动物体内微量元素摄入的参数。分析了不同微量元素含量的作物产品在饲养过程中动物器官结构和功能的变化。
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引用次数: 0
Development of V.I. Vernadsky’s Ideas about Natural Waters: Biogeochemical Processes and Water Quality V.I.Vernadsky关于自然水体的思想发展:生物地球化学过程与水质
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-10-25 DOI: 10.1134/S0016702923100087
T. I. Moiseenko

The paper analyzes the effect of ever increasing anthropogenic impacts on land waters and analyzes V.I. Vernadsky’s works on natural waters and their significance for assessing modern biogeochemical processes. The paper demonstrates the scale of the influx of chemical elements and compounds into the modern biosphere as a result of the emission of greenhouse gases, nitrogen and phosphorus dissemination, acid-forming gases, and metals. Key changes in some regions and the biosphere as a whole are highlighted. The consequences of anthropogenically induced processes are illustrated by the example of a remote Arctic region, the northern Kola Peninsula in Russia: the effects of climate warming and the acidification and eutrophication of the waters and their enrichment in metals. In the wake of V.I. Vernadsky’s ideas about the role of land waters in supporting the life necessities of the planet’s human population, approaches to assessing water quality from the standpoint of the ecological paradigm are described.

本文分析了不断增加的人为影响对陆地水域的影响,并分析了V.I.Vernadsky关于自然水域的著作及其对评估现代生物地球化学过程的意义。这篇论文展示了由于温室气体的排放、氮和磷的传播、酸性气体和金属,化学元素和化合物涌入现代生物圈的规模。重点介绍了一些区域和整个生物圈的主要变化。以俄罗斯科拉半岛北部一个偏远的北极地区为例,说明了人为诱发过程的后果:气候变暖、海水酸化和富营养化及其金属富集的影响。根据V.I.Vernadsky关于陆地水域在支持地球人口生活必需品方面的作用的观点,描述了从生态范式的角度评估水质的方法。
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引用次数: 0
Current Development of V.I. Vernadsky’s Biogeochemical Ideas 维尔纳德斯基生物地球化学思想的发展现状
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-10-25 DOI: 10.1134/S001670292310004X
V. V. Ermakov

The paper discusses the core ideas and the development of biogeochemistry as an integrated research avenue in geochemistry and biology created by V.I. Vernadsky. Much attention is paid to the key concepts of biogeochemistry: living matter, the biogenic migration of chemical elements, and the chemical elemental composition of organisms and its ecological significance. The development of the various functions of the biosphere is analyzed: ecological, concentrational, and informational. The differentiation of the chemical elemental composition of organisms is analyzed under conditions when the biosphere is impacted by anthropogenic activities (the development of industries). The role of biogeochemistry is demonstrated with reference to the development of biotechnologies and the elaboration of a biogeochemical indication of the ecological state of biospheric taxons. The progress in biogeochemistry and its current problems are briefly analyzed.

本文讨论了V.I.Vernadsky提出的生物地球化学作为地球化学和生物学综合研究途径的核心思想和发展。人们非常关注生物地球化学的关键概念:生物物质、化学元素的生物迁移、生物的化学元素组成及其生态意义。分析了生物圈的各种功能的发展:生态功能、集中功能和信息功能。在生物圈受到人为活动(工业发展)影响的条件下,分析了生物化学元素组成的分化。生物地球化学的作用是通过生物技术的发展和生物圈分类单元生态状态的生物地球化学指示的阐述来证明的。简要分析了生物地球化学的研究进展及其存在的问题。
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引用次数: 0
Biogeochemical Aspects of Local Interaction in the Society–Nature System at Technogenesis of the Biosphere 生物圈技术起源时社会-自然系统中局部相互作用的生物地球化学方面
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-10-25 DOI: 10.1134/S0016702923100051
E. V. Evstafeva, E. V. Yaseneva, A. M. Bogdanova, A. S. Makarova, O. A. Zalata, S. L. Tymchenko, O. B. Moskovchuk, A. E. Slusarenko, I. A. Evstafeva, Y. A. Boyarinceva, S. A. Zinchenko

The paper presents evidence that a biogeochemical approach should be applied in analyzing interactions in the system society–nature when the biosphere is affected by anthropogenic impacts, whose key indicator is the health status of the human population. The basic principles and tasks of multilevel medico-ecological monitoring are described, which make it possible to systematically proceed from the qualitative assessment of the state of the human population health and ecological situation to the quantitative assessment of the ecological health risks and regional standards for permissible levels of technogenic factors, with regard to the probable changes in their effects due to the biogeochemical conditions of the environment. The paper provides verification results of the monitoring methods applied at a regional (Republic of Crimea), subregional (in the cities of Sevastopol and Simferopol), and local (individual cohorts of the urban population) levels. Although the official statistics received from various state departments is less informative for the regional research, it nevertheless allowed us to outline (at a reasonable probability level) territories with contrastingly different parameters of environmental health risk. Subregional (within settlements) biomonitoring in Sevastopol and Simferopol has revealed a spatial heterogeneity and loci with higher contents of some heavy metals and other chemical elements in the environment and biosubstrates (soil and plants). Cohort studies of residents of these cities and assessment of 29 chemical elements in the human organism were followed by the examination of the functional state of target systems in humans belonging to risk groups. Results of correlation and regression analysis allowed us to estimate the physiological significance of the elements and the effects of their complex influence at a background exposure.

该论文提供了证据,表明当生物圈受到人为影响时,应采用生物地球化学方法来分析系统-社会-自然的相互作用,其关键指标是人类的健康状况。阐述了多级医学生态监测的基本原则和任务,使其能够系统地从对人口健康和生态状况的定性评估转向对生态健康风险的定量评估,以及技术成因因素允许水平的区域标准,由于环境的生物地球化学条件,其影响可能发生变化。本文提供了在区域(克里米亚共和国)、次区域(塞瓦斯托波尔市和辛菲罗波尔市)和地方(城市人口的个体群体)层面应用的监测方法的验证结果。尽管从各州各部门收到的官方统计数据对区域研究的信息较少,但它使我们能够(在合理的概率水平上)勾勒出环境健康风险参数截然不同的地区。塞瓦斯托波尔和辛菲罗波尔的分区域(定居点内)生物监测显示,环境和生物基质(土壤和植物)中存在空间异质性和一些重金属和其他化学元素含量较高的位点。对这些城市的居民进行的队列研究和对人类生物体中29种化学元素的评估之后,对属于风险群体的人类目标系统的功能状态进行了检查。相关和回归分析的结果使我们能够估计元素的生理意义以及它们在背景暴露下的复杂影响的影响。
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引用次数: 0
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Geochemistry International
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