Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Lee Coshell"'
Autor:
Christopher R. Omelon, Lee Coshell, Michael R. Rosen, John G. Warden, Katinka X. Ruthrof, Daniel O. Breecker
Publikováno v:
Geobiology. 17:536-550
Modern microbialites are often located within groundwater discharge zones, yet the role of groundwater in microbialite accretion has yet to be resolved. To understand relationships between groundwater, microbialites, and associated microbial communit
Publikováno v:
Journal of Hydrology. 560:495-511
Lake Hayward is one of only about 30 hypersaline lakes worldwide that is meromictic and heliothermal and as such behaves as a natural salt gradient solar pond. Lake Hayward acts as a local groundwater sink, resulting in seasonally variable hypersalin
Publikováno v:
Sedimentary Geology. 148:357-371
Terrestrial sediments are generally simple to differentiate from lacustrine sediments, but the interface between the two is difficult to recognise when clean beach sand is absent. In addition, tracing the dispersal of pollutant trace metals at this i
Publikováno v:
Sedimentology. 45:1005-1018
Holocene stromatolites are described from Lake Walyungup, a coastal hyposaline lake in south-western Australia. At summer low water, this groundwater-fed depression comprises two permanent shallow water bodies and an ephemeral southern pool, set with
Publikováno v:
Sedimentology. 45:579-594
Development of a diagenetic anhydrite bed at the base of the Cretaceous Maha Sarakham Saline Formation (the ‘Basal Anhydrite’ member) of the Khorat Plateau in north-eastern Thailand took place due to leaching and/or pressure dissolution of salt a
Publikováno v:
Geochimica et Cosmochimica Acta. 59:979-990
The δ180 of carbonate minerals in a seasonally stratified hypersaline lake are > +2.3% PDB and are inconsistent with calculated δ18O values for carbonate in equilibrium with the lake water during the spring and winter. When the lake is stratified,
Autor:
Michael R. Rosen, Lee Coshell
Publikováno v:
Sedimentology. 39:161-166
Holocene dolomite forms in the sediment of Lake Hayward, a small permanent hypersaline lake in the Clifton-Preston Lakeland System, Western Australia. The geomorphological setting of dolomite formation in Lake Hayward is similar to the Coorong region