Annals of Geophysics, 55 (3), 2012: NIKITINA Geodiversity, and the geoethical principles for its preservation Nataliya Nikitina LLC Intergeo Managing Company, License Department, Moscow, Russia ANNALS OF GEOPHYSICS, 55, 3, 2012; doi: 10.4401/ag-5492 ABSTRACT The history of the origin and evolution of the term ‘geodiversity’ is described, and its present definitions are given. Several types of values of geodiversity are considered. Moreover, a new type of value is defined: the information value of geodiversity, as developed from the ethical principles of geodiversity preservation. 1. Introduction In the ordinary sense, diversity is the existence of dis- parate, non-recurring, items and a lack of uniformity. Natural diversity is a fundamental feature of Nature. It reflects the set of structural and functional characteris- tics of the natural organization that has been imple- mented during evolution. It currently ensures sustainable development of planetary life, of the biospheres and geospheres, and it supports ecological balance and eco- logical stability, while at the same time allowing the de- velopment of the true potential of Nature. In science, there are several points of view of the concept of ‘natural diversity’: sometimes, it is treated as being synonymous with biological diversity, sometimes as a combination of all species of animals, plants and microorganisms, and of all ecosystems, and their place in ecological processes. Ac- cordingly, there are three levels of biodiversity: – genetic diversity (the amount of genetic information contained in the genes of all species of plants, animals and microorganisms); – species diversity (the number of species); – ecosystem diversity (the number of different habitats, biotic communities, and ecological processes). In biology, diversity is associated with the funda- mental features of life and its organization, while its pro- liferation in geosciences originally had a purely pragmatic aspect of preserving natural values. Geodiversity and the concept of its preservation are new definitions for most people. The concept that the physical features of the Earth (rocks, subsoil, mineral resources) need good manage- ment and preservation is not obvious for the majority, as the structures on the surface of the Earth and within its subsoil look strong, solid and stable. In the past 15 years, the problems of preservation and use of the geological environment has prompted the formation of geodiversity and landscape diversity concepts. 2. Geodiversity and its value In the modern sense, the term ‘geodiversity’ was first used in Tasmania, shortly after the adoption of the Biodi- versity Convention at the International Summit in Rio de Janeiro in 1992. However, before 1992, geoscientists used terms such as the “diversity of the Earth”, and “geomor- phological diversity”. It was a direct consequence of the parallelization with biodiversity and use of terms such as “landscape species” and “landscape community” in biodi- versity theory. Thus, in the early 1990s when biodiversity became an accomplished event, Tasmanian geologists quickly adapted it for the geological equivalent geodiver- sity, to describe the variety within abiotic Nature (Table 1) [Australian Heritage Commission 1996, 1999, 2002]. The basic definitions of geodiversity are given in Table 1. All of these definitions come from a variety of rocks and minerals, landforms, soils, mineral resources and ge- ological processes, or from the inseparable connections between geologic formations, systems and processes, and the people associated with our natural heritage, such as biodiversity and geodiversity, and our cultural land- scapes, and more. Note these defining characteristics of geodiversity. First, it involves both endogenous and exogenous geological processes. Second, the definition implicitly includes past and present geological time and space. However, all of these def- initions have one disadvantage. They do not include the dif- ferent levels of geological systems, and the complex interactions between these geological systems that do not involve the use of different scales, from global (continents and oceans) to elemental (atoms and ions) [Krut’ 1978]. Endogenous and exogenous geological processes have a leading role in the formation, preservation and de- struction of the variety of subsoils, surfaces and land- Article history Received December 1, 2011; accepted February 29, 2012. Subject classification: Geodiversity, Geodiversity value, Ethical principles, Sustainable development, Management of mineral resources. 497 scapes of the Earth, because of their great power and du- ration, which is not comparable with the duration of the existence of the human species. Now the human impacts on the Earth as a geological body are only related to the lithosphere, which they affect in terms of the following basic activities: – geological surveys and exploration (carried out without any material surface integrity); – mining; – construction and maintenance of underground fa- cilities unrelated to mineral production; – formation of lithospheric technical zones under ter- ritories of cities and industrial developments; – dumping of household and industrial wastes, in- cluding radioactive and toxic wastes; – lithospheric (geological) weapons that use cata- strophic geological processes (earthquakes, volcanic erup- tions, large-scale rock falls and landslides) as adverse factors. At the present time, no questions have been raised about the possible limits of this damage, and about the re- sistance of the lithosphere, and the other geological spheres, to this damage. The creative human activities in the sphere of subsoil use are not so great. These are limited to the special pro- tection of geological features of scientific, cultural, aes- thetic, health and recreational values (scientific and training grounds, geological reserves, wildlife and geo- logical sanctuaries, natural monuments, caves and other underground areas). There are six types of values of geodiversity [Sharples 1995, Eberhard 1997, Prosser 2002, Gray 2004], which are: – internal or intrinsic value: the intrinsic value goes back to the ethical approval that some things (in our case geodiversity of Nature) have value simply because they exist, not only because they can be used by people (utili- tarian value); this is the most difficult value to understand and describe, as it involves ethical and philosophical di- mensions of the relationships between society and Nature; – cultural value: as geomythological, archeological and historical value; – aesthetic value: this is the most tangible, real con- cept, as it is based on the visual perception of the physical natural environment, the positive physiological and psy- chological effects of various geological objects on health and human consciousness; – economic value: determined primarily by the need to use subsoil, mineral resources, underground waters, landscapes, and underground cavities in the economic de- velopment of civilization; – functional value: something that provides a substrate for the functioning of the terrestrial biosphere, for the exis- tence of the atmosphere, hydrosphere and lithosphere; – research and educational value: this provides the process of scientific cognition of the world, and is the basis for the monitoring of natural processes, including dangerous geological processes, such as earthquakes, floods and landslides. In addition to these six types of values of geodiversity, there is one more: the information value of abiotic Nature, by analogy with the genetic diversity of species [Nikitina 2011]. Each geological object has its own unique geological information, and the complexity of this information is di- rectly dependent on the hierarchical level of the geological object. At the present stage, only a small part of this infor- mation is available to our surveying and understanding. Every year, tens of thousands of long-term geologi- cal carriers are withdrawn from the geological environ- ment. As a result, the geologically complex hierarchy objects, sophisticated geological systems, and accompany- ing processes are deprived of their future (mineral deposits, NATALIYA NIKITINA 498 Year Author of the definition Definition 2004 Murray Gray The natural range (diversity) of geological (rocks, minerals, fossils), geomorphological (landform, processes) and soil features. It includes their assemblages, relationships, properties, interpretations and systems [Gray 2004]. 2004 David Roche The variety of rocks, minerals, landforms etc., and the processes that have formed these features through geological time. 2002 Collin Prosser The variety of rocks, fossils and minerals and natural processes [Prosser 2002]. 2002 Mick Stanley The link between people, landscape and culture; the variety of geological environments, phenomena and processes that make those landscapes, rocks, minerals, fossils and soils that provide the frame- work for the processes of life on Earth [Stanley 2002]. 1997 Rolan Eberhard The natural range (diversity) of geological (bedrock), geomorphological (landform) and soil features, assemblages, systems and processes. Geodiversity includes evidence for the history of the Earth (evi- dence of past life, ecosystems and environments), and a range of processes (biological, hydrological and atmospheric) that are currently acting on rocks, landforms and soils [Eberhard 1997]. 1995 Chris Sharples The range (or diversity) of geological (bedrock), geomorphological (landform) and soil features, as- semblages, systems and processes [Sharples 1995, Houshold and Sharples 2008]. Table 1. Basic definitions of geodiversity. 499 ore formations). New mechanisms for stabilizing the crustal processes are originated, which lead to the activation of deep faults. This withdrawal of complex hierarchical ob- jects and sophisticated geological systems from the litho- sphere without explaining their relevance to the geological and geophysical evolution of the Earth can be potentially considered as the start of planetary disorganization. 3. Geoethical principles for geodiversity preservation Apart from the introduction of the term geodiversity into the geosciences, the major theoretical achievements of “the geodiversity doctrine” are: 1. The six core principles of sustainable development and use of mineral resources [Gray 2004] are similar to the principles of “deep ecology” that were suggested by Norwegian philosopher Alexander Naess in 1974 [Naess 1984, 1994]: accept that natural change is inevitable, work with the natural functions and processes, manage natural systems within the limits of their capacity, manage natu- ral systems in a spatially integrated manner, use non-re- newable Earth resources wisely and sparingly and at a rate that does not restrict future options. Use renewable re- sources within their regeneration capacity. 2. Classification of value types of geodiversity and cre- ation of the concept of ‘Nature and geological heritage’. 3. Develop a rationale for objective necessity to main- tain geodiversity because of the responsibility of living generations to future generations, and recognize the hard benefit of sustainable development of natural resources to mankind and to the natural world. 4. Action-oriented recommendations for geodiversity conservation and practical realization [Limestone Land- scapes 2010, Zwolinski 2010]. In general, the geodiversity doctrine is a significant achievement in geosciences. However, due to the insuffi- cient development of the ethical foundations of this doc- trine, we can see contradictions between its basic elements. For example, the recognition of the internal (intrin- sic) value of abiotic Nature essentially means that people do not have the right to reduce the geodiversity; in other words, people do not have the right to exploit objects that are abiotic in nature, or to interfer in the organiza- tion processes that occur in abiotic Nature. In this case, any proposed options for preservation of geodiversity will constantly lose competition to the mining industry, because revenues from this sector are obvious and tan- gible. The proposed principles for the preservation of ge- odiversity do not contain any indications of the boundaries of the right to exist. What geological fea- tures, objects, systems, processes and phenomena “have value simply because they exist”? How does this relate to the objective necessity for human use of mineral re- sources for the maintenance of the existing human civi- lization? Should we stop the spread of geological processes that are dangerous for us? In developing the ethical principles of geodiversity preservation, I have tried to rely not on an abstraction of the universal validity of moral norms, but on their poten- tial realizability. 1. Being a part of Nature, people should not re-orga- nize geological systems, particularly on a global and re- gional scale. It is permissible to interfere with natural geologic processes on a local level in cases where they are a threat to human life. 2. People have no right to reduce geodiversity, except to meet basic needs. 3. Recognition of the need to establish effective lim- its of consumption and use of mineral resources, as com- ponents of the geological environment, on the basis of stabilization of the world population; to substitute the lin- ear degradation of mineral resources using renewable re- sources and the recycling of mining wastes. 4. Opposition to an unregulated market economy, es- pecially if it is a mineral-resources-based economy. 5. The use of mineral resources, and of objects and components of the geological environment should be based on the recognition of the objective laws of develop- ment and interactions between the geospheres and society, on the modern scientific and technological achievements, on the combination of possibilities of geospheres, and on the economic interests of society, providing real guarantees for the rights of citizens to benefit from the use of the sub- soil (scientific principle). 6. Policies, strategies and tactics of geological her- itage preservation should be formed as a complex inter- active system of institutions and individuals: governments, public and social organizations, on the global, national and regional levels; geoscientists, geoexperts, and ‘geological heritage consumers’ (visitors to geoparks and geological museums, tourists). 7. In the ‘man-and-abiotic-nature’ system, the whole takes precedence over the singular, such that if the use of a geological object does not to lead to a decrease in the geodiversity of higher geosystems, then that object can be used). Our proposed variant of ethical principles for geodi- versity preservation is not the only feasible theory. We hope that our colleagues and/or ‘opponents’, especially for the ethics, will offer other projects, following the logic of which we will have an opportunity to improve the ge- odiversity concept. 4. Conclusions Thus, in contrast to the concept of biodiversity, the term geodiversity, its value, and the need for its conserva- tion, has not yet entered the broad academic community. GEODIVERSITY, AND THE GEOETHICAL PRINCIPLES FOR ITS PRESERVATION However, it is clear that in addition to biodiversity con- servation, geodiversity (and in the future, the variety of animate and inanimate Nature) should also be a priority in any human activity on Earth. It is characteristic of the ge- ological diversity, and ethical guidelines for its conserva- tion should serve as a basis for policy, as we aspire to manage our mineral resources to ensure sustainable eco- nomic development. Undoubtedly, in the third millennium, we have to search for new geoethical ideals in our subsoil use. References Australian Heritage Commission (1996). Australian Nat- ural Heritage Charter, 1st ed., Canberra, Australian Heritage Commission. Australian Heritage Commission (1999). Natural Heritage Places Handbook, Canberra, Australian Heritage Com- mission. Australian Heritage Commission (2002). Australian Nat- ural Heritage Charter, 2nd ed., Canberra, Australian Heritage Commission. Eberhard, R., ed. (1997). Pattern and Process: Towards a Re- gional Approach to National Estate Assessment of Ge- odiversity, Canberra, Australian Heritage Commission. Gray, J.M. (2004). Geodiversity. Valuing and Conserving Abiotic Nature, Chichester, John Wiley & Sons Ltd. Houshold, I., and C. Sharples (2008). Geodiversity in the wilderness: a brief history of geoconservation in Tas- mania, Geol. Soc. London, Spec. Publ., 300, 257-272. Krut’, I. (1978). Introduction to the uniform theory of the Earth, Levels of Geosystems Organization, Nauka, Moscow (in Russian). Limestone Landscapes (2010). Geodiversity action plan 2010-2015, Geology and landscape England programme: http://www.limestonelandscapes.info/Pages/publica tions.aspx Naess, A. (1984). A defense of the deep ecology move- ment, Environ. Ethics, 6, 265-270. Naess, A. (1994). The deep ecological movement: some philosophical aspects, In: Environmental Ethics, edited by L.P. Pojman, Boston-London, Jones and Bartlett Publisher, 411-421. Prosser, C. (2002). Term of endearment, Earth Herit., 17, 12-13. Nikitina, N. (2011). Ethical principles and the valuable ap- proach for preservation of geodiversity, VIII Forum Italiano di Scienze della Terra, Torino, September 19- 23, 2011, Abstract V. 274. Sharples, C. (1995). Geoconservation in forest manage- ment: principles and procedures, Tasforest, 7, 37-50. Stanley, M. (2002). Geodiversity – linking people, landscape and their culture. Abstract for Natural and Cultural Landscape Conference, Dublin, Royal Irish Academy, 14. Zwolonski, Z. (2010). The routine of landform geodiver- sity map design for the Polish Carpathian Mts, Land- form Analysis, 11, 77-85. Corresponding author: Nataliya Nikitina, LLC Intergeo Managing Company, Moscow, Russia; e-mail: nikitinank@mmcintergeo.ru. © 2012 by the Istituto Nazionale di Geofisica e Vulcanologia. All rights reserved. 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