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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">gesj</journal-id><journal-title-group><journal-title xml:lang="en">GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY</journal-title><trans-title-group xml:lang="ru"><trans-title>GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2071-9388</issn><issn pub-type="epub">2542-1565</issn><publisher><publisher-name>Russian Geographical Society</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.15356/2071-9388_01v09_2016_01</article-id><article-id custom-type="elpub" pub-id-type="custom">gesj-89</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>GEOGRAPHY</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>География</subject></subj-group></article-categories><title-group><article-title>BIOSPHERIC ORGANIZATION AS A “CONTINENTS – OCEANIC BASINS” SYSTEM</article-title><trans-title-group xml:lang="ru"><trans-title></trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="western" xml:lang="en"><surname>Gorshkov</surname><given-names>Sergei P.</given-names></name></name-alternatives><email xlink:type="simple">spgor-smir@yandex.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="western" xml:lang="en"><surname>Mochalova</surname><given-names>Olga I.</given-names></name></name-alternatives><email xlink:type="simple">face@neicon.ru</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff xml:lang="en" id="aff-1"><institution>Dubna University</institution><country>Russian Federation</country></aff><aff xml:lang="en" id="aff-2"><institution>LLC Design Office – Centre for Environmental Initiatives</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2016</year></pub-date><pub-date pub-type="epub"><day>01</day><month>03</month><year>2016</year></pub-date><volume>9</volume><issue>1</issue><fpage>4</fpage><lpage>20</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Gorshkov S.P., Mochalova O.I., 2016</copyright-statement><copyright-year>2016</copyright-year><copyright-holder xml:lang="ru">Gorshkov S.P., Mochalova O.I.</copyright-holder><copyright-holder xml:lang="en">Gorshkov S.P., Mochalova O.I.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://ges.rgo.ru/jour/article/view/89">https://ges.rgo.ru/jour/article/view/89</self-uri><abstract><p>The functional characteristics of the biosphere are reflected in its binominale frame: continents – oceanic basins. The river-basin land, on the one hand, and pericontinental oceanic waters on the other hand, are the main components of the homeostatic mechanism of the biosphere. In the Archean and Early-Middle Proterozoic, seawater biofiltration did not exist. In the Late Proterozoic and part of the Early Paleozoic, biofiltration started to develop and the oceans have become the main heat-engine of the Earth. Today, the maximum concentration of productive phytoplankton and zooplankton – filter bio-systems – is in the pericontinental oceanic zones. This is a response to the maximal flow of nutrients from the land carried mainly with river flow. This is the main signal of a direct link between terrestrial and oceanic ecosystems. The feedback is the atmospheric precipitation induced by heat and moisture flows and carried from the oceans to the land within its primary river-basin part. These links are experiencing anthropogenic destabilization due to some misplaced priorities of sustainable development and its implementation.</p></abstract><kwd-group xml:lang="en"><kwd>biosphere</kwd><kwd>homeostasis</kwd><kwd>biospheric organization</kwd><kwd>frame of the biosphere</kwd><kwd>riverbasin land</kwd><kwd>phytoplankton</kwd><kwd>biofiltration</kwd><kwd>anthropogenic destabilization</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Bazilevich, N.I., Rodin, L.Ye., and Rozova, N.N. (1971) Skolko vesit zhivoye veshchestvo planety? (How Much Does the Living Matter of the Planet Weigh?), Priroda 1, 46–53.</mixed-citation><mixed-citation xml:lang="en">Bazilevich, N.I., Rodin, L.Ye., and Rozova, N.N. (1971) Skolko vesit zhivoye veshchestvo planety? 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