LAKES IN DRYLANDS: VARIATION IN CHIRONOMID COMMUNITIES IN WESTERN MONGOLIA LAKES R. William Bouchard Jr. Barbara L. Hayford Leonard C. Ferrington, Jr.

Slides:



Advertisements
Similar presentations
Turtle Lake Water Quality Index
Advertisements

The Chemical Water Quality of Lake Nipissing Andrew Paterson Dorset Environmental Science Centre Environmental Monitoring and Reporting Branch.
Salinity of Lakes, Rivers, and Reservoirs
Koktuli River Instream Flow Reservation Cathy Flanagan Bristol Bay Native Association.
Genetic Diversity of Stream Fish Populations in the Mid-Atlantic Region Suzanne Christ, Mark Bagley, Frank McCormick US Environmental Protection Agency,
Biogeochemical Cycles. Biogeochemical: Chemical elements and molecules that cycle through the Earth’s systems and provide the building blocks for life.
THE FOSSIL RECORD Ecology and Paleoecology Fundamental Concepts of Ecology and Paleoecology Paleoecologists are particularly interested in the marine (ocean)
Diatoms as Bioindicators of Water Quality Cassandra Messina April 19, 2005 ECOL 475.
Water Quality Analysis Methods and Applications. Water Quality Analysis Physical Factors including suspended materials (called suspended solids) and dissolved.
Community Ordination and Gamma Diversity Techniques James A. Danoff-Burg Dept. Ecol., Evol., & Envir. Biol. Columbia University.
Marine Water. n Marine waters may be fully saline, brackish or almost fresh. Marine habitats include those below spring high tide limit (or below mean.
Measuring abiotic components  Objectives  To make an exhaustive list of abiotic factors  To discuss the ways they are measured  To critically appraise.
Soil Testing and Analysis Nutrient Management Basics
Lesson 6: Ocean Layers I Chemical Oceanography. We have been learning about ocean chemistry What are two important cycling nutrients we have learned about?
SEAWATER and the properties of the water molecule.
Chapter : Seawater Fig Density of seawater to g/cm 3 Ocean layered according to density Density of seawater controlled by temperature,
Properties of Ocean Water. Chemical Properties of Ocean Water Determines composition Determines composition Enables it to dissolve other substances Enables.
Earth Science 2.2 Minerals.
Physical and Chemical Oceanography
Kiersten Honig. Lynnhaven River Watershed Comprises approximately 64 square miles of land and water, with nearly 150 miles of shoreline Used to be a prime.
Vulnerability of freshwater fish communities to human mediated impacts Jenni McDermid 1 and David Browne 1,2 1 Wildlife Conservation Society Canada, Peterborough,
BIOENGINEER ANALYSIS WATER. GOALS Students learn how to collect water samples. Then, they will aseptically collect a water sample and use a microscope.
2 The Oceanic Environment Notes for Marine Biology: Function, Biodiversity, Ecology By Jeffrey S. Levinton.
U.S. Department of the Interior U.S. Geological Survey Quantifying tolerance indicator values for common stream fish species of the United States Michael.
Physical Oceanography Section 2: Seawater
PROPERTIES OF SEAWATER
Temperature Measured with a thermometer Units are ◦C
A Comparative Stream Study of Two First Order Streams in Nixon Park, York PA Susan Price Department of Biological Sciences, York College Introduction Macroinvertebrates.
Ocean Water (63) Oceans are important sources of food, energy, and minerals. Energy sources such as oil and natural gas are found beneath the ocean floor.
Empirical determination of N critical loads for alpine vegetation William D. Bowman, Julia L. Gartner, Keri Holland, and Magdalena Wiedermann Department.
Welcome Grant from National Science Foundation: Fire, Atmospheric pCO 2, and Climate as Alternative Primary Controls of C 4 -Grass Abundance: The Late-Quaternary.
Unit 2: Surface Processes and the Hydrosphere Lesson 7: Physical Oceanography Pt. 2 ( Heath Earth Science – Pg )
Copyright © 2011 InteractiveScienceLessons.com Composition of Ocean Water Name Water96.5% 40 Wide 25 High 40 x 25 =1000 squares
© 2011 Pearson Education, Inc. CHAPTER 5 Water and Seawater.
Properties of seawater. Properties of water 1.Polarity and hydrogen bonding cohesion good solvent many molecules dissolve in H 2 O 2.lower density as.
NWQMC San Jose, CA May 8, 2006 Combining Dynamic Assessment with Traditional Monitoring Approaches to Improve Understanding of NPS Pollution Impacts William.
Fig. 7-CO, p Fig. 7-1, p. 186 Condensation Precipitation 111,000 Precipitation 385,000 Transpiration and Glaciers Evaporation 425,000 Groundwater.
A Multi-proxy Paleolimnological Reconstruction of Holocene Climate Conditions in the Great Basin, United States 1 Department of Geography, The Ohio State.
Oceans. Ocean-Atmosphere Links Exchange of water, carbon dioxide and heat. Surface ocean currents are driven by atmospheric circulation. Oceans and atmosphere.
Using Data to Explore Ocean Processes Koshland Science Museum of the National Academy of Sciences.
The Impact of pH on pCO 2 Levels in Florida Lakes Jenney L. Kellogg Florida LAKEWATCH Florida LAKEWATCH Dept. of Fisheries and Aquatic Sciences University.
Arsenic in Iowa’s Groundwater – The Unknown Threat: A Pilot Study in Cerro Gordo County Arsenic Conference November 9, 2011.
Chapter 22 – The Water Planet
Water Quality Testing.
OBJECTIVES a. To evaluate the impact of continuing schemes
Aquatic, Watershed, and Earth Resources
Caddo Lake Nutrient Study Roy Darville - Caddo Lake Institute
Scott W. Starratt US Geological Survey
Nichole Holdbak November 2009
Chemical Oceanography
Lesson 6: Ocean Layers I Chemical Oceanography
Figure 1. The relationships of bacterial operational taxonomic unit richness (A) and phylogenetic diversity (B) with aridity index based on 97% sequence.
Ocean Water California Standards: 5d, 7b
Lesson 6: Ocean Layers I Chemical Oceanography
Earth’s Oceans.
MOUNTAINS AT RISK.
Physical and Chemical Oceanography
Section 2: Seawater Oceans have distinct layers of water masses that are characterized by temperature and salinity. K What I Know W What I Want to Find.
Salinity of the Ocean Notes
Environmental Systems
We have been learning about upwelling and nutrients
Monday’s graph.
Combinations (= multimetrics)
Physical and Chemical Oceanography
Properties of Ocean Water
Lesson 6: Ocean Layers I Chemical Oceanography
Non-marine biological evidence
Seawater 15.2.
Properties of Ocean Water
The Common Elements Notebook Page 27:
Presentation transcript:

LAKES IN DRYLANDS: VARIATION IN CHIRONOMID COMMUNITIES IN WESTERN MONGOLIA LAKES R. William Bouchard Jr. Barbara L. Hayford Leonard C. Ferrington, Jr.

Western Mongolia Western Mongolia is a semi-arid to arid – Desert steppe, typical steppe, mountain steppe, alpine forests, meadows, and glaciers Eleven Mongolian Special Protected Areas and a UNESCO world heritage site

Western Mongolia Numerous lakes that range from alpine to lowland evaporative basin lakes Lakes exhibit strong, natural environmental gradients (e.g., salinity, nutrients) High elevation, freshwater Low elevation, saline (Uvs Nuur, UNESCO World Heritage Site) Low elevation, freshwater

Threats Climate change can impact: salinity, timing of salinity, hydrograph, temperature and thermal stratification Over grazing and high density of domesticated grazers western Mongolia Desertification caused by climate change and intensive land use in arid and semi-arid lands

OBJECTIVE Climate change, over grazing and collectively desertification threaten diversity thus our objectives are: 1.To document diversity of a common lake invertebrate, the non-biting midge (Diptera: Chironomidae) 2.To relate environmental conditions to diversity, unique communities, and individual taxa in lakes of Western Mongolia

Background Diatom communities influenced largely by salinity and nutrient gradients

Methods 54 lakes Strong environmental gradients (elevation, size, depth, nutrients, salinity) Shinneman et al. (2009) Diatoms communities influenced by salinity and nutrient gradients

From Shinnerman et al. (2009)

Kranzfelder et al. (2015) Journal of Visualized Experiments 101, e Single pupal exuviae sample from each lake 500 count subsamples slide mounted Identification to species/morphospecies

Chironomid Diversity 117 species collected 54 taxa after removing rare taxa (taxa present in ≥5% of sites)

Environmental Variables Latitude, Longitude, Elevation, Water Temperature, Specific Conductance, pH, Dissolved Oxygen, Secchi Depth, Chlorophyll-a, Total Phosphorus, Total Nitrogen, Nitrate, Organic Nitrogen, Kjeldahl Nitrogen, Ammonia, Chloride, Sulfate, Sodium, Magnesium, Aluminum, Silicon, Potassium, Calcium, Iron, Manganese, Dissolved Organic Carbon, Dissolved Inorganic Carbon, Carbonic Acid, Bicarbonate, Carbonate, Lake Type

Midges and Lake Attributes Partial constrained correspondence analysis (cca; R 3.2.2, “vegan” package) performed individually on all physical and chemical variables to identify those which were significantly (P ≤ 0.01) related to chironomid community composition Total Nitrogen Kjeldahl Nitrogen Specific Conductance Chloride Sulfate Sodium Magnesium Silicon Potassium Dissolved Organic Carbon Bicarbonate Carbonate

Redundant Measures SalinityNitrogenInorganic CarbonIndependent Specific ConductanceTotal NitrogenDissolved Organic CarbonSilicon ChlorideKjeldahl nitrogenBicarbonate SulfateCarbonate Sodium Magnesium Potassium

CCA cca; R 3.2.2, “vegan” package

Salinity GrpClassification Salinity (ppt) FFreshwater<0.5 OOligohaline0.5-5 MMesohaline5-18 PPolyhaline +>18 metaMDS; R 3.2.2, “vegan” package

Taxa Richness metaMDS, ordisurf; R 3.2.2, “vegan” package

A Lake Typology Categorized lakes based on size, depth and salinity Classification Shallow Freshwater Deep Freshwater Small Shallow Saline Small Deep Saline Large Saline Terminally Valley Saline Hypersaline

Lake type comparisonTp Large SalineShallow Freshwater Large SalineDeep Freshwater Large SalineHypersaline Large SalineTerminal Valley Saline Large SalineSmall Shallow Saline Large SalineSmall Deep Saline Shallow FreshwaterDeep Freshwater Shallow FreshwaterHypersaline Shallow FreshwaterTerminal Valley Saline Shallow FreshwaterSmall Shallow Saline Shallow FreshwaterSmall Deep Saline Deep FreshwaterHypersaline Deep FreshwaterTerminal Valley Saline Deep FreshwaterSmall Shallow Saline Deep FreshwaterSmall Deep Saline HypersalineTerminal Valley Saline HypersalineSmall Shallow Saline HypersalineSmall Deep Saline Terminal Valley SalineSmall Shallow Saline Terminal Valley SalineSmall Deep Saline Small Shallow SalineSmall Deep Saline MRPP Multi Response Permutation Procedure (MRPP) tests whether communities are distinct from one another Multi-Response Permutation Procedure (MRPP; PC-ORD 6)

Taxon CodeTaxonGroup CRPTRWB1Cryptotendipes RWB pe1Large Saline CRYPSUPCryptochironomus supplicansLarge Saline CLDORWB1Cladotanytarsus RWB pe1Large Saline CLAD0VIRCladopelma viridulumShallow Freshwater CRICRWB3Cricotopus (Cricotopus) RWB pe3Shallow Freshwater PTNYDIMParatanytarsus cf. dimorphisShallow Freshwater PROHRWB1Procladius (Holotanypus) RWB pe1Shallow Freshwater CRISRWB4Cricotopus (Isocladius) RWB pe4Shallow Freshwater ORTHPOGOrthocladius (Pogonocladius) consobrinusDeep Freshwater ABLMONAblabesmyia monilisDeep Freshwater TANYTPUNTanypus punctipennisDeep Freshwater DICRLOBDicrotendipes lobigerDeep Freshwater CRICRWB2Cricotopus (Cricotopus) RWB pe2Deep Freshwater CRIISSYLCricotopus (Isocladius) sylvestrisDeep Freshwater PSECPBREPsectrocladius (Psectrocladius) brehmiDeep Freshwater CRICRWB9Cricotopus (Cricotopus) RWB pe9Hypersaline CHIRRWB2Chironomus RWB pe2Terminal Valley Saline CLDORWB2Cladotanytarsus RWB pe2Terminal Valley Saline CRIISLAECricotopus (Isocladius) laetusTerminal Valley Saline PROHRWB4Procladius (Holotanypus) RWB pe4Small Shallow Saline GLYPBARGlyptotendipes barbipesSmall Shallow Saline CGNARWB1Chironomini Genus A RWB pe1Small Deep Saline CLDORWB4Cladotanytarsus RWB pe4Small Deep Saline CRIISORNCricotopus (Isocladius) ornatusSmall Deep Saline PSECPRWB1Psectrocladius (Psectrocladius) RWB pe1Small Deep Saline Indicator Species Calculated indicator species to see which taxa best defined these communities

Indicator Species Psectrocladius (Psectrocladius) brehmi glm; R Cricotopus (Isocladius) laetus

Summary Taxa rich fauna (>100 species) Distinct communities that largely follow a salinity gradient (although nutrients are probably also important) Unique habitats face threats from climate change and changing land use

Thanks National Science Foundation (NSF) grant DEB National Science Foundation (NSF) grant DEB Jim Almendinger – Science Museum of Minnesota Jim Almendinger – Science Museum of Minnesota Mark Edlund – Science Museum of Minnesota Mark Edlund – Science Museum of Minnesota