Net ecosystem carbon exchange in three contrasting Mediterranean ecosystems – the effect of drought

Droughts reduce gross primary production (GPP) and ecosystem respiration (Reco), contributing to most of the inter-annual variability in terrestrial carbon sequestration. In seasonally dry climates (Mediterranean), droughts result from reductions in annual rainfall and changes in rain seasonality. W...

Full description

Bibliographic Details
Main Authors: T. S. David, T. A. Paço, J. Banza, V. Andrade, J. S. David, C. Pio, G. Pita, L. M. Aires, J. A. Mateus, J. S. Pereira, A. Rodrigues
Format: Article
Language:English
Published: Copernicus Publications 2007-09-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/4/791/2007/bg-4-791-2007.pdf
_version_ 1818551422729322496
author T. S. David
T. A. Paço
J. Banza
V. Andrade
J. S. David
C. Pio
G. Pita
L. M. Aires
J. A. Mateus
J. S. Pereira
A. Rodrigues
author_facet T. S. David
T. A. Paço
J. Banza
V. Andrade
J. S. David
C. Pio
G. Pita
L. M. Aires
J. A. Mateus
J. S. Pereira
A. Rodrigues
author_sort T. S. David
collection DOAJ
description Droughts reduce gross primary production (GPP) and ecosystem respiration (Reco), contributing to most of the inter-annual variability in terrestrial carbon sequestration. In seasonally dry climates (Mediterranean), droughts result from reductions in annual rainfall and changes in rain seasonality. We compared carbon fluxes measured by the eddy covariance technique in three contrasting ecosystems in southern Portugal: an evergreen oak woodland (savannah-like) with ca.~21% tree crown cover, a grassland dominated by herbaceous annuals and a coppiced short-rotation eucalyptus plantation. During the experimental period (2003&ndash;2006) the eucalyptus plantation was always the strongest sink for carbon: net ecosystem exchange rate (NEE) between &minus;861 and &minus;399 g C m<sup>&minus;2</sup> year<sup>&minus;1</sup>. The oak woodland and the grassland were much weaker sinks for carbon: NEE varied in the oak woodland between &minus;140 and &minus;28 g C m<sup>&minus;2</sup> year<sup>&minus;1</sup> and in the grassland between &minus;190 and +49 g C m<sup>&minus;2</sup> year<sup>&minus;1</sup>. The eucalyptus stand had higher GPP and a lower proportion of GPP spent in respiration than the other systems. The higher GPP resulted from high leaf area duration (LAD), as a surrogate for the photosynthetic photon flux density absorbed by the canopy. The eucalyptus had also higher rain use efficiency (GPP per unit of rain volume) and light use efficiency (the daily GPP per unit incident photosynthetic photon flux density) than the other two ecosystems. The effects of a severe drought could be evaluated during the hydrological-year (i.e., from October to September) of 2004&ndash;2005. Between October 2004 and June 2005 the precipitation was only 40% of the long-term average. In 2004&ndash;2005 all ecosystems had GPP lower than in wetter years and carbon sequestration was strongly restricted (less negative NEE). The grassland was a net source of carbon dioxide (+49 g C m<sup>&minus;2</sup> year<sup>&minus;1</sup>). In the oak woodland a large proportion of GPP resulted from carbon assimilated by its annual vegetation component, which was strongly affected by the shortage of rain in winter. Overall, severe drought affected more GPP than Reco leading to the deterioration of NEE. Although the rain-use efficiency of the eucalyptus plantation increased in the dry year, this was not the case of evergreen oak woodland, which rain-use efficiency was not influenced by drought. Recovery after drought alleviation, i.e., beginning with heavy rain in October 2005, was fully accomplished in 2006 in the oak woodland and grassland, but slow in the eucalyptus plantation.
first_indexed 2024-12-12T08:59:41Z
format Article
id doaj.art-03d70f66089b4e3f9d4ef6c2413c0f45
institution Directory Open Access Journal
issn 1726-4170
1726-4189
language English
last_indexed 2024-12-12T08:59:41Z
publishDate 2007-09-01
publisher Copernicus Publications
record_format Article
series Biogeosciences
spelling doaj.art-03d70f66089b4e3f9d4ef6c2413c0f452022-12-22T00:29:52ZengCopernicus PublicationsBiogeosciences1726-41701726-41892007-09-0145791802Net ecosystem carbon exchange in three contrasting Mediterranean ecosystems &ndash; the effect of droughtT. S. DavidT. A. PaçoJ. BanzaV. AndradeJ. S. DavidC. PioG. PitaL. M. AiresJ. A. MateusJ. S. PereiraA. RodriguesDroughts reduce gross primary production (GPP) and ecosystem respiration (Reco), contributing to most of the inter-annual variability in terrestrial carbon sequestration. In seasonally dry climates (Mediterranean), droughts result from reductions in annual rainfall and changes in rain seasonality. We compared carbon fluxes measured by the eddy covariance technique in three contrasting ecosystems in southern Portugal: an evergreen oak woodland (savannah-like) with ca.~21% tree crown cover, a grassland dominated by herbaceous annuals and a coppiced short-rotation eucalyptus plantation. During the experimental period (2003&ndash;2006) the eucalyptus plantation was always the strongest sink for carbon: net ecosystem exchange rate (NEE) between &minus;861 and &minus;399 g C m<sup>&minus;2</sup> year<sup>&minus;1</sup>. The oak woodland and the grassland were much weaker sinks for carbon: NEE varied in the oak woodland between &minus;140 and &minus;28 g C m<sup>&minus;2</sup> year<sup>&minus;1</sup> and in the grassland between &minus;190 and +49 g C m<sup>&minus;2</sup> year<sup>&minus;1</sup>. The eucalyptus stand had higher GPP and a lower proportion of GPP spent in respiration than the other systems. The higher GPP resulted from high leaf area duration (LAD), as a surrogate for the photosynthetic photon flux density absorbed by the canopy. The eucalyptus had also higher rain use efficiency (GPP per unit of rain volume) and light use efficiency (the daily GPP per unit incident photosynthetic photon flux density) than the other two ecosystems. The effects of a severe drought could be evaluated during the hydrological-year (i.e., from October to September) of 2004&ndash;2005. Between October 2004 and June 2005 the precipitation was only 40% of the long-term average. In 2004&ndash;2005 all ecosystems had GPP lower than in wetter years and carbon sequestration was strongly restricted (less negative NEE). The grassland was a net source of carbon dioxide (+49 g C m<sup>&minus;2</sup> year<sup>&minus;1</sup>). In the oak woodland a large proportion of GPP resulted from carbon assimilated by its annual vegetation component, which was strongly affected by the shortage of rain in winter. Overall, severe drought affected more GPP than Reco leading to the deterioration of NEE. Although the rain-use efficiency of the eucalyptus plantation increased in the dry year, this was not the case of evergreen oak woodland, which rain-use efficiency was not influenced by drought. Recovery after drought alleviation, i.e., beginning with heavy rain in October 2005, was fully accomplished in 2006 in the oak woodland and grassland, but slow in the eucalyptus plantation.http://www.biogeosciences.net/4/791/2007/bg-4-791-2007.pdf
spellingShingle T. S. David
T. A. Paço
J. Banza
V. Andrade
J. S. David
C. Pio
G. Pita
L. M. Aires
J. A. Mateus
J. S. Pereira
A. Rodrigues
Net ecosystem carbon exchange in three contrasting Mediterranean ecosystems &ndash; the effect of drought
Biogeosciences
title Net ecosystem carbon exchange in three contrasting Mediterranean ecosystems &ndash; the effect of drought
title_full Net ecosystem carbon exchange in three contrasting Mediterranean ecosystems &ndash; the effect of drought
title_fullStr Net ecosystem carbon exchange in three contrasting Mediterranean ecosystems &ndash; the effect of drought
title_full_unstemmed Net ecosystem carbon exchange in three contrasting Mediterranean ecosystems &ndash; the effect of drought
title_short Net ecosystem carbon exchange in three contrasting Mediterranean ecosystems &ndash; the effect of drought
title_sort net ecosystem carbon exchange in three contrasting mediterranean ecosystems ndash the effect of drought
url http://www.biogeosciences.net/4/791/2007/bg-4-791-2007.pdf
work_keys_str_mv AT tsdavid netecosystemcarbonexchangeinthreecontrastingmediterraneanecosystemsndashtheeffectofdrought
AT tapaco netecosystemcarbonexchangeinthreecontrastingmediterraneanecosystemsndashtheeffectofdrought
AT jbanza netecosystemcarbonexchangeinthreecontrastingmediterraneanecosystemsndashtheeffectofdrought
AT vandrade netecosystemcarbonexchangeinthreecontrastingmediterraneanecosystemsndashtheeffectofdrought
AT jsdavid netecosystemcarbonexchangeinthreecontrastingmediterraneanecosystemsndashtheeffectofdrought
AT cpio netecosystemcarbonexchangeinthreecontrastingmediterraneanecosystemsndashtheeffectofdrought
AT gpita netecosystemcarbonexchangeinthreecontrastingmediterraneanecosystemsndashtheeffectofdrought
AT lmaires netecosystemcarbonexchangeinthreecontrastingmediterraneanecosystemsndashtheeffectofdrought
AT jamateus netecosystemcarbonexchangeinthreecontrastingmediterraneanecosystemsndashtheeffectofdrought
AT jspereira netecosystemcarbonexchangeinthreecontrastingmediterraneanecosystemsndashtheeffectofdrought
AT arodrigues netecosystemcarbonexchangeinthreecontrastingmediterraneanecosystemsndashtheeffectofdrought