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Fire disturbance regimes and vegetation interactions in East Africa during the Late Quaternary Colin J. Courtney Mustaphi , Nicolas Deere, Esther Githumbi, Rob Marchant * York Institute for Tropical Ecosystems, Environment Department, University of York, United Kingdom *[email protected] Decadal-to-millennial scale controls of fire Natural influences on fire regimes Anthropogenic influences Land-use changes Infrastructure, irrigation Plant assemblage changes Biomass abundance changes Disturbance (pests, herbivores) Long-term palaeoenvironmental context Palaeoclimatology Palaeoecology Sedimentology Data syntheses Lines of inquiry and major toolsets Introduction Approach (1) Bonnefille R., Chalié F., 2000. Pollen-inferred precipitation time-series from Equatorial mountains, Africa, the last 40 kyr BP. Global and Planetary Change, 26: 25-50. (2) Tierney et al, 2010. A molecular perspective on Late Quaternary climate and vegetation change in the Lake Tanganyika basin, East Africa. Quaternary Science Reviews 29: 787-800. (3) Fire Information for Resource Management System https://earthdata.nasa.gov/data/near-real-time-data/firms: MOD14/MYD14 (4) AfSIS online data repository (http://www.africasoils.net/data/datasets?page=1) (5) Trabucco et al., 2009. Global Aridity Index and Global Potential Evapo-Transpiration Geospatial Database. CGIAR Consortium for Spatial Information. ttp://www.csi.cgiar.org/ (6) Platts et al, 2011. Delimiting tropical mountain ecoregions for conservation. Environmental Conservation, 38: 312-324. PAGES KU Leuven Feb 3-7, 2014 Fig. 1: Overview of major long-term influences of vegetation cover and fire activity. 2D 2E 2F 2G References. www.york.ac.uk/environment/research/kite www.indie403.com/paleo Visit us!! Human land-use patterns Archaeological info Anthropological info Demographic change Recent vegetation and fire regime changes Air photos Satellite imagery MODIS data Effects on Microclimates Global climate change Photo: Colin Beale, U of York Accidental/purposeful burning Direct + indirect plant assemblage changes Arid or moist conditions Climate-mediated changes to vegetation Climate variability Climatic Influences Landscape Influences Fuel Characteristics climate fuel landscape Orientation Slope Channeling Erosion www.real-project.eu Photo: Anna Shoemaker Photo: Anna Shoemaker Study region 2C 0 2000 4000 6000 8000 10000 12000 14000 16000 18000 20000 -2.5 0.0 2.5 5.0 z-score Biomass burning -800 -400 0 400 800 mm/yr Precipitation 21 23 25 27 °C Temperature Human history Pastoralism Year BP −150 −50 0 50 100 150 −40 0 40 Longitude Latitude Site used in biomass burning composite 2B We use a blend of palaeoenvironmental approaches, ranging from establishing new proxy records from sediment cores (Fig.2A), synthesising available palaeoecoinformatics from large databases (Fig.2B), remotely-sensed data (Figs.2C-G), and integrate data from the social sciences. By examining the major controls of fire activity over the recent period and in long-term reconstructions of vegetation and biomass burning we will begin to constrain the signal of anthropogenic ecosystem change and understand how these environments may respond in the future. 2A and B 2C to F 2G www.real-project.eu 2A Fig. 2: Showing the integrative study required to disentangle fire dynamics: these include A) coring swamp sediments for new proxy records. B) Synthesis of existing records, such as a biomass burning composite using 7 sites in East Africa from the Global Charcoal Database v3; reconstructed precipitation differences from modern precipitation (1); and reconstructed annual temperatures from the Lake Tanganyika basin (2). 2 2 East African C) annual fire hotspots; D) fire radiative power (W/m ), both as 10 year averages (>50% confidence; 2001-2010) from MODIS active fire data (3); E) net primary productivity (kg C/m ),10 year average (4); F) aridity index (mean annual precipitation/mean annual potential evapotranspiration (5); G) population pressure exerted on the landscape (distance decay function, σ = 5) (6). Fire is one of the most important disturbances to vegetation and influences ecosystem structure and function. Human use of fire on the landscape has influenced vegetation composition, biomass abundance, and biodiversity in many ecosystems. Fire management also has implications for carbon cycling and can result in a net carbon sink or source under certain conditions. There ecosystem interactions guide our research questions: To what extent have humans influenced fire regimes and vegetation? What are the important spatial controls of fire activity (Fig.1)?

interactions in East Africa during the Late Quaternary€¦ · Site used in biomass burning composite 2B We use a blend of palaeoenvironmental approaches, ranging from establishing

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Page 1: interactions in East Africa during the Late Quaternary€¦ · Site used in biomass burning composite 2B We use a blend of palaeoenvironmental approaches, ranging from establishing

Fire disturbance regimes and vegetationinteractions in East Africa during the Late Quaternary

Colin J. Courtney Mustaphi , Nicolas Deere, Esther Githumbi, Rob Marchant*

York Institute for Tropical Ecosystems, Environment Department, University of York, United Kingdom

*[email protected]

Decadal-to-millennialscale controls of fire

Natural influenceson fire regimes

Anthropogenicinfluences

Land-use changes

Infrastructure, irrigation

Plant assemblage changes

Biomass abundance changes

Disturbance (pests, herbivores)

Long-termpalaeoenvironmental

contextPalaeoclimatologyPalaeoecologySedimentologyData syntheses

Lines of inquiry and major toolsets

Introduction

Approach

(1) Bonnefille R., Chalié F., 2000. Pollen-inferred precipitation time-series from Equatorial mountains, Africa, the last 40 kyr BP. Global and Planetary Change, 26: 25-50.(2) Tierney et al, 2010. A molecular perspective on Late Quaternary climate and vegetation change in the Lake Tanganyika basin, East Africa. Quaternary Science Reviews 29: 787-800.(3) Fire Information for Resource Management System https://earthdata.nasa.gov/data/near-real-time-data/firms: MOD14/MYD14(4) AfSIS online data repository (http://www.africasoils.net/data/datasets?page=1)(5) Trabucco et al., 2009. Global Aridity Index and Global Potential Evapo-Transpiration Geospatial Database. CGIAR Consortium for Spatial Information. ttp://www.csi.cgiar.org/ (6) Platts et al, 2011. Delimiting tropical mountain ecoregions for conservation. Environmental Conservation, 38: 312-324.

PAGES KU Leuven Feb 3-7, 2014

Fig. 1: Overview of major long-terminfluences of vegetation cover and fire activity.

2D 2E 2F 2G

References.

www.york.ac.uk/environment/research/kitewww.indie403.com/paleo

Visit us!!

Human land-usepatterns

Archaeological infoAnthropological infoDemographic change

Recent vegetationand

fire regime changes

Air photosSatellite imageryMODIS data

Effects on Microclimates

Global climate change

Photo: Colin Beale, U of York

Accidental/purposeful burning

Direct + indirect plantassemblage changes

Arid or moist conditions

Climate-mediated changesto vegetation

Climate variability

ClimaticInfluences

LandscapeInfluences

FuelCharacteristics

clim

ate

fuel

landscape

Orientation

Slope

Channeling

Erosion

www.real-project.eu

Photo: Anna Shoemaker Photo: Anna Shoemaker

Study region

2C

0

2000

4000

6000

8000

10000

12000

14000

16000

18000

20000 -2.5 0.0 2.5 5.0

z-score

Biom

assbu

rning

-800 -400 0 400 800

mm/yr

Precipita

tion

21 23 25 27

°C

Tem

pera

ture

Hum

an h

isto

ry

Past

ora

lism

Year

BP

−150 −50 0 50 100 150

−4

00

40

Longitude

La

titu

de

Site used in biomass burning composite

2B

We use a blend of palaeoenvironmental approaches, ranging from establishing new proxy records from sediment cores (Fig.2A), synthesisingavailable palaeoecoinformatics from large databases (Fig.2B), remotely-sensed data (Figs.2C-G), and integrate data from the social sciences.By examining the major controls of fire activity over the recent period and in long-term reconstructions of vegetation and biomass burning wewill begin to constrain the signal of anthropogenic ecosystem change and understand how these environments may respond in the future.

2A and B 2C to F

2G

www.real-project.eu

2A

Fig. 2: Showing the integrative study required to disentangle fire dynamics: these include A) coring swamp sediments for new proxy records. B) Synthesis of existing records, such as a biomass burning compositeusing 7 sites in East Africa from the Global Charcoal Database v3; reconstructed precipitation differences from modern precipitation (1); and reconstructed annual temperatures from the Lake Tanganyika basin (2).

2 2East African C) annual fire hotspots; D) fire radiative power (W/m ), both as 10 year averages (>50% confidence; 2001-2010) from MODIS active fire data (3); E) net primary productivity (kg C/m ),10 year average (4);F) aridity index (mean annual precipitation/mean annual potential evapotranspiration (5); G) population pressure exerted on the landscape (distance decay function, σ = 5) (6).

Fire is one of the most important disturbances to vegetation and influences ecosystem structure and function. Human use of fire on the landscapehas influenced vegetation composition, biomass abundance, and biodiversity in many ecosystems. Fire management also has implications for carbon cycling and can result in a net carbon sink or source under certain conditions. There ecosystem interactions guide our research questions:To what extent have humans influenced fire regimes and vegetation? What are the important spatial controls of fire activity (Fig.1)?