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Showing 61-80 of 89 results
  1. Structure of the precambrian sedimentary cover and upper part of the basement in the Central Russian Aulacogen and Orsha Depression (East European Platform)

    The Precambrian sedimentary section and upper part of the basement of the Central Russian Aulacogen and Orsha Depression, two largest structures...

    N. P. Chamov, V. V. Kostyleva, A. F. Veis in Lithology and Mineral Resources
    Article 21 January 2010
  2. Viable Cyanobacteria and Green Algae from the Permafrost Darkness

    This review represents an overview of the existence, distribution and abundance of the photoautotrophic microorganisms in the deep subsurface...
    Tatiana A. Vishnivetskaya in Permafrost Soils
    Chapter 2009
  3. Microfossils from the Arymas and Debengda formations, the Riphean of the Olenek Uplift: Age and presumable nature

    Studied assemblages of diverse organic-walled microfossils separated from the Arymas and Debengda formations of the Olenek Uplift include several...

    A. M. Stanevich, E. N. Maksimova, ... T. V. Donskaya in Stratigraphy and Geological Correlation
    Article 24 February 2009
  4. On the nature of the Precambrian microfossils Arctacellularia and Glomovertella

    Possible phylogenetic relationships between the organic-walled microfossils of the form genus Arctacellularia Hermann, 1976, representing chainlike...

    T. N. Hermann, V. N. Podkovyrov in Paleontological Journal
    Article 01 October 2008
  5. Postglacial sedimentary record and history of West Hawk Lake crater, Manitoba

    West Hawk Lake (WHL) is located within the glacial Lake Agassiz basin, 140 km east of Winnipeg, Manitoba. The small lake lies in a deep, steep-sided,...

    James T. Teller, Zhirong Yang, ... Alice M. Telka in Journal of Paleolimnology
    Article 05 March 2008
  6. New Riphean microbiotas of the Billyakh Group, the north Anabar region (Fomich River basin): To Riphean biostratigraphy of the Siberian platform

    Excellently preserved organic-walled and silicified microfossils are first found in the Lower Riphean Ust-Il’ya and Kotuikan formations of the...

    V. N. Sergeev, N. G. Vorob’eva, P. Yu. Petrov in Stratigraphy and Geological Correlation
    Article 01 February 2007
  7. Principal stages in evolution of Precambrian organic world: Communication 1. Archean and Early Proterozoic

    Expounded in this work are the results of critical consideration of published and original data on biologic nature and appearance chronology of...

    V. N. Sergeev, M. A. Semikhatov, ... N. G. Vorob’eva in Stratigraphy and Geological Correlation
    Article 01 April 2007
  8. The importance of Precambrian microfossils for modern biostratigraphy

    A new model of the distribution of Proterozoic microorganisms is developed, based on studies of Riphean and Vendian silicified and organic-walled...

    V. N. Sergeev in Paleontological Journal
    Article 01 October 2006
  9. Habitats and probable nature of acritarchs from the Upper Riphean Chencha Formation

    Morphology and taphonomy of acritarchs from the Upper Riphean deposits of the Baikal Folded Region (eastern Siberia) are analyzed. The morphotypes of...

    A. M. Stanevich, E. N. Chatta, ... V. K. Nemerov in Paleontological Journal
    Article 01 February 2007
  10. Palaeobiology of Mesoproterozoic Salkhan Limestone, Semri Group, Rohtas, Bihar, India: Systematics and significance

    Mesoproterozoic (∼ 1600 Ma old) Salkhan Limestone (Semri Group) of the Vindhyan Supergroup, exposed in Rohtas district of Bihar, India, preserves an...

    Article 01 February 2006
  11. DIVERSITY, DISTRIBUTION AND BIOGEOCHEMICAL SIGNIFICANCE OF NITROGEN-FIXING MICROORGANISMS IN ANOXIC AND SUBOXIC OCEAN ENVIRONMENTS

    Nitrogen fixation, the reduction of atmospheric dinitrogen (N2) to biologically available ammonium, has been important in the balance of biologically...
    Jonathan P. Zehr, Matthew J. Church, Pia H. Moisander in Past and Present Water Column Anoxia
    Conference paper 2006
  12. The History of Recent Limnological Changes and Human Impact on Upper Klamath Lake, Oregon

    Hypereutrophic Upper Klamath Lake has been studied for almost 50 years to evaluate the nature, cause, and effects of its very productive waters....

    J. Platt Bradbury, Steven M. Colman, Richard L. Reynolds in Journal of Paleolimnology
    Article 01 February 2004
  13. Anomalous magnetic susceptibility values and traces of subsurface microbial activity in carbonate banks on San Salvador Island, Bahamas

    Pure limestones beneath the paleosols on San Salvador Island, Bahamas, contain strong positive magnetic susceptibility anomalies, although the iron...

    J. Hladil, J. L. Carew, ... A. Langrova in Facies
    Article 08 June 2004
  14. A 1500-year record of climatic and environmental change in ElkLake, Minnesota III: measures of past primary productivity

    Diatom analysis of a varved sediment core from Elk Lake, Minnesotadocuments important natural and human-caused shifts in primary productivity...

    Platt Bradbury, Brian Cumming, Kathleen Laird in Journal of Paleolimnology
    Article 01 April 2002
  15. Subaerial Microbial Mats and Their Effects on Soil and Rock

    Microbial mats (or biofilms) under permanent water cover contain 95–98% biologically stabilised water at ambient temperature, while biofilms in...
    Anna A. Gorbushina, Wolfgang E. Krumbein in Microbial Sediments
    Chapter 2000
  16. Anthropogenic changes in the sediment composition of Lake Gości& aogon;ż (central Poland), during the last 330 yrs*

    According to historical sources, the development of settlement around Lake Gości& aogon;ż during the last 330 yrs was intense at two time periods:...

    Tomasz Goslar, Magdalena Ralska-Jasiewiczowa, ... Adam Walanus in Journal of Paleolimnology
    Article 01 September 1999
  17. A summary of past and recent plankton of Lake Winnipeg, Canada using algal fossil remains

    Although the phytoplankton and protozoan assemblages of Lake Winnipeg are quite variable both, spatial and temporally, knowledge of their current...

    H. J. Kling in Journal of Paleolimnology
    Article 01 March 1998
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