Bo Wallén

Growth-limiting nutrients in Sphagnum-dominated bogs subjects to low and high atmospheric nitrogen supply

The effects of increased nitrogen or phosphorus supply on the productivity of Sphagnum-dominated ombrotrophic bogs in northern and southern Sweden were studied. Atmospheric nitrogen deposition in souther Sweden (high-N site) exceeds that in northern Sweden (low-N site) by about tenfold. Vertical height growth of the Sphagnum carpet was measured by the crankedwire method. Length growth of individuals was measured by autoradiography after labelling with 14 CO 2 . The results of both methods were significantly correlated, but the cranked-wire data were systematically lower. Productivity of Sphagnum at the low-N site increase almost fourfold after additional nitrogen supply (4 g N m −1 year −1 ), but no increase was found after additional phosphorus supply (0.4 g P m −2 year −1 ) (...)

Vascular plant controls on methane emissions from northern peatforming wetlands

Methane emissions from wetlands are highly variable, both spatially and temporally and at scales ranging from microtopographic to regional differences. To comprehend this variation fully and also to predict responses to climate change, an understanding of the intimate linkage between carbon cycling and methane emission in these systems is needed. The presence of vascular plants has been recognized recently as one of the key factors controlling the scale of methane fluxes because it affects processes coupled to transport, production and consumption of methane. A wide area of research has therefore opened up, calling for investigations into details of the impact of vascular plants on methane emissions.

Interactions betweenSphagnum mosses and field layer vascular plants in the development of peat-forming systems

The interactions between field layer vascular plants andSphagnum mosses in peat-forming systems are discussed in terms of differences in growth strategies, access to light, acquisition of mineral nutrients and water and the processes involved in the formation of the micro-topographical structures characteristic for these systems.To keep pace with the vertical growth ofSphagnum, the co-occurring vascular plants require a growth strategy involving continuous movement of the growing point and meristematic tissue upwards and a frequent formation of adventitious roots.The growth form and architecture of the vascular plants determine the occurrence and distribution of the structural units on a mire, the hummocks, lawns and hollows. Dwarf shrubs and other vascular plants with an orthotropic growth pattern characterise hummocks, where they form a firm matrix which reinforces and supports the spongy biomass ofSphagnum. In a similar way, clonal herbs stabilise the lawns because of the predominantly plagiotropic, or only weakly orthotropic, growth pattern of the rhizomes and coarse roots in the upper, oxic layers.Extended periods of drought often may have deleterious effects on the mosses but smaller impacts on the vascular plants because of their more efficient water conducting system. Different sources of mineral nutrients are used bySphagnum (atmospheric deposition) and the vascular plants (mineralisation of the organic matter). The presence ofSphagnum, therefore, reduces the supply of nutrient resources to the vascular plants.Sphagnum thereby gains a competitive advantage. A high rate of mineralisation would be beneficial to the vascular plants by increasing their growth rates causing shading of theSphagnum mosses and covering the moss layer by the above-ground litter fall. However, the slow decomposition ofSphagnum litter keeps the system in balance as it will reduce the nutrient supply to the vascular plants.

Input rates, decay losses and accumulation rates of carbon in bogs during the last millennium: internal processes and environmental changes

In peatlands the balance between litter input and decay loss in the oxic acrotelm determines the rate of carbon input to the anoxic catotelm with carbon lost at very slow rate. In the acrotelm the C/N-quotient decreases with depth and indicates the loss of carbon from the acrotelm. On one boreo-nemoral and three subalpine ombrotrophic bogs in Sweden the carbon losses in the acrotelm plus the apparent carbon-accumu lation rates in the catotelm for the last millennium revealed a constant carbon-sequestering rate up to the end of the nineteenth century equalling that in recent Sphagnum-dominated communities. On the boreo-nemoral bog the carbon-accumulation rate in the catotelm decreased by 50% over the same period while it remained constant on the subalpine bogs. A catotelm with permafrost may have provided more constant conditions for the carbon accumulation than a rising water level creating anoxic conditions. Due to vegetation changes, the recent carbon sequestering in the peat-forming communities is lower than previously and only just enough to compensate for the integrated losses. It is argued that because of internal processes the bogs up to the end of the nineteenth century had obtained or were approaching a steady-state with regard to the carbon input to the catotelm and the supply of mineral nutrients. In contrast, an increased climatic humidity around 1000 cal. BP resulted in high carbon-accumulation rates in the boreo-nemoral bog. Climate could have triggered the recent vegetation changes, but an increased nitrogen deposition is also a probable reason.

STRATIGRAPHIC AND PALEOCLIMATIC STUDIES OF A 5500-YEAR-OLD MOSS BANK ON ELEPHANT ISLAND, ANTARCTICA

Analyses of a core from the deepest known moss peat bank in Antarctica, on Elephant Island, South Shetlands, show that this Chorisodontium aciphyllum-dominated bank began to grow ca. 5500 14C yr BP. Combined with other studies in the region the present study indicates more extensive glaciation before 5000 to 6000 BP than today on some of the South Shetland Islands. The main hypothesis is that these frozen moss banks contain important paleoclimatic information. The stratigraphic parameters analyzed included degree of humification, organic and mineral matter content, bulk density, chronology, volumetric growth and organic accumulation rates, carbon and nitrogen concentrations, C/N ratios, nitrogen accumulation rates, and finally magnetic analyses to detect tephra horizons. A discussion of the interrelationships between these parameters is followed by theoretical calculations of annual net primary productivity combined with multivariate analysis of the data set. Results of the analysis show that three calculated productivity peaks coincide with three periods of milder and more humid summers, at 4150-3900, 3180-3030, and 2030-1840 BP. However, the period with possibly the warmest summers, 3180-3030 BP, is interpreted also to have been characterized by cold winters. The data suggest that the periods with the coldest summers (and possibly also winters) prevailed at the earliest stage of the moss bank development, at ca. 3500 BP, and 2500 BP.

Spatial and temporal performance of the miniface (free air CO2 enrichment) system on bog ecosystems in northern and central Europe

The Bog Ecosystem Research Initiative (BERI) projectwas initiated to investigate, at five climaticallydifferent sites across Europe, the effects of elevatedCO2 and N deposition on the net exchange ofCO2 and CH4 between bogs and the atmosphere,and to study the effects of elevated CO2 and Ndeposition on the plant biodiversity of bogcommunities. A major challenge to investigate theeffects of elevated CO2 on vegetation andecosystems is to apply elevated CO2concentrations to growing vegetation without changingthe physical conditions like climate and radiation.Most available CO2 enrichment methods disturb thenatural conditions to some degree, for instance closedchambers or open top chambers. Free Air CO2Enrichment (FACE) systems have proven to be suitableto expose plants to elevated CO2 concentrationswith minimal disturbance of their natural environment.The size and spatial scale of the vegetation studiedwithin the BERI project allowed the use of a modifiedversion of a small FACE system called MiniFACE. Thispaper describes the BERI MiniFACE design as well asits temporal and spatial performance at the five BERIfield locations. The temporal performance of theMiniFACE system largely met the quality criteriadefined by the FACE Protocol. One minute averageCO2 concentrations measured at the centre of thering stayed within 20% of the pre-set target for morethan 95% of the time. Increased wind speeds werefound to improve the MiniFACE systems temporalperformance. Spatial analyses showed no apparentCO2 gradients across a ring during a 4 day periodand the mean differences between each sampling pointand the centre of the ring did not exceed 10%.Observations made during a windy day, causing aCO2 concentration gradient, and observations madeduring a calm day indicated that short term gradientstend to average out over longer periods of time. On aday with unidirectional strong winds, CO2concentrations at the upwind side of the ring centrewere higher than those made at the centre and at thedownwind side of the ring centre, but the bell-shapeddistribution was found basically the same for thecentre and the four surrounding measurement points,implying that the short term (1 sec) variability ofCO2 concentrations across the MiniFACE ring isalmost the same at any point in the ring. Based on gasdispersion simulations and measured CO2concentration profiles, the possible interferencebetween CO2-enriched and control rings was foundto be negligible beyond a centre-to-centre ringdistance of 6 m.

Leaf litter fall and soil acidity during half a century of secondary succession in a temperate deciduous forest

Vegetation, leaf litter fall and soil pH were sampled repeatedly within semipermanent plots in a South-Swedish deciduous forest, 1935–1983. Leaf litter fall was summarized in a litter quality index. Vegetation types were differentiated along similar gradients in soil pH and leaf litter quality. The greatest shifts in dominance among field layer species were found in those plots where the quality of the leaf litter had improved. These plots also showed a halt in the general tendency towards a decreasing pH in the top soil.

Inorganic elements above and below ground in dwarf shrubs on a subarctic peat bog

Concentrations of N, P, K, Na, Mg, Ca, Mn, Fe, Zn and Cu are given for four different biomass fractions (shoot with green leaves, stems and coarse roots above and below ground, and fine roots, respectively) of two dwarf shrubs, Andromeda polifolia L. and Empetrum hermaphroditum Hagerup, growing on a peat bog in subarctic Scandinavia. Two types of concentration gradients were found within the plants. When combined with biomass estimates from the same site, it was shown that 80% or more of the total plant content of these elements is in the fine roots (<0.5 mm). These observations from a very nutrient poor environment are discussed in relation to the turnover of plant nutrients in the ecosystem and the growth strategy of the