Evolution of wetlands since the Last Glacial Maximum

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since the Last Glacial Maximum Pirita Oksanen University of Bristol

description

Evolution of wetlands since the Last Glacial Maximum. Pirita Oksanen University of Bristol. Wetland synthesis - distribution, extent, type and accumulation Public database Maps Data – model comparisons Since ca. 21 000 BP Phase 1. Northern extratropics. Phase 2. Tropics. - PowerPoint PPT Presentation

Transcript of Evolution of wetlands since the Last Glacial Maximum

Page 1: Evolution of wetlands since the Last Glacial Maximum

Evolution of wetlands since the Last Glacial Maximum

Pirita Oksanen University of Bristol

Page 2: Evolution of wetlands since the Last Glacial Maximum

• Wetland synthesis - distribution, extent, type and accumulation

• Public database• Maps• Data – model comparisons• Since ca. 21 000 BP• Phase 1. Northern extratropics.• Phase 2. Tropics.

Page 3: Evolution of wetlands since the Last Glacial Maximum

• Peatlands net sink of CO2 – vegetation sequesters from the atmosphere

• Wetlands net source of CH4 – methanogenesis in waterlogged environment

• ca. 5 million km2 natural wetlands• over 1 million km2 irrigated cultivation • 400-500 Gt C in peat• 100-150 Tg CH4/a from natural wetlands• ca. 40 Tg CH4/a from rice paddies• estimates for the LGM 80-110 Tg CH4/a

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• temperature, water table and vegetation control CH4 production and flux

• wide variation of CH4 fluxes both between and within wetlands and seasons

Mean values (Aselmann & Crutzen -89)• Bogs – 15 (1-50) CH4/m2/day• Fens – 80 (28-216)• Swamps – 84 (57-112)• Marshes – 253 (137-399)• Floodplains – 100 (50-200)• Lakes – 43 (17-89)• Rice paddies – 310 (179-438)

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~INLAND WETLANDS~

BOGS

SWAMPS

FENS

OPEN WETLANDS

MARSHES

SPRINGS GEOTHERMAL WETLANDSFLUVIAL

LACUSTRINE

Open WoodedRaised Blanket

Aapa

Rich Oligotrophic

Eutrophic Mesotrophic

Wooded

Paludifying forestSwamp forest Cloud forest

Raised Rich

Open

Eutrophic Mesotrophic

Shrub-swamp

Shrub-marshCarr Alder thicket

Palsa mirePolygonal mire

Wet tundra

High palsa mire Plateau palsa mire

Sloping mire

Wet meadow

Saline/brackish AlkalineFreshwater

Flooded meadow Sedge marsh

Terrestrialising lake

~COASTAL/MARINE WETLANDS~

INTERTIDAL MARSHES INTERTIDAL SWAMPS

AQUATIC BEDSINTERTIDAL FLATS

Salt marsh Salt meadow SaltingRaised FreshwaterBrackish

Mangrove Nipah

Tidal freshwater swamp forest

~HUMAN-MADE WETLANDS~

AGRICULTURAL

ARTIFICIAL LAKES

CANALSEXCAVATIONS

Rice field Wet meadow

Pond Reservoir

Wastewater treatment

Thermokarst lake

Wet moor

Oligotrophic

Alpine wet meadow

~NOT WETLAND~DRIED PEATLAND BURIED PEATLAND

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Wetland vegetation plant functional types

OPEN

mosses with dwarf-shrubs and forbs – bogs and fens

tall sedges and grasses (>1.5 m height) - fens and marshes

low sedges and grasses - fens and other open wetlands

open water

WOODED (>5% tree cover) - bogs and fens

wooded, evergreen broad-leaved

wooded, evergreen needle-leaved

wooded, seasonal broad-leaved

wooded, seasonal needle-leaved

FORESTED (>40% tree cover) - swamps

forested, evergreen broad-leaved

forested, evergreen needle-leaved

forested, seasonal broad-leaved

forested, seasonal needle-leaved

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Mires today, sites with bottom dates

Previous databases used: Oksanen 2005, Gorham et al. 2005, McDonald et al. 2006, PAIN.

Lappalainen et al. 1996

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Basal peat dates 50 000 – 21 000 BP

Continental and ice-sheet outlines by Patrick Bartlein, University of Oregon

Page 9: Evolution of wetlands since the Last Glacial Maximum

Mires at 13000 BP

Experimental ice-sheet data by W.R Peltier, University of Toronto

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Mires

at 11000 BP

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Mires at 10000 BP

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Mires

at 9000 BP

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Mires at 6000 BP, sites with basal peat dates

Continental and ice-sheet outlines by Patrick Bartlein, University of Oregon

Page 14: Evolution of wetlands since the Last Glacial Maximum

Mire initiation in arctic/boreal regions

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mire initiation casescumulative/ 5

0 2000 5000 8000 11000 15000 >21000