Vascular plant responses to elevated CO2 in a temperate lowland Sphagnum peatland

TY - JOUR

T1 - Vascular plant responses to elevated CO2 in a temperate lowland Sphagnum peatland

AU - Milla, Ruben

AU - Cornelissen, Johannes H. C.

AU - van Logtestijn, Richard S. P.

AU - Toet, Sylvia

AU - Aerts, Rien

PY - 2006/1

Y1 - 2006/1

N2 - Vascular plant responses to experimental enrichment with atmospheric carbon dioxide (CO2), using MINIFACE technology, were studied in a Dutch lowland peatland dominated by Sphagnum and Phragmites for 3 years. We hypothesized that vascular plant carbon would accumulate in this peatland in response to CO2 enrichment owing to increased productivity of the predominant species and poorer quality (higher C/N ratios) and consequently lower decomposability of the leaf litter of these species. Carbon isotope signatures demonstrated that the extra 180 ppmv CO2 in enriched plots had been incorporated into vegetation biomass accordingly. However, on the CO2 sequestration side of the ecosystem carbon budget, there were neither any significant responses of total aboveground abundance of vascular plants, nor of any of the individual species. On the CO2 release side of the carbon budget (decomposition pathway), litter quantity did not differ between ambient and CO2 treatments, while the changes in litter quality (N and P concentration, C/N and C/P ratio) were marginal and inconsistent. It appeared therefore that the afterlife effects of significant CO2-induced changes in green-leaf chemistry (lower N and P concentrations, higher C/N and C/P) were partly offset by greater resorption of mobile carbohydrates from green leaves during senescence in CO2-enriched plants. The decomposability of leaf litters of three predominant species from ambient and CO2-enriched plots, as measured in a laboratory litter respiration assay, showed no differences. The relatively short time period, environmental spatial heterogeneity and small plot sizes might explain part of the lack of CO2 response. When our results are combined with those from other Sphagnum peatland studies, the common pattern emerges that the vascular vegetation in these ecosystems is genuinely resistant to CO2-induced change. On decadal time-scales, water management and its effects on peatland hydrology, N deposition from anthropogenic sources and land management regimes that arrest the early successional phase (mowing, tree and shrub removal), may have a greater impact on the vascular plant species composition, carbon balance and functioning of lowland Sphagnum-Phragmites reedlands than increasing CO2 concentrations in the atmosphere.

AB - Vascular plant responses to experimental enrichment with atmospheric carbon dioxide (CO2), using MINIFACE technology, were studied in a Dutch lowland peatland dominated by Sphagnum and Phragmites for 3 years. We hypothesized that vascular plant carbon would accumulate in this peatland in response to CO2 enrichment owing to increased productivity of the predominant species and poorer quality (higher C/N ratios) and consequently lower decomposability of the leaf litter of these species. Carbon isotope signatures demonstrated that the extra 180 ppmv CO2 in enriched plots had been incorporated into vegetation biomass accordingly. However, on the CO2 sequestration side of the ecosystem carbon budget, there were neither any significant responses of total aboveground abundance of vascular plants, nor of any of the individual species. On the CO2 release side of the carbon budget (decomposition pathway), litter quantity did not differ between ambient and CO2 treatments, while the changes in litter quality (N and P concentration, C/N and C/P ratio) were marginal and inconsistent. It appeared therefore that the afterlife effects of significant CO2-induced changes in green-leaf chemistry (lower N and P concentrations, higher C/N and C/P) were partly offset by greater resorption of mobile carbohydrates from green leaves during senescence in CO2-enriched plants. The decomposability of leaf litters of three predominant species from ambient and CO2-enriched plots, as measured in a laboratory litter respiration assay, showed no differences. The relatively short time period, environmental spatial heterogeneity and small plot sizes might explain part of the lack of CO2 response. When our results are combined with those from other Sphagnum peatland studies, the common pattern emerges that the vascular vegetation in these ecosystems is genuinely resistant to CO2-induced change. On decadal time-scales, water management and its effects on peatland hydrology, N deposition from anthropogenic sources and land management regimes that arrest the early successional phase (mowing, tree and shrub removal), may have a greater impact on the vascular plant species composition, carbon balance and functioning of lowland Sphagnum-Phragmites reedlands than increasing CO2 concentrations in the atmosphere.

KW - CO2-enrichment

KW - FACE

KW - litter respiration

KW - nutrient resorption

KW - species abundance

KW - Sphagnum

KW - The Netherlands

KW - LEAF-LITTER DECOMPOSITION

KW - ATMOSPHERIC CO2

KW - OMBROTROPHIC BOG

KW - GROWTH-RESPONSE

KW - N DEPOSITION

KW - ECOSYSTEMS

KW - VEGETATION

KW - CHEMISTRY

KW - NORTHERN

KW - QUALITY

U2 - 10.1007/s11258-005-9028-9

DO - 10.1007/s11258-005-9028-9

M3 - Article

SN - 1385-0237

VL - 182

SP - 13

EP - 24

JO - Plant ecology

JF - Plant ecology

IS - 1-2

ER -