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Morphology of microbes and microbial communities at ...
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Morphology of microbes and microbial communities at the 52°C Big Spring and outflow channel at Thermopolis, Wyoming
Morphology of microbes and microbial communities at the 52°C Big Spring and outflow channel at Thermopolis, Wyoming
Name:Personal
Colgin, Nicolas Role :Text(marcrelator)
creator
Colgin, Nicolas Role :Text(marcrelator)
creator
Name:Personal
Hammer, Selena Role :Text(marcrelator)
creator
Hammer, Selena Role :Text(marcrelator)
creator
Name:Personal
Lyon, Andrea Role :Text(marcrelator)
creator
Lyon, Andrea Role :Text(marcrelator)
creator
Name:Personal
Veggian, Cheryl Role :Text(marcrelator)
creator
Veggian, Cheryl Role :Text(marcrelator)
creator
Name:Personal
Smaglik, Suzanne M. Role :Text(marcrelator)
contributor
Smaglik, Suzanne M. Role :Text(marcrelator)
contributor
Name:Personal
McAllister, Steven J. Role :Text(marcrelator)
contributor
McAllister, Steven J. Role :Text(marcrelator)
contributor
typeOfResource
still image genre
Origin Information
Place
Laramie, Wyoming
University of Wyoming (keyDate="yes")
2009-05-13
Laramie, Wyoming
University of Wyoming (keyDate="yes")
2009-05-13
Language:Text
eng
eng
Physical Description
born digtal
born digtal
abstract
The Big Spring at Thermopolis is roughly 5 m in diameter, with a 4 m outflow channel 150 m in length to the first cooling pond. The mineral-rich 52-54°C water flowing from the spring is the result of groundwater flow from the Owl Creek Mountains to the south, intersecting an east-west fault-line beneath the Thermopolis valley. Water and microbial samples have been collected on a semi-regular basis from August 2008 to present. We describe microbial communities, the microbe types within them, and how they change “downstream” at 11 sites from the inflow to the outflow, and 5 sites beyond the cooling ponds. The main spring supports a multitude of pigmented bacteria: a thin green layer covering a thicker reddish-brown layer, a growth pattern typical of cyanobacteria; purple and green filamentous bacteria; and yellow spongiform mats around the edges. There is a clear distinction of morphologies of the microbial communities with distance from the outflow. In the outflow channel the morphology changes from green to white filamentous and biofilms near the outflow, to algal mats with abundant trapped gas bubbles, to spongiform mats and vertical columns pushed upward by trapped gas bubbles within the mat, at the edge of the cooling pond. note
From - Undergraduate Research Day 2009 - Celebration of Research - Abstracts
Subject
microbial communities
microbial communities
Subject
Big Spring at Thermopolis
Big Spring at Thermopolis
Related Item:series
Title Information
Undergrauate Research Day 2009
Undergrauate Research Day 2009
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(usage="primary display")
accessCondition:useAndReproduction
http://digital.uwyo.edu/copyright.htm
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languageOfCataloging
:Text(ISO639-2B)
English :Code(ISO639-2B)
eng
English :Code(ISO639-2B)
eng