Schneider, Jürgen F.

[["dc.bibliographiccitation.firstpage","45"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Marine Ecology"],["dc.bibliographiccitation.lastpage","63"],["dc.bibliographiccitation.volume","4"],["dc.contributor.author","Schneider, Jürgen"],["dc.contributor.author","Torunski, Horst"],["dc.date.accessioned","2019-07-19T09:24:39Z"],["dc.date.available","2019-07-19T09:24:39Z"],["dc.date.issued","1983"],["dc.description.abstract","Biokarst-forms on limestone coasts are developed and arranged according to the bionomic zonation. The development of biokarst is the result of bioerosion, a synergistic effect of biological corrosion by endoliths and biological abrasion by grazers. The cumulative effect of biogenic carbonate destruction leads to coastal destruction with a resulting highly profiled morphology on the limestone surfaces along the coastal profile. Under the influence of environmental factors a zonation of organisms develops which brings in turn a zonation of erosion rates (0.1-1.1 mm a-1) resulting in biokarst-forms such as rock holes, rock pools and notches. Products of bioerosion on limestone coasts are dissolved carbonate (by biological corrosion, 10–30% of the decomposed limestone) and particulate carbonate (by biological abrasion, 70–90% of the decomposed limestone) both of which contribute directly or indirectly to nearshore sedimentation. Size and shape of the bioerosional grains are determined by the boring pattern of the endoliths. The fine-grained sediments (maximum within the fraction 20–63 μm) contribute 3–25 % to the nearshore sediments. Drastic changes in the biological zonation (like the mass invasion of the sea urchin Paracentrotus lividus in the Northern Adriatic since 1972 which eliminated nearly the entire macrophyte zone) due to unknown factors or pollution can have a profound effect on the bioerosion rates, altering them by as much as a factor of ten."],["dc.identifier.doi","10.1111/j.1439-0485.1983.tb00287.x"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61766"],["dc.language.iso","en"],["dc.notes.status","final"],["dc.relation.issn","0173-9565"],["dc.relation.issn","1439-0485"],["dc.title","Biokarst on Limestone Coasts, Morphogenesis and Sediment Production"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","2259"],["dc.bibliographiccitation.issue","12"],["dc.bibliographiccitation.journal","Journal of General Virology"],["dc.bibliographiccitation.lastpage","2264"],["dc.bibliographiccitation.volume","65"],["dc.contributor.author","Yamamoto, N."],["dc.contributor.author","Okada, M."],["dc.contributor.author","Hinuma, Y."],["dc.contributor.author","Hirsch, F. W."],["dc.contributor.author","Chosa, T."],["dc.contributor.author","Schneider, J."],["dc.contributor.author","Hunsmann, G."],["dc.date.accessioned","2022-10-06T13:35:39Z"],["dc.date.available","2022-10-06T13:35:39Z"],["dc.date.issued","1984"],["dc.identifier.doi","10.1099/0022-1317-65-12-2259"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/116149"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-602"],["dc.relation.eissn","1465-2099"],["dc.relation.issn","0022-1317"],["dc.relation.orgunit","Deutsches Primatenzentrum"],["dc.title","Human Adult T-Cell Leukaemia Virus Is Distinct from a Similar Isolate of Japanese Monkeys"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","227"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Hydrobiologia"],["dc.bibliographiccitation.lastpage","232"],["dc.bibliographiccitation.volume","143"],["dc.contributor.author","Schneider, Jürgen"],["dc.contributor.author","Müller, Jens"],["dc.contributor.author","Sturm, Michael"],["dc.date.accessioned","2019-07-19T09:17:58Z"],["dc.date.available","2019-07-19T09:17:58Z"],["dc.date.issued","1986"],["dc.description.abstract","Traunsee was formed by glacial overdeepening of a pre-existing fault system. Present-day morphology is characterized by a deep (189 m) narrow trough with steep slopes (>50°) in the southern part surrounded by the Northern Calcareous Alps. The northern part of the lake is bordered by flysch and glacial deposits with gentle slopes (<30°) and exhibits several ridges, basins and troughs. During the late and postglacial period, more than 45 m of sediment has accumulated in the central basin. Sedimentation in the southern part of Traunsee is mainly controlled by the river Traun forming a prograding delta in the south and — within the past 50 years — by industrial tailings consisting mainly of calcite. Sediments are distributed by undercurrents and by turbidites. Cores from the central basin thus show an intercalation of Traun-derived dolomite-rich sediments with anthropogenic muds from the tailings deposited up to more than 6 km from its source. Within the northern basin, land slides from the flysch region played an important role leading to drastic changes in the morphology of slopes and adjacent basins. These slumps have persisted until historic times. Sedimentation in the shallow sublittoral regions is dominated by benthic biogenic decalcification. The frequency of turbidite sedimentation within the profundal basin decreased during the last 200 years probably due to man's activities in the drainage area such as regulation of rivers and torrents. Sedimentation rates during the past decades range from 2–3 cm/a in the southern basin to 0.4 cm/a in the northern part as shown by 137Cs-dating."],["dc.identifier.doi","10.1007/BF00026666"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61763"],["dc.language.iso","de"],["dc.notes.status","final"],["dc.relation.issn","0018-8158"],["dc.relation.issn","1573-5117"],["dc.title","Geology and sedimentary history of Lake Traunsee (Salzkammergut, Austria)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","57"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Medical Microbiology and Immunology"],["dc.bibliographiccitation.lastpage","64"],["dc.bibliographiccitation.volume","173"],["dc.contributor.author","Yamamoto, N."],["dc.contributor.author","Hayami, M."],["dc.contributor.author","Komuro, A."],["dc.contributor.author","Schneider, J."],["dc.contributor.author","Hunsmann, G."],["dc.contributor.author","Okada, M."],["dc.contributor.author","Hinuma, Y."],["dc.date.accessioned","2022-10-06T13:27:05Z"],["dc.date.available","2022-10-06T13:27:05Z"],["dc.date.issued","1984"],["dc.identifier.doi","10.1007/BF02123570"],["dc.identifier.pii","BF02123570"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/115246"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-602"],["dc.relation.eissn","1432-1831"],["dc.relation.issn","0300-8584"],["dc.relation.orgunit","Deutsches Primatenzentrum"],["dc.title","Experimental infection of cynomolgus monkeys with a human retrovirus, adult T-cell leukemia virus"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","233"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Hydrobiologia"],["dc.bibliographiccitation.lastpage","246"],["dc.bibliographiccitation.volume","143"],["dc.contributor.author","Behbehani, Ahmad-Reza"],["dc.contributor.author","Müller, Jens"],["dc.contributor.author","Schmidt, Roland"],["dc.contributor.author","Schneider, Jürgen"],["dc.contributor.author","Schröder, Heinz-Gerd"],["dc.contributor.author","Strackenbrock, Ines"],["dc.contributor.author","Sturm, Michael"],["dc.date.accessioned","2019-07-19T09:22:25Z"],["dc.date.available","2019-07-19T09:22:25Z"],["dc.date.issued","1986"],["dc.description.abstract","Attersee represents a good example of a lake situated in the Northern forelands of the Northern Calcareous Alps and influenced by different sediment-supplying processes during the postglacial. Several compounds, of different origin, form the sediments of the basin. Clastics which are mainly composed of dolomites derive from the Northern Calcareous Alps. Clastic input of organic and inorganic particles is accomplished by rivers and landslides. They are responsible for the main input of siliciclasts like quartz, feldspar and mica. A high proportion of the sediment results from autochthonous biogenic carbonate precipitation. In the shallow sublittoral areas of the northern part of the lake benthic decalcification caused by encrusting macroand micro-phytes is dominant, while in the southern and central parts of the lake epilimnetic decalcification caused by the blooming of phytoplancton is more important during summer. The total biogenic calcium carbonate production reaches about 11 000 to 12 000 metric tons a year. Nutrients and residues of cyanophytes (Oscillatoria rubescens) deriving from the eutrophic lake Mondsee were washed into lake Attersee by the Mondseeache. High amount of phosphorus in the sediments of the southern basin depicts local eutrophication in the mouth area of the Mondseeache. The average sedimentation rate in lake Attersee can be determined by different dating methods. Sedimentation rates increased during the last 110 years from 1 mm a year to 1.8–2 mm a year as a result of human activities. Five main phases in the postglacial sedimentary history can be recognized: Würm moraines and finely banded varves (before 13 000 B.P.), the early Attersee stage (from 13 000 B.P. up to 1200 B.P.), and the later Attersee stage after the Bavarian colonization (from 1 200 B.P. on). Using heavy metal and isotope analyses the sedimentary history can be reconstructed in more detail for the last 100 years."],["dc.identifier.doi","10.1007/BF00026667"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61765"],["dc.language.iso","en"],["dc.notes.status","final"],["dc.relation.issn","0018-8158"],["dc.relation.issn","1573-5117"],["dc.title","Sediments and sedimentary history of Lake Attersee (Salzkammergut, Austria)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","775"],["dc.bibliographiccitation.lastpage","821"],["dc.bibliographiccitation.volume","6"],["dc.bibliographiccitation.volumetitle","Protection: RESEARCH, SEALING AND CROSS-CUTTING ISSUES"],["dc.contributor.author","Burghardt, Wolfgang"],["dc.contributor.author","Banko, G."],["dc.contributor.author","Höke, S."],["dc.contributor.author","Hursthouse, A."],["dc.contributor.author","L´Escaille, T. de"],["dc.contributor.author","Ledin, S."],["dc.contributor.author","Marsan, F. A."],["dc.contributor.author","Sauer, Daniela"],["dc.contributor.author","Stahr, Karl"],["dc.contributor.author","Amann, E."],["dc.contributor.author","Quast, J."],["dc.contributor.author","Nerger, M."],["dc.contributor.author","Schneider, J."],["dc.contributor.author","Kuehn, K."],["dc.contributor.editor","Camp, L. B. Van"],["dc.date.accessioned","2017-09-07T11:49:09Z"],["dc.date.available","2017-09-07T11:49:09Z"],["dc.date.issued","2004"],["dc.identifier.gro","3149613"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/6297"],["dc.language.iso","en"],["dc.notes.status","public"],["dc.notes.submitter","chake"],["dc.publisher","Office for Official Publications of the European Communities"],["dc.publisher.place","Luxembourg"],["dc.relation.ispartof","Reports of the Technical Working Groups established under the Thematic Strategy for Soil"],["dc.title","Task Group 5 on Sealing soils, soils in urban areas, land use and land use planning"],["dc.type","book_chapter"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","2678"],["dc.bibliographiccitation.issue","21-22"],["dc.bibliographiccitation.journal","Quaternary Science Reviews"],["dc.bibliographiccitation.lastpage","2681"],["dc.bibliographiccitation.volume","25"],["dc.contributor.author","Nitychoruk, J."],["dc.contributor.author","Binka, K."],["dc.contributor.author","Ruppert, Hans"],["dc.contributor.author","Schneider, J."],["dc.date.accessioned","2018-11-07T09:04:19Z"],["dc.date.available","2018-11-07T09:04:19Z"],["dc.date.issued","2006"],["dc.description.abstract","The problem of correllating the Holsteinian Interglacial with the Marine Isotope Stage (MIS) is still disputed. Generally, a view persists that this interglacial should be linked with MIS 11, although this approach has many adversaries. Palynologic and geochemical data from well preserved fossil lake deposits from the Holstemian Interglacial in eastern Poland have enabled their correlation with MIS 11. (c) 2006 Elsevier Ltd. All rights reserved."],["dc.identifier.doi","10.1016/j.quascirev.2006.07.004"],["dc.identifier.isi","000243286300002"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/25091"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0277-3791"],["dc.title","Holsteinian Interglacial = Marine Isotope Stage 11?"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","401"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Hydrobiologia"],["dc.bibliographiccitation.lastpage","405"],["dc.bibliographiccitation.volume","143"],["dc.contributor.author","Müller, Jens"],["dc.contributor.author","Schneider, Jürgen"],["dc.contributor.author","Sturm, Michael"],["dc.date.accessioned","2019-07-19T09:19:09Z"],["dc.date.available","2019-07-19T09:19:09Z"],["dc.date.issued","1986"],["dc.description.abstract","Tailings from salt work and a soda work have been pumped into the southern part of Traunsee (bay of Ebensee) for more than 50 years. Solid wastes have accumulated to form a pile > 40 m high with a total volume of > 3 × 106 m3. The sandy silty mud consists of calcite and other phases of CaCO3, brucite, CaO resp. Ca(OH)2 and gypsum. The chemical environment of the mud is characterized by extreme alkaline pore water (pH > 10 up to 12.5; total amount of pore water: 3 × 106 t) and highly negative Eh-values. These values result from the pumped tailings and from postdepositional chemical processes such as dissolution resp. reaction of CaO, brucite and gypsum and precipitation of CaCO3."],["dc.identifier.doi","10.1007/BF00026689"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61764"],["dc.language.iso","en"],["dc.notes.status","final"],["dc.relation.issn","0018-8158"],["dc.relation.issn","1573-5117"],["dc.title","Industrial tailings in Lake Traunsee (Salzkammergut, Austria)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","167"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Medical Microbiology and Immunology"],["dc.bibliographiccitation.lastpage","170"],["dc.bibliographiccitation.volume","173"],["dc.contributor.author","Hunsmann, G."],["dc.contributor.author","Bayer, H."],["dc.contributor.author","Schneider, J."],["dc.contributor.author","Schmitz, H."],["dc.contributor.author","Kern, P."],["dc.contributor.author","Dietrich, M."],["dc.contributor.author","Büttner, D. W."],["dc.contributor.author","Goudeau, A. M."],["dc.contributor.author","Kulkarni, G."],["dc.contributor.author","Fleming, A. F."],["dc.date.accessioned","2022-10-06T13:27:06Z"],["dc.date.available","2022-10-06T13:27:06Z"],["dc.date.issued","1984"],["dc.identifier.doi","10.1007/BF02123765"],["dc.identifier.pii","BF02123765"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/115249"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-602"],["dc.relation.eissn","1432-1831"],["dc.relation.issn","0300-8584"],["dc.relation.orgunit","Deutsches Primatenzentrum"],["dc.title","Antibodies to ATLV/HTLV-1 in Africa"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","291"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Virology"],["dc.bibliographiccitation.lastpage","298"],["dc.bibliographiccitation.volume","150"],["dc.contributor.author","Jurkiewicz, E."],["dc.contributor.author","Nakamura, H."],["dc.contributor.author","Schneider, J."],["dc.contributor.author","Yamamoto, N."],["dc.contributor.author","Hayami, M."],["dc.contributor.author","Hunsmann, G."],["dc.date.accessioned","2022-10-06T13:32:38Z"],["dc.date.available","2022-10-06T13:32:38Z"],["dc.date.issued","1986"],["dc.identifier.doi","10.1016/0042-6822(86)90290-4"],["dc.identifier.pii","0042682286902904"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/115429"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-602"],["dc.relation.issn","0042-6822"],["dc.relation.orgunit","Deutsches Primatenzentrum"],["dc.title","Structural analysis of p19 and p24 core polypeptides of primate lymphotropic retroviruses (PLRV)"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dspace.entity.type","Publication"]]