1-4 OF 4 RESULTS FOR

autotropism

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Image
Showing the microplankton raw data record for the same interval as Figure 12, the marginal-marine–terrestrial depositional environment of this succession is marked by the low frequencies of microplankton and their sporadic distribution. Pulses of inner neritic marine facies are recorded in the Hildasay Member section and at the base of sequence T45. These are characterized by the autotropic gonyaulacoid dinocysts C. comatum, I ligospinosum and S, ramosus subsp ramosus. A similar association is seen in the middle neritic sediments of the Lamba Formation at the base of the figure. Here, the dinocyst A. gippingensis is significant both in age, not occurring in sediments younger than sequence T38, and also as an indicator of eutrophic turbid shelf conditions. Further flooding surfaces are marked by brackish to freshwater marginal-marine taxa. A flooding surface at the base of LAZ Rc3 is marked by a brackish water flora containing B braunii (a chrolophycean algae) and the acritach Leiosphera spp, A second dominantly freshwater flooding event is seen within LAZ Rc5, marked by the freshwater taxa B braunii, S. parvus (a Spirogyra type) and the turbid water, arenaceous facies acritarch P. indentata. It is of interest to integrate this microplankton palynoflora with the pollen and spore record for the same interval (Fig. 12). This is dominated by floating freshwater ferns (Azolla), bulrushes (S. magnoides), and the mire/transitional swamp taxa P. platycaryroides and C veripites. This interval can be interpreted as broadly freshwater estuarine with a flanking complex floodplain overbank zone of lakes, mire and transitional swamps. Understanding of the ecology and the seral successional composition of Palaeogene microplankton and higher plant communities is essential for the appreciation of environmental controls on biostratigraphical events, and hence their stratigraphical utility.
Published: 16 July 2013
are recorded in the Hildasay Member section and at the base of sequence T45. These are characterized by the autotropic gonyaulacoid dinocysts C. comatum, I ligospinosum and S, ramosus subsp ramosus . A similar association is seen in the middle neritic sediments of the Lamba Formation at the base
Journal Article
Published: 16 July 2013
Petroleum Geoscience (2013) 19 (3): 273–288.
... are recorded in the Hildasay Member section and at the base of sequence T45. These are characterized by the autotropic gonyaulacoid dinocysts C. comatum, I ligospinosum and S, ramosus subsp ramosus . A similar association is seen in the middle neritic sediments of the Lamba Formation at the base...
FIGURES
First thumbnail for: Development of intra-basaltic lava-field drainage ...
Second thumbnail for: Development of intra-basaltic lava-field drainage ...
Third thumbnail for: Development of intra-basaltic lava-field drainage ...
Journal Article
Published: 28 January 2016
Geochemistry: Exploration, Environment, Analysis (2016) 16 (1): 85–99.
... gradients are most favourable for autotropic organisms. This may be an analytical artifact because autotrophic organisms commonly colonize electrode surfaces (e.g. Parra & Lin 2009 ). This yields erroneous ORP values relative to the bulk inorganic oxidation potential of the soil slurry...
FIGURES
First thumbnail for: Geochemical processes in the formation of ‘forest ...
Second thumbnail for: Geochemical processes in the formation of ‘forest ...
Third thumbnail for: Geochemical processes in the formation of ‘forest ...
Journal Article
Published: 03 October 2019
Quarterly Journal of Engineering Geology and Hydrogeology (2019) 52 (4): 481–500.
... rocks, through conversion in metamorphic rocks and in sedimentary environments by the metabolic processes of autotropic bacteria. Such bacteria reduce sulfates derived from saline waters and form framboids a few micrometres in size, as illustrated in Figure 1a and b . The anoxic conditions required...
FIGURES
First thumbnail for: Tackling problems in civil engineering caused by t...
Second thumbnail for: Tackling problems in civil engineering caused by t...
Third thumbnail for: Tackling problems in civil engineering caused by t...