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How will climate change affect pasture plant species and their reserves?
Jean-François Soussana, Florence Volaire, Frédérik Le Dily
To cite this version:
Jean-François Soussana, Florence Volaire, Frédérik Le Dily. How will climate change affect pasture plant species and their reserves?. ”Les réserves végétales et leur importance agronomique et sylvicole”, Institut National de Recherche Agronomique (INRA). UMR UMR INRA / Univ. Caen : Laboratoire de physiologie et biochimie végétales (0950)., Jun 2009, Caen, France. 66 p. �hal-02819471�
How will climate change affect
pasture plant species
and their reserves?
Jean-François Soussana
1, Florence Volaire
2and Frédérik Le Dily
31 : UR874 Grassland Ecosystem Research, INRA, Clermont, France 2 : UMR SYSTEM, INRA, Montpellier, France
Outlook
• Introduction: climate change
• 1° Plant types, reserves and climate
• 2° Elevated CO
2
and incremental warming
effects on reserves
• 3° Drought and survival: the role of
reserves
What is climate change?
Increase in the main greenhouse gases
Carbon dioxide (CO
2)
Methane (CH
4)
Nitrous oxide (N
2O)
Changes in climate
Temperature
Precipitation
Extreme events
Global increase in anthropic greenhouse gas emissions
Global greenhouse gas emissions covered by the Kyoto protocol have increased by 70 % from 1970 to 2004
years BP ('000) 0 50 100 150 200 250 300 350 400 450 CO 2 160 180 200 220 240 260 280 300 320 340 360 380
Atmospheric CO
2
in the past
The last 400‘000 years
today
Global warming since 1880
7
Projected droughting
of South Europe
Climate changes
(IPPC, 2007)Predictions for Southern Europe
Increased frequency of severe droughts
Reduction of water availabilityClimate models converge for
changes in rainfall in Europe
-Likely progression northwards of Mediterranean influence
- Frequency of severe summer droughts is likely to double
Impacts of climate variability and
extremes on grasslands
Interannual variability
Agricultural
Climate change: incremental warming
and increased variability
Years Climate variable
Variability
Incrementa l change
Growth
Reserves cycle
A synchronism exists between growth & dynamic
of reserves
Perennial Yr n-1 Yr n Yr n+1 … Storage : Fall - winter Mobilisation : Winter - spring Mi n i a ir tem p . N reserves Goulas et al. 2001 e.g. cloverGrowth
Reserves cycle
A synchronism exists between growth & dynamic
of reserves
Sucro se in t ap roo tDays after sowing
Le Dily et al. 1992 e.g. carota Bisannual Yr 1 Yr 2 Storage : Early fall Mobilisation : Winter - spring Yr 1 Yr 2 G R cycle
N per
plan
te
Annual
Storage :
Spring (leaf growth)
Mobilisation : Mid-spring (flowering)
e.g. oilseed rape
The synchronism between growth & dynamic of
reserves vary with phenology
Malagoli et al. 2005
Leaf development
G
Space for time analogy
• Which are the dominant pasture lifeforms in warmer/drier
climates?
– Perennials are dominant in temperate grasslands. However, earlier
flowering is documented at warmer/drier sites (e.g. Dactylis
glomerata, Volaire, 2001; Lolium perenne F. Balfourier,)
– Annuals become dominant in arid climates (below 300 mm)
– Geophytes (e.g. Poa bulbosa, Hordeum bulbosum; Dactylis ssp.
Hispanica cv. Kasbah) are located in semi-arid areas and are
summer dormant
• Can we keep perennials under climate change?
• Should we learn how to manage their C/N reserves?
• Would geophytes and annuals become useful?
• 2° Elevated CO
2
and incremental warming
effects on reserves
Years Climate variableVariability
Incrementa l changeElevated CO
2
and incremental
warming effects on reserves
Leaf proteins
Shoot structure
Roots
N reserve
C reserve
C subs
tra
te
N su
bs
tra
te
Respiration Photosynthesis NO 3 - uptake Root length Uptake capacity Leaf area &vertical distribution Leaf N Structural mass Relative growth rate Daily radiative partitioning
Leaf proteins
Shoot structure
Roots
N reserve
C reserve
C subs
tra
te
N su
bs
tra
te
Respiration Photosynthesis NO 3 - uptake Root length Uptake capacity Leaf area &vertical distribution Leaf N Structural mass Relative growth rate Daily radiative partitioning
+
+
+
Temperature
+
?
Elevated CO
2
and incremental
Elevated CO
2effects
(Free Air Carbon dioxide Enrichment)
CO2 released into the
ambient airstream Wind
Consistent increase in leaf photosynthesis
All studies: +58% (Drake et al., 1997)
FACE studies: +35 % (Ainsworth and Long, 2005)
Response to elevated CO
2
of maximal
carboxylation capacity
Nitrogen, leaf area and biomass allometry
in
Lolium perenne
(Soussana et al., 1996; Casella & Soussana, 1997; Calvet & Soussana, 2001)
Leaf area per unit root+shoot mass declines under elevated CO
2.This decline correlates with that in shoot N content
Ambient CO2
C-N fluxes in elevated CO
2with
L. perenne
N Min Water soluble carbohydrates +Photosynthesis
Rhizo-deposition
C:N
Respiration
SOILN immobilisation
N uptake
C yield
+
+
+
Organic C +
+
-
-
+
-
-
+
Negative feedback on yield, because of an increased soil N immobilization and increased allocation of C below-groundNegative
feedback
(Soussana et al., 1996; Loiseau & Soussana, 2000)WSC pools in laminae and sheath of perennial
ryegrass monocultures (mean of two N supplies)
(Casella and Soussana, 1997, J. Exp. Bot.)
Ambient Elevated CO2 +3°C Elevated CO2 350 700 700+ m g g -1 DM 0 50 100 150 200 250
Lamina (Hex. Sucr) Lamina (Fructans) Sheath (Hex. Sucr.) Sheath (Fructans) a A B B b b
Transplant experiment with a semi-natural grassland
(mini-FACE system, INRA Clermont)
Water soluble carbohydrate contents of
laminae (L) and stems (S) of plant community
at two cutting frequencies (C-, C+)
(Picon-Cochard et al., 2004, EJA)
Ambient Elevated CO2 2D Graph 8 '350 '600 m g g -1 DM 0 20 40 60 80 100 120 140 160 Laminae Cut- Laminae Cut+ Stems Cut- Stems Cut+ a a A A b b A A
'350 '600 mg g -1 D M 0 20 40 60 80 100 120 140 Grasses Cut- Grasses Cut+ Forbes Cut- Forbes Cut+
Water soluble carbohydrate contents of
grasses and forbes at two cutting frequencies
(Teyssonneyre et al., 2002 GCB; Picon-Cochard et al., 2004, EJA)
Ambient Elevated CO2
a a
A A
b b
A A
At leaf level
Farquhar’s photosynthetic model Stomatal regulation
Coordination of leaf N content Leaf N distribution vs. light Acclimation to temperature, CO2
Morphogenesis Architecture
Plasticity for some traits …
At root level NO3-, NH4+ uptake vs.
acquisition in function
of N in plant/ soil concentration Morphogenesis Architecture Acclimatation to Temperature … At soil level Inorganic N balance
SOM dynamics (four SOM pools)
Microbial turnover (two decomposer types)
At plant axis level
Assimilate partitioning
Functional balance between roots & shoots Reserve dynamics
Substrate dynamics
Root, shoot structure & shoot proteins dynamics …
At population level
Self thining
Axis density dynamics
Density dependent recruitment Mortality
…
At community level
Radiative balance (Kubelka-Munk equations) Inorganic N balance (diffusion driven competition) Community dynamics
At ecosystem level
Primary productivity C and N cycles
Grassland Ecosystem Model with Individual
centred Interactions (GEMINI)
Modelling reserve and substrate dynamics
Same dynamics for N substrate and reserve
(Soussana et al., 2000, Soussana & Oliveira Machado, 2001)
Simulated CO
2response ratio of substrate
and reserve dynamics
(Festuca arundinacea, cut-, N+, 10 yrs simulation)
Days since start of simulation
0 1000 2000 3000 4000 CO 2 r esponse rat io 700 /350 0 1 2 3 4 Substrate C Labile reserve C Slow reserve C
Days since start of simulation
0 1000 2000 3000 4000 CO 2 r esponse rat io 700 /350 0.6 0.8 1.0 1.2 1.4 1.6 1.8 2.0 Substrate N Labile reserve N Slow reserve N Carbon Nitrogen
Gradual saturation in C reserves Initial decline in N reserves,
Simulated CO
2response ratio of leaf
proteins, shoot structures and roots
(Festuca arundinacea, cut-, N+)
Days since start of simulation
0 1000 2000 3000 4000 CO 2 r esponse rat io (700 /350 ) 0 1 2 3 4 5 6 Leaf proteins Shoot structures Roots
Role of reserves under incremental
warming and elevated CO
2
Increasing demands on the buffering capacity in plants:
Between increased supply (CO
2) and increased demand (warming) of
carbohydrates,
Between increased C assimilation and reduced soil N supply,
Which strategies for managing carbohydrate (and
storage proteins) under climate change?
Increased buffering capacity to avoid down-regulation of leaf photosynthesis under elevated CO2 ?
Which plant parts for storage? e.g. breeding for tap roots, rhizomes, stolons.. Which forms of storage? Fructans, VSP, starch...
• 3° Drought and survival: the role of
reserves
YearsVariability
& extremes
Incrementa l change34
Increased importance of drought resistance
in forage grasses
Drought survival
Autumn recovery
Perenniality
Sustainability of agro-ecological functions
Stability production
Autumn/winter/spring
Stability soil cover
35
Stages of plant responses
of perennial grasses under a standard climatic scenario
June July August September Increasing water deficit
Green Progressive senescence Total senescence
STAGE1 STAGE 2 STAGE 3
---SURVIVAL PERIOD ---Rehydration Survival/Mortaliy Recovery Leaf Development & growth Root growth Mature lamina
STAGE 1: Transpiration & assimilation unaffected – Growth modulation STAGE 2: Transpiration & assimilation reduced – Growth reduced & stopped
STAGE 3: Transpiration (cuticular) – progressive senescence progressive (Blum, 1989)
Surviving organs Meristems
? ?
Main research areas (litterature) Research questions36
Drought survival
of aerial meristems - surviving organs
=
combination of adaptations 3 strategies
Dehydration delay
Increase of water uptake
(root system)
Reduction of water loss
(lamina senescence)
Dehydration tolerance
Sugars: fructans + Proteins: dehydrins
cell membrane stability
37
Dehydration tolerance
No discriminating differences
in
le
thal hydration of
meristematic tissues
Lethal hydration of meristems in dactylis = 35 % to 45%
much lower than lethal hydration of lamina
BUT
Discriminating differences
in
duration of survival at low
hydration
38
Accumulation of
water soluble
carbohydrates
(Julander, 1945; Suzuki & Nass, 1988…)
Accumulation of
dehydrins -
LEA
Proteins associated with desiccation & osmotic stress Abundant in dormant embryos and resurrection plants (Bartels et al., 1996; Close, 1996, 1997)
Factors
contributing
to dehydration
tolerance of
meristems ?
Dehydration tolerance
39
Water soluble carbohydrates
Dehydration tolerance
Total WSC High-DP fructans Low-DP fructans Sucrose Osmotic adjustment (-4 to –7 MPa) Monosaccharides 80 days 8 days Drought recovery Rehydration40
Accumulation of highly polymerised fructans
Sensitive populations Resistant populations
Water soluble carbohydrates:
Discriminating adaptationDehydration tolerance
Volaire & Gandoin (1996) Volaire & Lelièvre (1997) Volaire et al. (1998b)
41
Accumulation of highly polymerised fructans
Sensitive populations Resistant populations
Water soluble carbohydrates:
Discriminating adaptationDehydration tolerance
Volaire & Gandoin (1996) Volaire & Lelièvre (1997) Volaire et al. (1998b)
Fructans DP >3
Carbon reserves (regrowth after rehydration)Stabilisation lipidic layers of cell walls
Crowe et al. (1987); Demel et al. (1998); Hincha et al. (2002, 2007); Vereyken et al. (2003)
42
Dehydration tolerance
Water soluble carbohydrates:
Interaction withmanagement
Severe defoliation in Spring Depletion of Carbon reserves
Low summer survival + Low autumn recovery
Volaire (1994)
Spring intensity of defoliation affects autumn recovery after drought through fructan accumulation in meristems in Summer
Fructan concentration in meristems in July -drought (mg / g DM)
0 100 200 300 400 Recov ery A ut um n biom ass (g/ m²) 0 50 100 150 200 250 Resistant Dactylis Sensitive Dactylis LOW LOW MEDIUM MEDIUM HIGH HIGH
43
Dehydration tolerance
Dehydrins :
Non discriminating differences– Dactylis - resistant ++ Dactylis - sensitive + Volaire et al. (2001), Volaire (2002) – Barley - resistant +++ Barley - sensitive +++ Volaire (2003)
– Fescue - resistant ++ Fescue - sensitive +++ Norton et al. (2006)
Correlated with water content of tissues
(maximum when WC < 50 %)
Not correlated with levels of dehydration tolerance
Dehydrins : Hydrophilic proteins stabilisation of cell walls
Hoekstra et al. (2001); Goyal et al. (2005); Tompa et al. (2006)
Interaction with fructans
44
Conclusion - Strategies of perennial grasses under drought
Leaf growth Leaf senescence Photosynthesis Carbon Reserves Lamina turgescence Root growth WHOLE PLANT MERISTEMS
none low moderate high severe INCREASING DROUGHT
STRATEGIES 100 0 Growth maintainance Dehydration delay Dehydration tolerance Desiccation tolerance 0 0 0 Lamina mortality Tissue hydration Carbon reserves Dehydrins Membrane stability Tiller mortality 0 0 0 0
Conclusions (1/3)
• Basic knowledge of reserve dynamics in plants
needs to be extended and applied to climate
change adaptation.
• Which ideotypes for optimal C-N reserve
dynamics in a future climate?
– Increased reserve levels (insurance hypothesis)?
– Increased share of specialized organs (e.g. rhizomes,
bulbs, stolons, tap roots)?
– Are fructans and VSP preferable to other reserve types
(water stress tolerance)?
Conclusions (2/3)
• Adapting plant material
– Take advantage and increase Genetic variability ;
Genotype x Environment interactions;
– Breed genotypes with high plasticity; use populations?
– Use mixtures rather than monocultures?
– Breed for adapted plant reserve dynamics
• Adapting pasture management
– Avoid excess reserve depletion (e.g. frequent cutting,
severe grazing)
Conclusions : research needs
• Modelling
• Improve formalisms for: mortality, high temperatures etc..
• Observations
• Climatic gradient (e.g. Morocco—South of France)
• Experiments
• Impacts of extreme climatic events
• Biotic interactions
• Competition (weeds)
• Pests and pathogens
VALIDATE : expérience
avec extrêmes
Expérience in-situ à l’air libre combinant
sécheresse et
réchauffement de 3°C (scénario 2050)
avec ou sans extrêmes Un événement extrême appliqué en été 2009
de magnitude égale à celle de 2003 ou à celle projetée en 2050
Exclusion de pluie : rideaux automatisés Réchauffement : émetteurs infra-rouge
Exclusion de pluie Chauffage infra-rouge Lusignan 12 °C (ORE) Prairie temporaire Theix 9°C (ORE) Prairie permanente Mauguio 15°C Prairie temporaire Lautaret 2°C (CNRS) Alpage Lusignan 12 °C (ORE) Prairie temporaire Theix 9°C (ORE) Prairie permanente Mauguio 15°C Prairie temporaire Lautaret 2°C (CNRS) Alpage
ECOTRON CEFE-CNRS
Macrocosmes : monolithes de prairie (5 m2) prélevés à Theix
Scénario 2050 : réchauffement, pluviométrie
Un événement extrême est appliqué. Suivi des bilans C et eau, avec ou sans enrichissement en CO2
Expérience avec/sans extrêmes (chaleur, sécheresse) avec
ou sans enrichissement en CO
2Atelier de Réflexion Prospective
ADAGE
ADaptation de l’AGriculture et des Ecosystèmes
anthropisés au changement climatique
A. Approche générique
1.Traitement de l’incertitude dans les études d’adaptation 2. Traitement de la biodiversité et de la santé 3. Traitement de l’innovation 4. Traitement de l’adaptabilité et de la vulnérabilité B. Approche matricielle
5. Définition de la matrice utilisée et recensement des études nationales 6. Biome cultures – filières alimentaires ou
non
7. Biome prairies-savanes ; filière élevage 8. Biome forêts ; filière bois et fibres 9. Biome hydrosystèmes continentaux et
océaniques ; filière pêche 10. Agriculture de subsistance 11. Zones protégées et corridors de
biodiversité
C. Approche systémique
12. Interactions entre adaptation, atténuation et utilisations non alimentaires de la
biomasse
13. Adaptation et ressources en eau et en sols 14. Adaptation sécurité alimentaire et
compétitivité des filières 15. Adaptation et territoires
D. Coordination & Synthèse 16. Gestion de l’information et des connaissances 17. Coordination et gestion de l’ARP
A. Approche générique
1.Traitement de l’incertitude dans les études d’adaptation 2. Traitement de la biodiversité et de la santé 3. Traitement de l’innovation 4. Traitement de l’adaptabilité et de la vulnérabilité B. Approche matricielle
5. Définition de la matrice utilisée et recensement des études nationales 6. Biome cultures – filières alimentaires ou
non
7. Biome prairies-savanes ; filière élevage 8. Biome forêts ; filière bois et fibres 9. Biome hydrosystèmes continentaux et
océaniques ; filière pêche 10. Agriculture de subsistance 11. Zones protégées et corridors de
biodiversité
C. Approche systémique
12. Interactions entre adaptation, atténuation et utilisations non alimentaires de la
biomasse
13. Adaptation et ressources en eau et en sols 14. Adaptation sécurité alimentaire et
compétitivité des filières 15. Adaptation et territoires
D. Coordination & Synthèse 16. Gestion de l’information et des connaissances 17. Coordination et gestion de l’ARP
•
species and cultivar
•
soil properties
•
(re)distribution of pests and pathogens
•
direct effects of elevated CO
2(photosynthesis)
•
interactions between CO
2- air temp - water stress – mineral
nutrition…
•
and adaptive responses of plants…
Crop yield responses to climate change depend upon
53
Influence of global changes on plant
growth and survival and
sustainability of perennial grasses
54
Plan
I.
Background - Objectives
II.
The main drought survival strategies
in grasses
55
Importance of drought
Mediterranean areas :
Chronic summer droughts
severe water stress
Summer water deficit
• 300 – 1000 mm
• 45 - 30° latitude
Diagramme ombrothermique Montpellier (1970 - 2000) Mois 1 2 3 4 5 6 7 8 9 10 11 12 Pré cipitation s (mm) Te mpé ratur es x 2 (° C) 0 20 40 60 80 100 Drought Diagramme ombrothermique Rabat - maroc (1970 - 2000) Mois 1 2 3 4 5 6 7 8 9 10 11 12 Pré cipitation s (mm ) Te mp ér atur es x 2 (° C ) 0 20 40 60 80 100 Drought Montpellier (1970 –2000) Drought 3 months Rabat (1970 –2000) Drought 5 months P <2TMediterranean areas
Relevant field-research environment
to analyse plant responses
under
increasing summer aridity
predicted for larger areas
under climate change
63
Methodological key-points
Comparison of species and genotypes with
contrasting resistance
Dactylis glomerata
(orchardgrass), Lolium arundinaceum (tall
fescue), Lolium perenne (ray-grass), Phalaris tuberosa
(phalaris), Poa bulbosa
Realistic conditions
– Whole plant (well developed plants)
–
Realistic water deficits
(progression – intensity) plant
64
Agronomical consequences
Strategies of perennial forage grasses to survive severe drought
(Volaire, 2008)
Dactylis Mediterranean +++ +++ ++ +++ Temperate ++ ++ - ++ Tall Fescue Mediterranean ++++ ++ + +++ Temperate +++ + - ++ Lucerne ++++ + + +++
Red fescue-turf - - - -
Dehydration
Delay Tolerance
Drought survival
65
Importance of the summer dormancy trait
Drought survival strategies in perennial forage grasses
(Volaire, 2008)Dactylis Semi-arid +++ +++ ++++ ++++ Mediterranean +++ +++ ++ +++ Temperate ++ ++ - ++ Tall Fescue Semi-arid +++ +++ ++ ++ ++++ Mediterranean ++++ ++ + +++ Temperate +++ + - ++ Lucerne ++++ + + +++
Red fescue-turf - - - -
Dehydration Summer
Delay Tolerance Dormancy
Drought survival