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South American Lake Gradient Analysis pact of climate on shifts in stable sta in shallow lakes Sarian Kosten Wageningen University The Netherlands

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Page 1: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

South American Lake Gradient Analysis

Impact of climate on shifts in stable statesin shallow lakes

Sarian KostenWageningen University

The Netherlands

Page 2: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Project outline

Preliminary results

Research questions

Page 3: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Outline

Temperate shallow lakes tend to be in either of two alternative stable states.

Preliminary work suggests that shallow lakes may be very sensitive to climatic change.

Page 4: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands
Page 5: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Low nutrient High nutrient

Page 7: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

83 lakes

Latitude 5 – 55 degrees south

Page 8: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Sample sites

Page 9: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

83 lakes

November 2004 – March 2006

Mid-summer samples

Shallow lakes (average 1.8 m [4.5 – 0.5])

Latitude 5 – 55 south

Low altitude / coastal

Area between 9 and 250 ha.

All sampled by the same team

Page 10: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

How do algae react to higher temperatures?• N versus P-limitation?• reach higher concentrations?

How do macrophytes react to higher temperatures?• resist higher turbidities?• disappear at higher nutrient levels?

Does the interaction between algae and macrophytes change at higher temperatures?

Questions

Page 11: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands
Page 12: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands
Page 13: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

How do algae react to higher temperatures?• N versus P-limitation?• reach higher concentrations?

How do macrophytes react to higher temperatures?• resist higher turbidities?• disappear at higher nutrient levels?

Does the interaction between algae and macrophytes change at higher temperatures?

Questions

Page 14: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Gyllstrom et al., 2005

Page 15: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Huszar et al., 2006

Algae reach a higher biomass – at a given total-P concentration - in colder climates

192 (sub)tropical lakes(Huszar et al. 2006)

N. American & European lakes(Mazumder 1994)

Page 16: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

• Both production and respiration will increase but respiration increases relatively more than production

Why do algae reach lower concentrations at a certain nutrient leven when the temperature increases?

(Lopez-Urrutia et al., 2006)

Page 18: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Trophic state

Preliminary results from our study:

Page 19: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Tropicalwith distinct dry season

Tropical – Subtropicalwith and without dry season

Subtropical

Polartundra

Köppen Climate Classification

Page 20: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Total phosphorus (μg L-1)

All lakes Polar Subtropic Tropic

Log Chl-a Log Tot-P

R2

1.5 1.4 1.9 1.6

0.59 0.94 0.56 0.38

Page 21: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Nitrogen limited

Phosphorus limited

Limiting nutrient

Redfield ratioN:P = 16:1

Next 2 slides is I did not show because of lack of time, but isn’t it interesting to see that we have a dominance of N limitation along almost the entire gradient. It will be nice to compare that with other shallow lakes around the globe.

Page 22: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Log Chl-a Log Tot-N

R2

1.1 1.1 1.1 1.1

0.78 0.72 0.81 0.69

All lakes Polar Subtropics Tropics

Total nitrogen (μg/l)

Ch

l-a

(μg

/l)

SLOPE EXACTLY THE SAME FOR ALL REGIONS!!

Page 23: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Overall the algae seem to reach a slightly higher biomass at a given total-P level at higher temperatures

In a comparative study between temperate and artic lakes Flanagan et al. (2003) found higher biomasses at higher temperatures as well.

Page 24: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

•Low enzyme activity when cold (Markager et al. 1999)

•Presence of cyanobacteria

•Absence of large zooplankton

Why would warmer be better for algae?

Page 25: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands
Page 26: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

How do algae react to higher temperatures?• N versus P-limitation?• reach higher concentrations?

How do macrophytes react to higher temperatures?• resist higher turbidities?• disappear at higher nutrient levels?

Does the interaction between algae and macrophytes change at higher temperatures?

Questions

Page 27: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Coverage percentage of submerged plants

Page 28: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Average Kd in lakes with a small (<30%) and a large (>30%) coverage of submerged plants

0

2

4

6

8

RN <30 RN >70 RJ <30 RJ >70 UY<30 UY >70 TF<30 TF>70

climate zone

Kd

[m

-1]

Tropical (Sub)tropical Subtropical Polar

Lakes with a coverage percentage of submerged plants <30%

Lakes with a coverage percentage of submerged plants >30%

Page 29: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

light intensity (average) at plant canopy

0

50

100

150

200

RN RJ UY TF

climate zone

lig

ht

inte

nsit

y

[E m

-2 m

in-1

]

Tropical (Sub)tropical Subtropical Polar

Page 30: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Maximum nutrient concentration at which submerged macrophytes occur

0

2

4

6

RN RJ UY TF

climate zone

tot

N o

r P

(m

g/l) max tot-P

max tot-N

Page 31: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

How do macrophytes react to higher temperatures?

Do they occur at higher turbidities?

Do they occur at higher nutrient levels?

>>> NO

>>> NO

Page 32: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Why?Not only temperature changes but total daily irradiance as well.

Unbalance of data set

Page 33: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

How do algae react to higher temperatures?• N versus P-limitation?• reach higher concentrations?

How do macrophytes react to higher temperatures?• resist higher turbidities?• disappear at higher nutrient levels?

Does the interaction between algae and macrophytes change at higher temperatures?

Questions

Page 34: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Polar climate

-100

-50

0

50

100

0.1 0.1 0.4 0.4 0.9 1.0 1.4 5.3

Total-N (mgN/l)

"wa

ter-

cle

ari

ng

-eff

ec

t" o

f s

ub

me

rge

d p

lan

ts (

%)

chl-a

turbidity

Tropical - Subtropical climate

-100

-50

0

50

100

0.2 0.2 0.2 0.3 0.3 0.8 0.9 0.9

Total-N (mgN/l)

"wa

ter-

cle

ari

ng

-eff

ec

t" o

f s

ub

me

rge

d p

lan

ts (

%)

chl-a

turbidity

Subtropical climate

-100

-50

0

50

100

0.0 0.1 0.2 0.2 0.3 0.4 1.0 1.1 1.3 2.4

Total-N (mgN/l)

"wat

er-c

lear

ing

-eff

ect"

of

sub

mer

ged

pla

nts

(%

)

chl-a

turbidity

Tropical climate

-100

-50

0

50

100

0.0 0.1 0.6

Total-N (mgN/l)

"wat

er-c

lear

ing

-eff

ect"

of

sub

mer

ged

pla

nts

(%

)

chl-a

turbidityWater clearing effect of submerged macropytesTropical climate

-100

-50

0

50

100

0.0 0.1 0.6

Total-N (mgN/l)

"wa

ter-

cle

ari

ng

-eff

ec

t" o

f s

ub

me

rge

d p

lan

ts (

%)

chl-a

turbidity

Page 35: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

We found a water clearing effect of submerged macropytes along the whole climate gradient

We found a small effect on the TP chl-a relationship

Preliminary results

We did not find submerged macrophytes in more turbid conditions in warmer climates

Page 36: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

NWO/WOTRO

The National Geographic Society

The Schure-Beijerinck-Popping fund

Kosten Watersport bv.

Page 37: South American Lake Gradient Analysis Impact of climate on shifts in stable states in shallow lakes Sarian Kosten Wageningen University The Netherlands

Gissell Lacerot

Andy LotterBart KoelmansCarla KrukChristina Branco David da Motta MarquesErik JeppesenEgbert van NesFabio Roland Jeroen de Klein John BeijerJose Luiz AttaydeJose PaggiKatleen van der GuchtLuc de MeesterMarten Scheffer Miquel LurlingNestor MazzeoSusana de PaggiVera Huszar

www.salga.wur.nl