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Journal articles on the topic 'Anthropogeny'

Author: Grafiati

Published: 4 June 2021

Last updated: 18 February 2022

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1

정해갑. "One Genus (γενος) -One Form (εἰδος) Hypothesis in Hellenistic Anthropogeny: Gender Discrimination as Quantitative Difference." Journal of Classic and English Renaissance Literature 22, no. 1 (June 2013): 47–63. http://dx.doi.org/10.17259/jcerl.2013.22.1.47.

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Freter, Björn. "Democritus on Being and Ought: Some Remarks on the Existential Side of Early Greek Atomism." Akropolis: Journal of Hellenic Studies 2 (December 31, 2018): 67–84. http://dx.doi.org/10.35296/jhs.v2i0.23.

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According to Democritus' anthropogeny is a microcosmic consequence within the process of cosmogony. However, the case of man is a peculiarity: man, this atom complex, is well aware of himself, yet is not aware of what he must do. Man does not naturally do that which promotes the harmonious ordering of his atoms. We must create a second nature. Now it becomes possible for us to be as we must be according to our first nature. Democritus is the is first thinker who explains to us what our nature is and who, from our being, derives an ought: he who wishes to do the right thing for both himself and others finds himself subject to the ought requirement to do that which brings the most calm to the atoms. This is a direct connection between being and ought, an extravagant mechanical existentialism.

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Vacín, Luděek. "Cosmogony, Theogony and Anthropogeny in Sumerian Texts. By Jan J. W. Lisman. Alter Orient und Altes Testament 409. Münster: Ugarit-Verlag, 2013. Pp. xii + 422. €82.00 (cloth)." Journal of Near Eastern Studies 75, no. 2 (October 2016): 397–401. http://dx.doi.org/10.1086/687542.

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Ломиашвили, Лариса, Larisa Lomiashvili, В. Сидельников, V. Sedelnikov, А. Постолаки, and A. Postolaki. "FROM UNITY TO THE VARIETY OF FORMS IN NATURE." Actual problems in dentistry 11, no. 3 (June 25, 2015): 4–13. http://dx.doi.org/10.18481/2077-7566-2015-11-3-4-4-13.

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<p>The questions of unity and variety of forms in nature are discussed In the presentpaper. Refers to the process of shaping the teeth, structural and functional unit of the tooth is determined: canine module – odontomer. The common structure of the tooth, hand and foot is demonstrated, moreover the morphological similarity is manifested at the stage of human embryo – histogenesis. Thus, at the stage of bookmarks, formation, growth and development of certain organs of a human embryo (hands, feet and teeth) one can see some similarity of their structure, the internal order of the morphological units (fingers, enameldentinal rollers), which describes the universal law of creation – "the golden proportion" . Dentists have to know the anatomy of the organs and tissues of the oral cavity very well when restoring the teeth. Also dentists should study their phylogeny, anthropogeny,ontogeny in order to reconstruct the missing tissue in their original form, in harmony. The stages of dental restorations made of composite materials based on modular technology are shown.</p><p>We have proposed a matrix model for shaping the crown of a tooth. At the base of a tooth crown several modules – odontometrs are laid, which are directed to the fissure of the first order. A doctor deliberately puts missing edges, filling empty spaces with composite material, thus performing a specific algorithm of a tooth construction. While restoration the missing tissue you operate with the canine tooth module and composite material and fill a tooth crown.</p><p>Thus, we consider a canine tooth as the initial unit, fractal part of ontogenesis of dento-facial system of a person in accordance with the set laws which are typical for the modular (fractal) structural organization.</p>

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Bugmann, Harald. "Anthropogene Klimaveränderung, Sukzessionsprozesse und forstwirtschaftliche Optionen | Anthropogenic Climate Change, Successional Processes and Forest Management Options." Schweizerische Zeitschrift fur Forstwesen 150, no. 8 (August 1, 1999): 275–87. http://dx.doi.org/10.3188/szf.1999.0275.

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Anthropogenic changes of the climate have the potential to significantly affect forests in the coming century. In this paper, methods for assessing the impacts of such changes are reviewed, and mathematical models are used to evaluate possible changes of the tree species composition and biomass storage of Swiss forests. The simulation results are discussed from an ecological as well as from a forestry perspective.

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Nesterchuk, I. "Physico-geographic distribution of Right Bank Polissya: prospects for development of specialties of tourism." Physical Geography and Geomorphology 89, no. 1 (2018): 41–48. http://dx.doi.org/10.17721/phgg.2018.1.06.

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The territory of the study of the Right Bank Polissya in this article is extremely vivid and dotted, it is possible to outline the following main tasks: the territorial physical and geographical differentiation of the region in the context of the methodology of studying the food traditions of the Polischuk; assessment of the territory for the prospects of practical management of gastronomic tourism within the united territorial communities. In general, the Polesie region is not a zonal phenomenon, and its origin is connected with paleogeographic conditions of anthropogeny, therefore it is the physical and geographical edge of the zone of mixed forests of the East European country. The involvement of geographic science in the study of the history of food prints of the Polyschuk in the original landscapes of residence deserves detailed study. The nutrition of the Polischuk apparently bears the landscape-specific consumption of food in certain areas. Organically healthy food demonstrates the geological past and predicts a nutrition system at the present stage without paying attention to the pace of the urban food culture. Under certain circumstances and with the complication of natural conditions, the gastronomy of the Polischuk differed by simple gastronomic markers, but not coarse and not perfect processes for the preparation of autochthonous dishes. The consideration of the physical and geographical preconditions for the formation of gastronomic tourism resources in the region contributed to the popularization of the gastronomic industry in a certain retrospective period. In Ukraine, tourism was underdeveloped, until 1914, when tourism activities were carried out by the Russian Society of Tourists and the Polish Local History Society. The study of physical and geographical regionalization of the region at an angle of gastronomic tourism is almost unknown. At the time there is a rather interesting scientific issue for the territory of the Right-bank Polissya in the reflections of the feeding of the Polischuk. But a significant financial leverage for the development of the united territorial communities is to have gastronomic tours within the boundaries of their original habitats and the transfer of gastronomic practices to a wide tourist community

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7

Klimenko, M. O., I. I. Zaleskyi, and O. O. Biedunkova. "Environmental evaluation of geochemical changes in bottom sediments of Ustia headwater." Ecology and Noospherology 27, no. 3-4 (October 22, 2016): 97–109. http://dx.doi.org/10.15421/031618.

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Any changes to anthropogenic impact within the watersheds involving the transformation of ecosystem relationships cause irreversible changes in the structure and composition of sediments. The objective of the research was to analytically compare the results of the study on heavy metals in Ustia River sediments with the use of various methods for determining environmental geochemical changes in headwaters due to human transformation of the basin between 1994 and 2015. Ustia River experienced the highest anthropogenic impact during 1968–1994. Starting from 1968 and up to the present time the wastewater volume disposed to the river is more than 25 m3 per day. Despite the downturn in the national economy since the mid 90-ies of the 20th century, the negative impact on the environment of surface water area does not stop. The environmental evaluation of the bottom sediments of Ustia River was held basing on the results of spectral analysis of air-dried samples of silt fraction from the selected samples. The researcher analysed the content of heavy metals which emission takes place within the river basin as a result of runoff generated by chemical and woodworking industries, transport, wastewater and agricultural use of the territory, particularly Pb, Mn, Co, Cu, Zn and Cd. For the first time, researchers have figured out that for the past twenty years there has been no improvement in the overall ecological state of the Ustia River bottom sediments. The human impacts on the hydro-ecosystem, assessed according to the content of heavy metals, have moderated only in the river section near the headstream. The author views this fact as a consequence of reduced chemicals’ usage (i.e. fertilizers, pesticides, compost, sewage and animal waste) on the cultivated land in this part of the basin. The remaining sections of riverbed have experienced deterioration of the bottom sediments; it is particularly notable with regard to the content of such elements as Mn, Cu, Zn and Pb within the urban areas. The increase of the concentrations of metals in the sediments near Basiv Kut Dam Lake in 2015, compared with the relevant data for 1994, can serve as the evidence that the negative impact on hydro-ecosystem has intensified. In both observation periods the bottom sediments of the upper part of the river has demonstrated extremely high content of Mn. Hence, in 1994 it markedly declined in the central section of the stream, and in 2015 it appeared in significant concentrations in the sediments along the channel. It is obvious that in this case there are geochemical features of the basin; however the situation in 2015 indicates a change in the state of bottom sediments with regard to the content of Mn under the influence of anthropogenic factors. The analysis of the geochemical changes in bottom sediments of Ustia headwater from 1994 until 2015 show that the concentrations of such elements as Cu, Zn, Pb, Co and Cd in the bottom sediments according to 2015 data turned out to be higher compared to 1994, excluding the upper part of the river. Nevertheless the geochemical anomalies of Mn contents noticed along the channel are also the case in this situation. The level of anthropogenic impact, measured in terms of total pollution index for the concentration of heavy metals in bottom sediments in both observation periods appeared to be «weak» or «slightly increased» if there were toxic elements. Hence, if in 1994 there was a high risk of pollution of bottom sediments with such elements as zinc, lead and copper both in case of the relative background values and hygiene criteria (maximum allowable concentrations in soil), in 2015 cobalt also appeared among such elements. The level of contamination of sediments according to international contamination classes mainly shows «significant» and «increased» impact on different parts of the river for the Mn content (5–6 grades) in both observation periods; the Cu and Zn content vary from «low» to «moderate» in 1994 (1–3 grades) and from «low» to «substantial» in 2015 (2–4 grades); the Pb content is «poor» (grade 1) in 1994 and «moderate» in 2015; Co and Cd content describes human impact on hydro-ecosystem as «weak» in both periods (0–1 grades). The assessment methods used by the researcher allowed tracking various aspects of heavy metal pollution in the bottom sediments. Furthermore, they help discovering that nowadays the sediments of Ustia River play the role of anthropogeny outcome battery against the geochemical anomalies of individual elements.

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Schroeder, Richard, Anneka Mordhorst, Heiner Fleige, Rainer Horn, and Bernd Burbaum. "Moorböden als Natur- und Kulturgeschichte in Schleswig-Holstein – Verfahren zur qualitativen Bewertung von Archivböden." Die Bodenkultur: Journal of Land Management, Food and Environment 71, no. 3 (September 1, 2020): 121–35. http://dx.doi.org/10.2478/boku-2020-0011.

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Zusammenfassung Die vielseitigen Funktionen von Moorlandschaften sind in kulturhistorischer und klimatischer Hinsicht von immer größer werdendem Interesse. Da Moore über lange Zeiträume anthropogene Zeugnisse konservieren und als Kohlenstoffsenke gelten, gilt es einen umfangreichen Schutz dieser Ökosysteme zu etablieren, um diese Funktionen aufrechtzuerhalten. In dieser Untersuchung wurden Informationen von über 140 Moorstandorten aus Schleswig-Holstein zusammengetragen und ausgewertet, anhand einer einheitlichen Bewertungsmatrix evaluiert und nach Güteklassen (A–D) kategorisiert. Als Grundlage der Güteklassen wurden Bewertungskriterien gewählt, welche durch ein Punktesystem (1–5) definiert sind. Die Bewertungskriterien gliedern sich in drei Hauptkategorien: „kulturelle Bedeutung“, „ökologische Bedeutung“ und „bodenkundliche/geologische Bedeutung“. Die Auswertung ergab, dass 15 % der ausgewerteten Moorstandorte als „konkrete Archivböden“ angesprochen werden können. Diese erfüllen ökologische Anforderungen in einem hohen Maße und erreichen somit eine Punktzahl von > 4, weshalb sie in die höchste Güteklasse „A“ fallen. Aufgrund unzureichender Dokumentation oder sichtbaren anthropogenen Einflüssen werden 46 % der Archivböden der Güteklasse „B“ zugeordnet und gelten als „potenzielle Archivböden“. Der Güteklasse „C“ werden 23 % der Moore zugeordnet und gelten ebenfalls als „potenzielle Archivböden“ und befinden sich in einem stark anthropogen geprägten Zustand, welcher kosten- und zeitintensive Renaturierungsmaßnahmen zur Folge hätte. In die niedrigste Güteklasse „D“ fallen 16 % der bewerteten Moore. Diese unterliegen einer irreversiblen Degradation und sind nicht mehr / kaum als Archivböden anzusprechen. Mit der ausgearbeiteten Bewertungsmatrix wird letztendlich eine flächendeckende Evaluierung und Kategorisierung der Moorstandorte in Schleswig-Holstein angestrebt, um den Erhalt dieser Ökosysteme langfristig sichern zu können.

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Harlfinger, Otmar, Wolfgang Kobinger, Gerald Fischer, and Harald Pilger. "Industrial Snowfalls - An Anthropogenic Phenomenon in Central Europe." Meteorologische Zeitschrift 9, no. 4 (September 20, 2000): 231–36. http://dx.doi.org/10.1127/metz/9/2000/231.

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del Carpio Penagos, Carlos Uriel. "Soconusco, Chiapas. Transformaciones ambientales de origen antrópico." DECUMANUS 2, no. 2 (2017): 7–26. http://dx.doi.org/10.20983/decumanus.2017.1.1.

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11

Steil, Peter, and Bernhard Luksch. "Messung anthropogener und biogener Kohlenwasserstoffe." Meteorologische Zeitschrift 7, no. 1 (February 18, 1998): 19–23. http://dx.doi.org/10.1127/metz/7/1998/19.

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12

Fellner, Johann, and Helmut Rechberger. "Anthropogene Ressourcen." Österreichische Wasser- und Abfallwirtschaft 67, no. 1-2 (January 22, 2015): 19–20. http://dx.doi.org/10.1007/s00506-015-0209-z.

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13

Novak, David, and Christian Synwoldt. "Causes and consequential costs of anthropogenic climate change." Archives of Business Research 8, no. 7 (August 4, 2020): 171–81. http://dx.doi.org/10.14738/abr.87.8588.

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On the one hand, this paper examines the costs directly caused by climate change, also com- paring the possible costs for preventing damage; on the other hand, it compares the effects of the radiation propulsion caused by anthropogenic greenhouse gas emissions on anthropogen- ic heat generation through the use of all types of fuels. In addition to the global warming ef- fect caused by anthropogenic heat radiation, there are also local heat islands that are affect- ed by a much greater rise in temperature. Purpose: A cost comparison of the damage caused by climate change and a quantitative com- parison of the direct heat development through the use of fuels with the radiative forcing through anthropogenic greenhouse gas emissions.Design / methodology / approach: In both cases, the research method is based on the analysis of public databases such as the International Energy Agency (IAE), as well as published lit- erature on global energy supply and the Federal Statistical Office. Results: The expected consequential damage caused by climate change will probably present most states with insoluble financial burdens. The radiation propulsion from anthropogenic greenhouse gas emissions makes an 80 times greater contribution to global warming than the anthropogenic heat generation from all types of fuels. Research / practical implications: Future research should show the consequences for the economy and the acquisition of money on the one hand and on the other hand include the ef- fects of global warming and the heat islands, both of which lead to a loss of habitat. Originality / Value: This paper has both the expected follow-up costs in view as well as the causes and effects of anthropogenic greenhouse gas emissions.

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Golwer, Arthur. "Long-term Effects of localised Accumulation of Anthropogenic Materials on the Groundwater." Zeitschrift der Deutschen Geologischen Gesellschaft 146, no. 1 (January 1, 1995): 191–200. http://dx.doi.org/10.1127/zdgg/146/1995/191.

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Kvesitadze, G. "DEGRADATION OF ANTHROPOGENIC CONTAMINANTS BY HIGHER PLANTS." Biotechnologia Acta 6, no. 4 (2013): 132–43. http://dx.doi.org/10.15407/biotech6.04.132.

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Wirth, Volkmar. "Trendwende bei der Ausbreitung der anthropogen geförderten Flechte Lecanora conizaeoides?" Phytocoenologia 23, no. 1-4 (December 15, 1993): 625–36. http://dx.doi.org/10.1127/phyto/23/1993/625.

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Richter, Thomas. "Anthropogene Krankheitsursachen minimieren." veterinär spiegel 20, no. 03 (September 2010): 127–32. http://dx.doi.org/10.1055/s-0030-1250154.

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Wurl, Jobst, Christian Sommer-Von Jarmersted, and Asaf Pekdeger. "Geogenic and anthropogenic impacts on the groundwater resources in southwest of Berlin." Zeitschrift der Deutschen Geologischen Gesellschaft 146, no. 1 (January 1, 1995): 243–49. http://dx.doi.org/10.1127/zdgg/146/1995/243.

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Peng, Tsung-Hung. "Anthropogenic CO₂ in the ocean." Scientia Marina 69, S1 (June 30, 2005): 85–96. http://dx.doi.org/10.3989/scimar.2005.69s185.

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Dölling, Manfred. "Geological Mapping as a Tool for Determination Anthropogenic Intervention." Zeitschrift der Deutschen Geologischen Gesellschaft 145, no. 1 (January 1, 1994): 116–22. http://dx.doi.org/10.1127/zdgg/145/1994/116.

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S.B., Abbasov, Baxtiyorova D., and Eshquvvatov B.B. "Ecological Status Of Anthropogenic Landscapes Of Samarkand Oash." American Journal of Applied Sciences 02, no. 09 (September 30, 2020): 175–79. http://dx.doi.org/10.37547/tajas/volume02issue09-27.

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Vácha, R., J. Němeček, and E. Podlešáková. "Geochemical and anthropogenic soil loads by potentially risky elements." Plant, Soil and Environment 48, No. 10 (December 22, 2011): 441–47. http://dx.doi.org/10.17221/4393-pse.

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The differentiation between anthropogenic and geogenic loads of the soils by potentially risky elements was observed. The collection of soil horizon samples from 21 localities with different anthropogenic loads (imission fall-outs, floods, historical mining) and geogenic loads (lithogenic, chalcogenic) was composed. The soil characteristics (pH, C<sub>ox</sub>), total content of 13 potentially risky elements, content of potentially risky elements in the extract of 2M HNO<sub>3</sub>, 1M NH<sub>4</sub>NO<sub>3</sub> (mobile forms) and 0.025M EDTA (potentially mobilizable forms) were detected. The solubility as the ratio of total content and the content of risky elements in the other extracts was calculated. The differences between the solubility for each risky element and for each type of the load were determined. It was concluded that the highest solubility was determined in the fluvisols contaminated by the floods and in the soils contaminated by imission fall-outs. Significantly lower solubility of potentially risky elements was determined in the soils with geogenic loads. The efficiency of the used extracts for the differentiation of the soil load was assessed (2M HNO<sub>3</sub>, 0.025M EDTA). The types of geogenic loads were characterised in the extent of used soil collection. Geochemically anomalous parent materials and soil types developed on these parent materials were described.

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Pérez, Fiz F., Javier Arístegui, Marcos Vázquez-Rodríguez, and Aida F. Ríos. "Anthropogenic CO₂ in the Azores region." Scientia Marina 74, S1 (November 15, 2010): 11–19. http://dx.doi.org/10.3989/scimar.2010.74s1011.

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Dickhof, Alfred. "Bodenbildung in anthropogen veränderten Substraten – Beobachtungen aus der großmaßstäbigen Waldbodenkartierung im Rheinland." Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften 73 (February 17, 2011): 19–30. http://dx.doi.org/10.1127/sdgg/73/2011/19.

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Ronda, M. "Anthropogenic Poetics." Minnesota review 2014, no. 83 (January 1, 2014): 102–11. http://dx.doi.org/10.1215/00265667-2782291.

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Simpkins, Graham. "Anthropogenic signals." Nature Climate Change 6, no. 11 (October 26, 2016): 982. http://dx.doi.org/10.1038/nclimate3152.

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Stahle, David W. "Anthropogenic megadrought." Science 368, no. 6488 (April 16, 2020): 238–39. http://dx.doi.org/10.1126/science.abb6902.

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Benner, Shawn. "Anthropogenic arsenic." Nature Geoscience 3, no. 1 (January 2010): 5–6. http://dx.doi.org/10.1038/ngeo726.

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Powers, Michael, Michael James Ellett Monson, Frederic S. Zimmerman, Sharon Einav, and David J. Dries. "Anthropogenic Disasters." Critical Care Clinics 35, no. 4 (October 2019): 647–58. http://dx.doi.org/10.1016/j.ccc.2019.06.002.

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McConkey, Kim. "Anthropogenic Disturbances." Resonance 25, no. 5 (May 2020): 677–89. http://dx.doi.org/10.1007/s12045-020-0983-1.

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Wagner, H. M. "Anthropogenes Ozon." Umweltwissenschaften und Schadstoff-Forschung 2, no. 4 (November 1990): 215–19. http://dx.doi.org/10.1007/bf03039399.

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Westphal, Uli. "Elephas anthropogenus." Zoologischer Anzeiger - A Journal of Comparative Zoology 256 (May 2015): 36–41. http://dx.doi.org/10.1016/j.jcz.2015.05.001.

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Maisuradze, G. M. "Anthropogene of the anticaucasus." Palaeogeography, Palaeoclimatology, Palaeoecology 72 (January 1989): 53–62. http://dx.doi.org/10.1016/0031-0182(89)90131-4.

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Klaschka, Ursula. "Verständigungsprobleme durch anthropogene Einträge?" Environmental Sciences Europe 21, no. 4 (July 7, 2009): 324–38. http://dx.doi.org/10.1007/s12302-009-0073-1.

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Egger, Garry, David Colquhoun, and John Dixon. "“Anthropogens” in Lifestyle Medicine." American Journal of Lifestyle Medicine 9, no. 3 (December 5, 2013): 232–40. http://dx.doi.org/10.1177/1559827613512596.

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Graßl, H. "Anthropogene Beeinflussung des Klimas." Physik Journal 45, no. 7 (July 1989): 199–206. http://dx.doi.org/10.1002/phbl.19890450704.

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Mohammad Reza, Khaleghi. "The influence of deforestation and anthropogenic activities on runoff generation." Journal of Forest Science 63, No. 6 (June 27, 2017): 245–53. http://dx.doi.org/10.17221/130/2016-jfs.

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In recent decades, due to rapid human population increases and in its results, destructive effects of anthropogenic activities on natural resources have become a great challenge. Land use and vegetation are important factors in soil erosion and runoff generation. This study was performed to assess the effects of different amounts of forest cover on the control of runoff and soil loss in the Talar basin, which is located in Mazandaran province, using a runoffrainfall model, geographical information system (GIS) and remote sensing (RS) to determine the hydrologic effects of deforestation on the Talar watershed (north of Iran). A runoff-rainfall model has been presented using GIS (HECGeoHMS) and hydrologic model (HEC-HMS). Land use changes (deforestation) and anthropogenic activities (roads and impervious surfaces development) were evaluated using RS techniques and satellite images. We used the Soil Conservation Service and Curve Number methods for hydrograph simulation and runoff estimation, respectively. First, a model was performed and optimized. Afterward, the optimized model was evaluated by other six events of floods (model validation). According to the obtained results, the runoff generation potential has been increased in the Talar watershed due to deforestation during the last forty years. Land use changes cause an increase in runoff volume and flood peak discharge.

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Remeš, J., and R. Šíša. "Biological activity of anthropogenic soils after spoil-bank forest reclamation." Journal of Forest Science 53, No. 7 (January 7, 2008): 299–307. http://dx.doi.org/10.17221/2075-jfs.

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The paper presents the results of relatively long-term research focused on spoil bank revitalization pro-cesses in the North Bohemian Brown Coal Basin after the first three years of observations. The biological activity of soil (namely catalase and phosphatase activity), indicators of basal and potential soil respiration, ammonification and growth, development and nutrition status of forest plantations were selected as indicators of this revitalization process. These parameters were determined in five localities of different age of reclamation where different technological approaches and tree species compositions were used. The results confirm the distinct time dependence of revitalization processes. From the aspect of biological activity older reclamations are close to natural forest soil. The enrichment of top soil layer with organic matter before the plantation (by ploughing in cellulose fibres and peat addition) increased some parameters of soil biological activity. The positive amelioration effect of black alder (<i>Alnus glutinosa</i>) was also confirmed.

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Leal-Noriega, Mario Helberto, and Carlos Alberto Vargas-Jiménez. "Sismicidad antropogénica en los alrededores de algunas represas en Colombia." Boletín de Geología 42, no. 3 (September 30, 2020): 123–39. http://dx.doi.org/10.18273/revbol.v42n3-2020005.

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Esta investigación analiza si la sismicidad registrada en los alrededores de cinco embalses en Colombia, está relacionada con la sobrecarga y descarga ejercida por sus ciclos de llenado y vaciado, respectivamente. Las represas seleccionadas cuentan con diferentes rangos de volumen de almacenamiento de agua, por ser uno de los parámetros que más suelen influir en la sismicidad detonada por embalses. El período de estudio se delimitó entre los años 2000 y 2017, empleando como información de referencia los siguientes insumos: eventos sísmicos registrados por la Red Sismológica Nacional de Colombia, reportes diarios sobre el volumen de almacenamiento de los embalses, así como información geológico-estructural de las áreas de estudio a nivel regional generada por el Servicio Geológico Colombiano. Los análisis realizados para los embalses de Betania, Calima, Urrá y Salvajina, no permiten establecer de forma contundente una relación directa entre los sismos registrados y los cambios de volumen de estos embalses; sin embargo, los resultados obtenidos para la represa de Topocoro estiman posible que la construcción de esta estructura pueda estar incidiendo en la ocurrencia de una mayor cantidad de eventos sísmicos en sus alrededores.

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Nardin, Dmitry Sergeevich. "Sustainable Development Management of Natural-anthropogenic Complexes of Rural Territories." Journal of Advanced Research in Dynamical and Control Systems 12, SP3 (February 28, 2020): 1447–52. http://dx.doi.org/10.5373/jardcs/v12sp3/20201397.

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Franzini, Marco. "Stones in monuments: natural and anthropogenic deterioration of marble artifacts." European Journal of Mineralogy 7, no. 4 (August 1, 1995): 735–44. http://dx.doi.org/10.1127/ejm/7/4/0735.

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Nitzsche, Niels, Wolfgang Siebel, and Ingrid Stober. "Geologische, hydrogeologische und anthropogene Einflüsse auf die Wasserchemie der Möhlin, Schwarzwald – eine Momentaufnahme." Grundwasser 26, no. 2 (February 22, 2021): 175–89. http://dx.doi.org/10.1007/s00767-021-00480-4.

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ZusammenfassungDiese Arbeit untersucht die geologischen, hydrogeologischen und anthropogenen Einflüsse auf die chemische Zusammensetzung eines Flusses, am Beispiel der Möhlin. Wasserproben wurden an verschiedenen Flussabschnitten genommen und mittels Alkalinitätstest und Ionenchromatographie auf die Ionen Ca2+, Mg2+, Na+, K+, HCO3−, CO32−, SO42−, Cl−, F− und NO3− untersucht. Daneben wurden Leitfähigkeit, Temperatur, Abfluss und pH-Wert gemessen und die δD- und δ18O‑Isotopenzusammensetzung durch Cavity-Ring-Down-Spektroskopie ermittelt. Die Untersuchung zeigt, dass es sich bei der Möhlin im Oberlauf um einen silikatisch geprägten Fluss handelt, während sie sich im Unterlauf an der Grenze von silikatisch bis karbonatisch bewegt. Die Geologie hat den stärksten Einfluss auf die Wasserchemie der Möhlin, wobei große Anteile am geologischen Fingerabdruck durch ihre Zuflüsse geprägt werden. Weitere Einflussfaktoren sind anthropogene Einleitungen, wasserbauliche Maßnahmen sowie der ehemalige Bergbau im Elsass und Schwarzwald. Insgesamt weist das Wasser der Möhlin in Bezug auf die untersuchten Parameter eine gute Wasserqualität auf.

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Ellis, Erle C. "The Anthropogenic Biosphere." Bulletin of the Ecological Society of America 96, no. 3 (July 2015): 494–95. http://dx.doi.org/10.1890/0012-9623-96.3.494.

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Livingston, Hugh D., and Pavel P. Povinec. "Anthropogenic marine radioactivity." Ocean & Coastal Management 43, no. 8-9 (January 2000): 689–712. http://dx.doi.org/10.1016/s0964-5691(00)00054-5.

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Raupach, M. R., C. Le Quéré, G. P. Peters, and J. G. Canadell. "Anthropogenic CO2 emissions." Nature Climate Change 3, no. 7 (June 25, 2013): 603–4. http://dx.doi.org/10.1038/nclimate1910.

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Gombosi, T. I., D. N. Baker, A. Balogh, P. J. Erickson, J. D. Huba, and L. J. Lanzerotti. "Anthropogenic Space Weather." Space Science Reviews 212, no. 3-4 (April 13, 2017): 985–1039. http://dx.doi.org/10.1007/s11214-017-0357-5.

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Vignieri, Sacha. "An anthropogenic cacophony." Science 371, no. 6529 (February 4, 2021): 580.10–582. http://dx.doi.org/10.1126/science.371.6529.580-j.

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Cevrim, Mustafa, Harald Heinz, Lutz Müller, and Harro Stolpe. "Evaluation of Geogenic and Anthropogenic Influences on Groundwater Chemistry during Landfill Site Investigations." Zeitschrift der Deutschen Geologischen Gesellschaft 141, no. 2 (December 1, 1990): 408–14. http://dx.doi.org/10.1127/zdgg/141/1990/408.

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Meiwirth, Kirsten, Lüder Kruse, Susanne Wachtendorf, Melanie Wienberg, Matthias Zabel, and Horst D. Schulz. "Enrichment of heavy metals in Baltic Sea sediments (Kiel Bight) - Early diagenesis and anthropogenic influence." Zeitschrift der Deutschen Geologischen Gesellschaft 147, no. 1 (May 29, 1996): 137–44. http://dx.doi.org/10.1127/zdgg/147/1996/137.

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Schönwiese, Christian-D. Walter, and Sven Brinckmann. "Statistical assessments of anthropogenic and natural global climate forcing. An update." Meteorologische Zeitschrift 19, no. 1 (February 1, 2010): 3–10. http://dx.doi.org/10.1127/0941-2948/2010/0421.

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