Daniel P. Bradley February 19 th, 2011 Winter Ecology Mountain Research Station, University of Colorado, Boulder EBIO 4100, Sec 570.

Slides:



Advertisements
Similar presentations
Biology 3A – human impact
Advertisements

Planet Earth.
– Winter Ecology. Introduction  Global Climate Change  How microbs may be affected by snowpack depth  Temperature/precipitation trends.
The effect of trees on snowpack: live versus dead lodgepole pines in subalpine forest Dylan Brown Winter Ecology Spring 2014 Mountain Research Station,
Affects of Varying Litter Types and Moisture on Soil pH Under Snowpack
Impact of snow molds on conifers of the ribbon forest Max Owens EBIO 4100, Spring 2013 Winter Ecology Mountain Research Station University of Colorado-Boulder.
How Thickness of Chlorophyll in Aspen Bark is dependent on Height and Stand type. Lizabeth Rodriguez Winter Ecology Spring 2014 CU Mountain Research Station.
The Biosphere.
Winter Ecology Spring 2009 Mountain Research Station, University of Colorado, Boulder.
Sensing Winter Soil Respiration Dynamics in Near-Real Time Alexandra Contosta 1, Elizabeth Burakowski 1,2, Ruth Varner 1, and Serita Frey 3 1 University.
How do snowpack depth and proximity to trees affect subnivean plant growth Robin Reibold Winter Ecology: Spring 2014 Mountain Research Station, University.
METEOROLOGIST KISHAN SRIPADA TEMPERATE DECIDUOUS FOREST.
Roadmap for remaining lectures: 1.Combine the abiotic world (Earth + Climate) with the biotic world (life). A. First talk about “Ecosystems”, and generally.
Niwot Ridge By: Kate Edwards GEOG 4401/5401 Soils Geography Fall 2007 – Univ of Colorado, Boulder.
Introduction Subalpine meadows play a crucial role in species diversity, supporting many endangered species of plant and wildlife. Subalpine meadows play.
DIFFERENCES IN SOIL RESPIRATION RATES BASED ON VEGETATION TYPE Maggie Vest Winter Ecology 2013 Mountain Research Station.
PRESENTED BY: ANDREW CARROLL WINTER ECOLOGY: SPRING SEMESTER 2013 MOUNTAIN RESEARCH STATION, UNIVERSITY OF COLORADO, BOULDER Bark Beetle’s Affect on Winter.
 Vegetation Density and Snow Accumulation Evan Esfahani Winter Ecology 2014 Mountain Research Station.
Winter Ecology, MRS 2013 Project by Rob McFadzean.
Nick Herdeg Winter Ecology: Spring 2014 Mountain Research Station, University of Colorado, Boulder.
Niwot Ridge-Green Lakes Valley LTER Niwot Ridge-Green Lakes Valley LTER Site Matt Miller
Supranivean travel of snowshoe hares on Niwot Ridge Marieta Bialek EBIO 4100 Winter Ecology Spring 2012.
Biomes and Climate.
Influences of Stationary Objects on Winter Subnivean Micro-Environments David Olson - Ebio 4120 – Spring 2010 Source: freestockphotos.com Winter Ecology.
Climate Zones.
The Biosphere and its Biomes
Winter and its effects on Soil Respiration Sara Fairchild Winter Ecology – Spring 2009 Mountain Research Station – University of Colorado, Boulder.
Ecosystems. Primary Vocabulary Terms o Ecosystem o Biomass o Law of Conservation of Energy o Law of Conservation of Matter o Trophic levels o Detritus.
The Impact of Forest on Snowpack Stability A presentation by Miles Daly 3/1/08 Winter Ecology Field Course Mountain Research Station, University of Colorado,
Soil Respiration Unit: Soil Science. Objectives O Define: soil respiration and soil microbes O Explain the role of soil respiration in determining soil.
Ethan Larson MRS, University of Colorado-Boulder Spring 2013.
Short-term changes in snowpack due to weather Sean Sutherland  University of Colorado, Boulder  EBIO 4100, Winter Ecology Spring 2011  Mountain Research.
Canopy Dynamics and Tree Well Size Does the canopy height and size of coniferous trees affect the size of the tree well at the snow surface? J. Kalin Puent.
The relationship between snow depth and soil respiration in upper montane winter environments Claire Hierseman Winter Ecology Spring 2013 Mountain Research.
Empirical determination of N critical loads for alpine vegetation William D. Bowman, Julia L. Gartner, Keri Holland, and Magdalena Wiedermann Department.
The effect of tree density and height on tree-flagging of Lodgepole Pines in Niwot’s sub-alpine forest Michael D. Schuster Winter Ecology – Spring 2010.
Winter Soil Respiration Near Dead and Living Lodgepole Pines at Niwot Ridge, CO Justin D’Atri Winter Ecology Spring 2010 Mountain Research Station – University.
MonthDayTopic Nov.8Individuals to populations 10Holiday! 13Populations to communities 15Community patterns 17Ecosystems 20Film-1 st showing 22Film-2 nd.
Subalpine soil microbial response to compaction of snow pack by snowmobiles Elizabeth Golden EBIO 4100, Winter Ecology, Spring 2013 Mountain Research Station,
Energy Flow Through the Biosphere
BIOGEOCHEMISTRY. What is Biogeochemistry? The study of the biological, geological and chemical factors that influence the movement of chemical elements.
Are the Snowpack Structures Different Between the Riparian and Upland Environments? Allie B. Cunningham Winter Ecology Spring 2015 CU Mountain Research.
Genesis Machek Winter Ecology, Spring 2010 Mountain Research Station - University of Colorado at Boulder.
Ecology Study of the relationships between organisms and their environments Study of the relationships between organisms and their environments Their interactions.
Are we polluting the Ridge’s precipitation? A study by Garrett Porter located on Niwot Ridge, Colorado. Performed on February 6, 2010 and presented on.
A snowpack comparison between a limber pine site and a spruce site within a spruce forest Sam Sartwell, Winter Ecology, EBIO 4100, Spring 2014, CU Mountain.
Kate Lonner Winter Ecology Spring 2015 Mountain Research Station, University of Colorado, Boulder.
How do soil temperature fluctuations affect water content? Winter Ecology Course CU Mountain Research Station Spring 2015 Evan Franklin.
MICROBE ACTIVITY COMPARISON BETWEEN NORTH AND SOUTH FACING SLOPES Jake DePompolo CU Mountain Research Station 2015.
The Influence of Vegetation Type on Winter Soil Respiration Rates Scott Clingan Winter Ecology Spring 2014.
CLIMATE. What is Climate?  Climate is the average conditions of temperature and precipitation in a particular area.  Caused by many factors including:
The Biosphere Chapter 3. What is Ecology? Ecology The study of the interactions among organisms and between organisms their environment.
Climate and Life. Climate Different than weather Climate is about averages –Average temperature, average humidity, average precipitation Climate affects.
Samuel T. Dunn 1, 2, Andrew G. Bunn 3, John D. Schade 1
Taylor Conte1, Elizabeth Burakowski2
Microbial Respiration in Soil Surrounding Aspen Trees
Biosphere.
Forestry and the Carbon Cycle
Where did your dinner come from?
A Comparison of Riparian Vegetation Structures
Spatial and Temporal Soil Respiration in the Subalpine
Winter Ecological Interactions between Alpine and Subalpine Ecosystems
Landscape Features Affecting Squirrel Cache Density and Location
The study of organisms and their environment
Ecology.
Decomposition and development:
BIOGEOCHEMISTRY Nitrogen Cycle Slide:
Chapter 18: Ecology.
Ecology                                          .
Tina Nguyen Vegetation Ecology Summer 2018
Presentation transcript:

Daniel P. Bradley February 19 th, 2011 Winter Ecology Mountain Research Station, University of Colorado, Boulder EBIO 4100, Sec 570

Life in the Winter Soils Soil microbes in snow covered soils are respiring every minute, consuming available nutrients, and off-gassing them as CO 2 (King 08). Our class experiment: g (0.653 oz) of carbon could be converted into CO 2 in 186 days (Oct 25 – May 1), in ~100 cm 2 (Winter Eco 11). Winter soil: An ideal environment for microbial life.

Pro’s and Con’s of Winter Microbial Life Pro’s Con’s Highly protected Predatory, UV Highly stable Temperature Water supply via the snowpack, varying (Brooks 96) A specialized niche Food Supply High, but non-replenishing Temperature Not ideal for metabolic processes

The Food Supply The food supply in a finite amount We can assume that the amount of food is equal throughout the forest.

Question If food is limited by the cover of the snowpack, does the depth of the snowpack affect the amount of carbon (food) in the soil? H A : There is a difference in soil carbon between sites of varying snowpack. H O : There is not a difference in soil carbon

Methods A deep and shallow site were found on Feb 5 th Five samples for each site were taken, with 2 sub sites for each site, from the top 5cm of the soil. The soils were refrigerated maintain metabolic processes The soils were then sieved, weighed into 5 gram samples The samples were dried, combusted and weighed. Percent differences and averages were derived.

The Sites CU Mountain Research Station - Google Earth

Results The data show that there was a significant difference (p- value ≤ 0.05) in soil carbon between the sites

The Data p-value = (paired t-test) Mean percent difference: deep=0.1057, shallow=0.3322

The Data p-value = (paired t-test) Mean difference, in grams: deep=0.0056, shallow=0.0182

Discussion The shallow snowpack had more carbon underneath it, why? Carbon is limiting for microbes, lower carbon indicates higher microbe populations/activity (Nemergut 11). Temperature swings. What is affecting snowpack? Wind, Precipitation What is affecting the amount of carbon (litter) under the snowpack? Beetle kill?

Summary Snowpack does have an affect on the microbial population of the soil, via carbon. More snowpack, more respiration, more carbon consumed.

Literature Cited Brooks, Paul D., Mark W. Williams, and Steven Schmidt. "Microbial Activity under Alpine Snowpacks, Niwot Ridge, Colorado " Biogeochemistry 32.2 (1996) Mark Williams. Web. 25 Jan King, A. J., A. F. Meyer, and S. K. Schmidt. "High Levels of Microbial Biomass and Activity in Unvegetated Tropical and Temperate Alpine Soils." Soil Biology and Biochemistry (2008): ScienceDirect. Web. 25 Jan Nemergut, Diana, CU-Boulder, INSTAAR. Personal interview. 16 Feb Winter Ecology 2011, and T. Kittle. TS. CU-Boulder, Mountain Research Station.