TICK COLLECTION CRITERIA Project title Michael Cherry| Dr. Ben Clarke| Bridges and Pathways Program 2010.

Slides:



Advertisements
Similar presentations
6.3 Natural processes break down rocks
Advertisements

Carbon stocks in a miombo woodland landscape: spatial distributions and controls Emily Woollen, Mathew Williams, Casey Ryan and John Grace The University.
Nitrogen Mineralization Across an Atmospheric Nitrogen Deposition Gradient in Southern California Deserts Leela E. Rao 1, David R. Parker 1, Andrzej Bytnerowicz.
Soil Horizons. Organic Layer (O-horizon) The uppermost layer; it is rich in organic material. Plant litter accumulates in the O- horizon and gradually.
SOIL. WHAT IS SOIL? SOIL IS A MATERIAL THAT FORMS THE CRUST OF THE EARTH. IT COMES FROM THE WEATHERING OF ROCKS AND DECOMPOSITION OF ORGANISMS. IT IS.
INVERTEBRATE SAMPLING METHODS INVERTEBRATE SAMPLING METHODS Therese A. Catanach Program in Ecology, Evolution, and Conservation 1816 South Oak Street,
Between-Bed pH pH is significantly higher in the two inner groups of beds relative to the outer two groups. Decomposition of the shredded leaves in the.
Ecoregions of Texas.
Influence of Chinese privet (Ligustrum sinense Lour.) on floodplain productivity and regeneration Eve Brantley, Jennifer Mitchell, and B. Graeme Lockaby.
Alfisols!!!!!!!!!!!!. Develop in semiarid to moist areas Primarily forested soils They have clay and nutrient rich sub-soils that hold and supply.
Thesis  Erin Harrington  Advisors  Bobbi Low  Phil Myers.
Vegetation Transects San Pedro Creek Study.
Fire Weather: Temperature & Moisture. Weather and the Earth’s Heat Balance Weather = motion in the atmosphere due to unequal heating Over time, the amount.
Dew Point and Relative Humidity
Black legged Ticks Lymes on the rise……….
Lyme on the rise The black legged tick
Rocks, Weathering, and Soil Information
Overview of Biomass Mapping The Woods Hole Research Center Alessandro Baccini, Wayne Walker and Ned Horning November 8 – 12, Samarinda, Indonesia.
CONSTRUCTING A FIVE CABIN LATRINE
Weather: The state of the atmosphere at a given time and place, with respect to variables such as temperature, moisture, wind velocity and direction,
Chapter Soil Chapter 12.4 Soil as a Resource
Welcome to Mr. Conroy’s Science Class co-made by Logan L., Vince D., Angela S., & Kayana C.
Section 3: Soil Preview Key Ideas Soil Soil Characteristics
Ecosystems A small – scale study of the school grounds.
ACTIVITY #1: Let’s Get the Ball Rolling!
Unit 2 Topic 2 soil. What is soil and why do we care about it?  complex mixture:  weathered mineral materials from rocks  partially decomposed organic.
Soils.
SOIL. What is soil? The loose covering of broken rock particles and decaying organic matter (humus) covering bedrock.
Chapter 12 Soil Resources.
Igneous Sedimentary Metamorphic Rock Very slowly weathered minerals (e.g., quartz, muscovite) Slowly weathered minerals (e.g., feldspars, biotite) Easily.
Topic 5 Part 1 soil.
PCB 3043L - General Ecology Data Analysis. OUTLINE Organizing an ecological study Basic sampling terminology Statistical analysis of data –Why use statistics?
The Tropical Rainforest IB SL. Location Introduction... They are the world's most productive ecosystems in terms of NPP and biomass. They are complex.
The effects of the 2002 Hayman Fire on the ponderosa pine/bunch grass ecosystem Nick Kelley Blake Schnebly
Five Ecoregions of Texas. What Is An Ecoregion?  Ecoregion – a major ecosystem with distinctive geography, characteristic plants and animals, ecosystems,
Nutrient cycles The nitrogen cycle Inputs of nutrients : 1.Precipitation & dry deposition 2.Weathering of bedrock 3.[Artificial supplements]
Weathering and Erosion
Weather Chapter 21 1.
Carbon and water cycling along the western Sierra gradient Anne Kelly SSCZO annual meeting August 21, 2012.
ELECTRICAL RESISTIVITY SOUNDING TO STUDY WATER CONTENT DISTRIBUTION IN HETEROGENEOUS SOILS 1 University of Maryland, College Park MD; 2 BA/ANRI/EMSL, USDA-ARS,
Temperate Deciduous Forest
PCB 3043L - General Ecology Data Analysis.
Ecoregions of Texas.
INTRODUCTION TO SOIL IAFNR Plant and Soil Sciences Module.
ROCK CYCLE. IGNEOUS ROCK Formed when –magma cools underground EX: granite –Or above ground EX: lava rock/pumice.
The Nature of soil. Dirt is what you find under your fingernails. Soil is what you find under your feet. Think of soil as a thin living skin that covers.
Soils.
Soil Taxonomy- Properties of Soil
 Natural Vegetation is plant life that hasn’t been planted or changed by humans, it has grown naturally or wildly as nature intended.  Humans however.
West Texas Mesonet – Texas Tech University TTU Wind Science & Engineering Atmospheric Science Group
© 2015 John Wiley & Sons, Inc. All rights reserved. BIO 112 June 22, 2015  The Soil System (part of ch. 14)  Soil Properties and Major Soil Types  California.
Origins- parent material; mixtures of eroded rock, mineral nutrients, decaying organic matter, and billons of living organisms (mostly decomposers)
SOIL: A RENEWABLE RESOURCE Soil is a slowly renewed resource that provides most of the nutrients needed for plant growth and also helps purify water. Soil.
Measuring Albedo. Type of surface cover Outgoing illuminance Incoming illuminance Albedo.
The Weather Station Model
Black Cohosh Presence and Abundance Relative to Environmental Gradients Nicole Hupp- Regis University, Denver, Colorado Dr. Luben Dimov- Alabama A & M.
Control Charts Definition:
Ex: Which vegetables grow better in my garden
The Nature of soil.
PCB 3043L - General Ecology Data Analysis.
Soil Formation Soil is an important natural resource
Rocks, Weathering, and Soil Information
Rocks, Weathering, and Soil Information
Unit 4 Weather about Doppler Radar.
Rocks, Weathering, and Soil Information
Rocks, Weathering, and Soil Information
4.1.2 Temporal variation in questing activity and survival
Chap 10, Sec 3 (From Bedrock to Soil)
Rocks, Weathering, and Soil Information
Rocks, Weathering, and Soil Information
Presentation transcript:

TICK COLLECTION CRITERIA Project title Michael Cherry| Dr. Ben Clarke| Bridges and Pathways Program 2010

TICK COLLECTION What criteria and procedures should be used when collecting ticks in the ‘wild’?

PROJECT OVERVIEW Where ticks are located Survey techniques should be consistent Use of standardized equipment Integrity of Data Collection Criteria and methods of recording

WHERE ARE TICKS LOCATED IN THE MIDWEST? Near or in deciduous forests Dry to mesic (moderate moisture) forests Alfisol-type soils of sandy or loam-sand textures overlying sedimentary rock Along ecotones (boundaries between varying ecosystems)

ALFISOL SOILS Alfisols are a soil order in USDA soil taxonomy. Alfisols form in semiarid to humid areas, typically under a hardwood forest cover. They have a clay-enriched subsoil and relatively high native fertility. "Alf" refers to Aluminium (Al) and Iron (Fe).USDA soil taxonomyhardwood Alfisol from East Tennessee.

WHERE ARE TICKS NOT LOCATED IN THE MIDWEST? Near coniferous forests Grasslands Wet and very damp forests Acidic soils of low fertility and a clay soil texture Precambrian bedrock

CONSTRUCTION OF DRAGGING EQUIPMENT – 70 x 90cm piece of light-colored corduroy – 1cm diameter wooden dowel along leading edge – Steel rod sewn into trailing edge for added weight – Rope or wood handle to allow front edge of ‘sheet’ to contact vegetation

COLLECTION TECHNIQUES FROM SCHULZE/JORDAN Same individual should perform the dragging for consistency – Speed, height Collected hourly from 0600 – 2100 hours 100m long transects, collect every 10m to prevent ticks from falling off Ramdomize dragging order, direction of travel, location within each transect (left, right, center) to minimize repeated dragging of same areas Minimize dew collection by drying on running pickup truck hood – To minimize effects of moisture on tick collection

STATISTICS For each sampling event (each hour) (use of Weather Station): – Ambient Temperature – Ambient Humidity – Place Weather Station in center of area, 1m above vegetation height – Litter temperature and humidity (digital thermometer) At least 2.5cm below leaf litter surface but not into the soil

STATISTICAL ANALYSIS Use of repeated measures of analysis of variance Use of multiple linear regression to examine relationships Use separate regressions for each species Tolerance value of 0.1 is acceptable Calculate temp gradient: subtract hourly litter temp from ambient Calculate humidity gradient: subtract litter H from ambient H Use Pearson correlation and linear regression to determine relationships between calculated gradients and numbers of questing ticks

CONCLUSION Consistency regarding the gathering of ticks and in measuring and recording statistics are critical to success

WORKS CITED Meteorologically Mediated Diurnal Questing of Ixodes Scapularis and Amblyomma Americanum Nymphs – Terry Schulze and Robert Jordan Journal of Medical Entomology (2003) Distribution of the Common Tick, Ixodes ricinus, in different vegetation types in Southern Sweden – Anders Lindstrom and Thomas Jaenson, Journal of Medical Entomology (2003)