Environmental and vegetation drivers of seasonal CO2 fluxes in a sub-arctic forest–mire ecotone

Poyatos, Rafael; Heinemeyer, Andreas; Ineson, Phil; Evans, Jonathan G. ORCID: https://orcid.org/0000-0003-4194-1416; Ward, Helen C.; Huntley, Brian; Baxter, Robert. 2014 Environmental and vegetation drivers of seasonal CO2 fluxes in a sub-arctic forest–mire ecotone. Ecosystems, 17 (3). 377-393. https://doi.org/10.1007/s10021-013-9728-2

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Official URL: https://link.springer.com/article/10.1007/s10021-0...

Abstract/Summary

Unravelling the role of structural and environmental drivers of gross primary productivity (GPP) and ecosystem respiration (Reco) in highly heterogeneous tundra is a major challenge for the upscaling of chamberbased CO2 fluxes in Arctic landscapes. In a mountain birch woodland-mire ecotone, we investigated the role of LAI (and NDVI), environmental factors (microclimate, soil moisture), and microsite type across tundra shrub plots (wet hummocks, dry hummocks, dry hollows) and lichen hummocks, in controlling net ecosystem CO2 exchange (NEE). During a growing season, we measured NEE fluxes continuously, with closed dynamic chambers,andperformedmultiple fits (onefor each 3-day period) of a simple light and temperature response model to hourlyNEE data. Tundra shrub plots were largely CO2 sinks, as opposed to lichen plots, although fluxes were highly variable within microsite type. For tundra shrub plots, microsite type did not influence photosynthetic parameters but it affected basal (that is, temperature-normalized) ecosystem respiration (R0). PAR-normalized photosynthesis (P600) increased with air temperature and declined with increasing vapor pressure deficit. R0 declined with soil moisture and showed an apparent increase with temperature, which may underlie a tight link between GPP and Reco. NDVI was a good proxy for LAI, maximum P600 and maximum R0 of shrub plots. Cumulative CO2 fluxes were strongly correlated with LAI (NDVI) but we observed a comparatively low GPP/LAI in dry hummocks. Our results broadly agree with the reported functional convergence across tundra vegetation, but here we show that the role of decreased productivity in transition zones and the influence of temperature and water balance on seasonal CO2 fluxes in sub-Arctic forest–mire ecotones cannot be overlooked.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1007/s10021-013-9728-2
UKCEH and CEH Sections/Science Areas:	Acreman Reynard
ISSN:	1432-9840
Additional Keywords:	carbon balance, ecosystem respiration, gross primary productivity, leaf area index, lichen, NDVI, net ecosystem exchange, soil moisture, transition zones, tundra
Date made live:	13 Mar 2019 14:31 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/522492

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1007/s10021-013-9728-2

UKCEH and CEH Sections/Science Areas:

Acreman
Reynard

ISSN:

1432-9840

Additional Keywords:

carbon balance, ecosystem respiration, gross primary productivity, leaf area index, lichen, NDVI, net ecosystem exchange, soil moisture, transition zones, tundra

Date made live:

13 Mar 2019 14:31 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/522492