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Bess Ward Department of Geosciences Princeton University
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Weddell Sea Ross Sea Palmer Peninsula
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Pine Island Glacier breaks away from the Palmer Peninsula -- global warming at work?
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Cooling Trend in Antarctica -- warmer in polar seas Doran et al., 2002
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Weddell Sea Ross Sea Palmer Peninsula
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Doran et al., 2002
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Antarctic Continental Cooling u Climate indicators u Reduced T, decreased wind, increased sunshine u Reduced river flow, thicker ice u Ecosystem effects u Less primary production u Fewer nematodes
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Conflicting Signals of Climate Change in Antarctica u Indications of global scale change? u Feedback effects of global climate? u Ecological consequences?
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The Mystery of the Dysfunctional Nitrogen Cycle Taylor Glacier South Pole West LB East Lake Bonney
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West LB East Lake Bonney STRANGE… N cycle non functional: Way too much nitrous oxide (N 2 O) and nitrate (NO 3 ) West Lake Bonney NORMAL N cycle functional: Very little nitrous oxide (N 2 O) and nitrate (NO 3 ) One lake, two lobes connected at the surface WHY????
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N 2 O = Greenhouse gas UV radiation Ozone layer N 2 O involved in Catalytic ozone destruction NO 3 bacteria Nitrous oxide (N 2 O): intermediate in denitrification N2N2
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Nitrogen Concentrations (µM) NORMAL Depth (m) West Lobe ammonium nitrate East Lobe STRANGE ammonium nitrate
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Nitrogen Concentrations (µM) East Lobe STRANGE ammonium nitrate
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Nitrogen Concentrations (µM) East Lobe STRANGE ammonium nitrate (Priscu et al., 1996; LTER) nitrous oxide Depth (m) East Lobe REALLY STRANGE
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First, drill a hole….
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Weather port, West Lobe Lake Bonney
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Sampling Hole through the Ice Cover
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“Lab” inside the weather port
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Isolate denitrifying bacteria and detect them in the lake Species- specific immunofluorescence
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Distribution of strain ELB17 (Marinobacter) in Lake Bonney (counted by immunofluorescence) East Lobe
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Optimal growth conditions for strain ELB17
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Nitrite reductase (nirS) genes in Lake Bonney u Central enzyme in denitrificaiton encoded by nirS u nirS genes found in both lobes Chris Francis
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Sharon Harris: Teacher Experiencing Antarctica Measuring denitrification rates based on N 2 O production
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Depth (m) West Lobe Denitrification rate
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Depth (m) East Lobe Denitrification rate
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Denitrification does not occur in the East Lobe… but all the ingredients are present u Denitrifiers can be isolated from the lake u The strains survive under in situ conditions u Denitrifying cells are detected in the lake u Denitrifying genes are detected in the lake u Denitrification happens in the bags, not in the lake u So what is the #?@@*#&^&*$ problem??
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Nitrogen Concentrations (µM) East Lobe STRANGE ammonium nitrate (Priscu et al., 1996; LTER) nitrous oxide Depth (m) East Lobe REALLY STRANGE
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EastWest Copperlowhi Silver low Mark Wells
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Nitrite Reductase, Nitrous Oxide Reductase NO 3 NO 2 NON2ON2O N 2 Inducible, conserved, gas metabolism (Cu, heme) (Cu)
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The Copper Hypothesis u Cu u Cu is required for denitrification u AgCu u Ag substitutes for Cu in denitrification enzymes, and makes them nonfunctional u AgCu u Ag toxicity or competition with Cu inhibits denitrification in the East AgCu u But how did the two lobes end up with such different Ag / Cu ratios?
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LTER East Lobe West Lobe Taylor Glacier
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Blood Falls, West Lake Bonney
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Cross section of Lake Bonney today W E Taylor Glacier
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Lake Bonney 3000 years ago “cold-dry” period W E Taylor Glacier
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W E
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W E
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W E
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W E
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Lake Bonney 1200 years ago Hypersaline pool in the East Lobe W E Taylor Glacier
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W E
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W E
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Cross section of Lake Bonney today W E Taylor Glacier
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Geochemical Evidence u West and East Lobes have different histories u History reflected in chemical composition of the water u Modern biogeochemistry depends on past climate change u Future climate change depends on current biogeochemistry
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Bonney Hoppers
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Sunrise at McMurdo, 11 July 2001
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