Organic Matter Accumulation and Community Change at the Peatland–Upland Interface: Inferences from 14C and 210Pb Dated Profiles

Peatland-margin habitats with organic matter accumulation of 40–150 cm make up a significant but poorly quantified portion of Canada’s boreal forest region. Spanning the transition between non-wetland forest and fen proper, these ecosystems represent a zone of complex environmental and vegetation change, yet little is known about their ecological function or development. We here use vegetation and macrofossil analysis, traditional ¹⁴C, bomb-spike ¹⁴C, and ²¹⁰Pb dating to investigate the development, organic matter accumulation, and recent vegetation history of peat margin communities at two sites in central Saskatchewan, Canada. Although similar in general shape, bomb-spike ¹⁴C and ²¹⁰Pb chronologies show limited agreement in three of the four profiles examined, with ²¹⁰Pb generally producing younger ages than ¹⁴C. Peat initiation and long-term organic matter accumulation at the Old Black Spruce (OBS) transect were probably driven mainly by the dynamics of Sphagnum, whereas at the Sandhill Fen (SF) transect, they were controlled by water level fluctuations in the neighboring fen. Bryophyte macrofossils suggest a recent drying of the vegetation surface at both sites, most likely triggered by regional drought in the late 1950s and 1960s. At OBS, the shift from Sphagnum- to feather moss-dominated communities continued in the 1990s, possibly reflecting effects of direct disturbance on local drainage patterns. Overall, our results suggest that community composition and C dynamics of peat-margin swamps respond dynamically to climatic and hydrologic fluctuations. However, uncertainties regarding the reliability of different chronologies limit our ability to link observed community changes to specific causal events. Author Contributions  IEB conceived/designed study, performed research, analyzed data, wrote paper. JSB conceived/designed study, wrote paper. CS performed research, analyzed data, wrote paper. RKW performed research and analyzed data. CMP performed research and wrote paper.     

香蒲对不同浓度Pb~(2+)胁迫的生理应答及其细胞超微结构变化

通过室内水培试验,研究了不同浓度Pb2+(0、0.25、0.50、1.00和2.00mmol·L-1)胁迫对东方香蒲根和叶中Pb含量、叶绿素含量、丙二醛(MDA)含量、抗氧化酶(SOD、CAT和POD)活性以及亚细胞结构的影响。结果显示:(1)随着外源Pb2+浓度的增加,Pb在香蒲根和叶中的积累量均显著高于对照,且Pb在根中的含量明显高于叶中,并与外源Pb2+浓度呈显著正相关关系。(2)香蒲叶片中的叶绿素a和叶绿素b含量随着外源Pb2+浓度的增加呈先升后降趋势,均在处理浓度为0.50mmol·L-1时达到峰值。(3)胁迫处理叶片的MDA含量与对照相比变化不显著,但根中MDA含量呈显著下降趋势。(4)叶片中SOD活性在1.00mmol·L-1 Pb2+处理时达到峰值,然后下降,但始终高于对照,CAT和POD活性则均低于对照组;根中SOD活性除1.00mmol·L-1 Pb2+处理组外均显著低于对照组,CAT和POD活性分别在0.25和0.50mmol·L-1 Pb2+处理时达到峰值,然后随处理Pb2+浓度升高而下降。(5)电镜观察发现,Pb2+胁迫使香蒲叶细胞中叶绿体被膜破裂,类囊体膨胀、破损;根和叶细胞中的线粒体被膜均破裂、内腔空泡化,细胞核核膜破损、核仁消失、染色质凝集。研究表明,Pb2+胁迫致使东方香蒲根、叶生理代谢失衡,亚细胞结构出现不可逆的损伤,这为从分子水平研究Pb2+作用的具体机理以及香蒲在重金属污染修复中的应用提供了依据。     

Peat and water chemistry at Big Run Bog,a peatland in the Appalachian mountains of West Virginia,USA

At Big Run Bog, aSphagnum-dominated peatland in the unglaciated Appalachian Plateau of West Virginia, significant spatial variation in the physical and chemical properties of the peat and in surface and subsurface (30 cm deep) water chemistry was characterized. The top 40 cm of organic peat at Big Run Bog had average values for bulk density of 0.09 g · cm^–3, organic matter concentration of 77%, and volumetric water content of 88%. Changes in physical and chemical properties within the peat column as a function of depth contributed to different patterns of seasonal variation in the chemistry of surface and subsurface waters. Seasonal variation in water chemistry was related to temporal changes in plant uptake, organic matter decomposition and element mineralization, and to varying redox conditions associated with fluctuating water table levels. On the average, total Ca, Mg, and N concentrations in Big Run Bog peat were 33, 15, and 1050 mol · g^–1, respectively; exchangeable Ca and Mg concentrations were 45 and 14 eq · g^–1 , respectively. Surface water pH averaged 4.0 and Ca⁺⁺ concentrations were less than 50 eq · L^–1 . These chemical variables have all been used to distinguish bogs from fens. Physiographically, Big Run Bog is a minerotrophic fen because it receives inputs of water from the surrounding forested upland areas of its watershed. However, chemically, Big Run Bog is more similar to true ombrotrophic bogs than to minerotrophic fens.     

Immobilization,mineralization and the availability of the fertilizer nitrogen during the decomposition of the organic matters applied to the soil

Summary Immobilization and mineralization of the tracer nitrogen (K¹⁵NO₃) applied to the soil together with several organic matters during their decomposition was investigated in incubation experiments.After incubation for three months at 30°C, the decomposition rates of rice straw, hardwood bark, sawdust, softwood bark and peat moss were 41, 15, 7, 5, and 5%, respectively. After incubation for three months at 30°C, 100 and 80% of the fertilizer nitrogen were immobilized in the treatment with 2.0% of rice straw and sawdust carbon, respectively. These resulted in the lowered uptake of the fertilizer nitrogen by plants. In case of peat moss and barks, the amount of fertilizer nitrogen which transformed to the organic nitrogen fractions was quite small and the plant uptake of the nitrogen was hardly affected. Remineralization of the immobilized nitrogen was clearly observed after 2 months' incubation in case where rice straw carbon was added to the extent of 0.5 and 1.0%, but it was not observed in case where other organic matter carbon was added.The data showed that peat moss and barks were highly resistant to the action of microorganisms. As a results the immobilization process of the fertilizer nitrogen incubated with these organic matter was quite slow.     

Microcalorimetric Study on the Toxic Effect of Pb<Superscript>2+</Superscript> to <Emphasis Type="Italic">Tetrahymena</Emphasis>

The toxic effect of Pb²⁺ has been studied in eukaryotic cells by using Tetrahymena as a target. The maximum power (P _m) and the growth rate constant (k) were determined, which showed that values of P _m and k were linked to the concentration (C) of Pb²⁺. The addition of Pb²⁺ caused a decrease of the maximum heat production and growth rate constant, indicating that Tetrahymena growth was inhibited in the presence of Pb²⁺, and Pb²⁺ took part in the metabolism of cells. From micrographs, morphological changes of Tetrahymena were observed with addition of Pb²⁺, indicating that the toxic effect of Pb²⁺ derived from destroying the membrane of surface of Tetrahymena. According to the thermogenic curves and photos of Tetrahymena under different conditions, it is clear that metabolic mechanism of Halobacterium halobium R1 growth has been changed with the addition of Pb²⁺.     

Cosmogenic 10Be as a potential dating tool in peat

Because ombrotrophic peat bogs receive inputs of water, nutrients, pollutants, and xerobiotic materials solely from the atmosphere, and accumulate organic matter vertically, dated peat cores can provide a historical record of deposition. We propose a novel method for accurately determining dates of peat, based on cosmogenic ¹⁰Be. In a laboratory study, we document limited post-depositional mobility of atmospherically-deposited Be, a requisite for ¹⁰Be dating. We provide an example of how the ²¹⁰Pb-dated upper portion of a peat core can be used to back-calculate a site-specific ¹⁰Be deposition rate, which can then be used to estimate dates for peat throughout a core, and also discuss limitations to the application of cosmogenic ¹⁰Be to the dating of peat deposits.     

Unique Characteristics of Pb in Soil Contaminated by Red Lead Anti-Corrosion Paint

Red lead (Pb₃O₄) has been extensively used in the past in anti-corrosion paints for the protection of steel constructions such as electricity pylons or bridges. Until recently, little has been known about the behavior of these Pb compounds in soils. Therefore, three pylon soils and six red lead anti-corrosion paints were characterized in terms of solubility, Pb mineral composition, extractability, sorption and desorption, and the chemical speciation of Pb in soil extracts. The pylon soils were characterized by moderate total Pb concentrations (≈700 mg kg^?1), while NH₄NO₃ extractable Pb was exceptionally high (up to 15% of total Pb). In soil extracts, the free Pb²⁺ fraction ranged from 33 to 81% of total soluble Pb. The equilibrium concentration of Pb derived from Pb₃O₄ in ultra-pure water reached 68.5 mg L^?1. This high solubility explains the observed high extractability in soils and contradicts earlier reports of much lower water solubilities of the compound.     

Estimation of biological nitrogen fixation associated withBrachiaria andPaspalum grasses using15N labelled organic matter and fertilizer

Summary Six pasture grasses,Paspalum notatum cv batatais,P. notatum cv pensacola,Brachiaria radicans, B. ruziziensis, B. decumbens andB. humidicola, were grown in concrete cylinders (60 cm diameter) in the field for 31 months. The soil was amended with either a single addition of¹⁵N labelled organic matter or frequent small (2 kg N. ha^–1) additions of¹⁵N enriched (NH₄)₂SO₄. In the labelled fertilizer treatment soil analysis revealed that there was a very drastic change in¹⁵N enrichment in plant-available nitrogen (NO ₃ ^– +NH ₄ ⁺ ) with depth. The different grass cultivars recovered different quantities of applied labelled N, and evidence was obtained to suggest that the roots exploited the soil to different depths thus obtaining different¹⁵N enrichments in soil derived N. This invalidated the application of the isotope dilution technique to estimate the contribution of nitrogen fixation to the grass cultivars in this treatment. In the labelled organic matter treatment the¹⁵N label in the plant-available N declined at a decreasing rate during the experiment until in the last 12 months the decrease was only from 0.274 to 0.222 atom % excess. There was little change in¹⁵N enrichment of available N with depth, hence it was concluded that although the grasses recovered different quantities of labelled N, they all obtained virtually the same¹⁵N enrichment in soil derived N. Data from the final harvests of this treatment indicated thatB. humidicola andB. decumbens obtained 30 and 40% respectively of their nitrogen from N₂ fixation amounting to an input of 30 and 45 kg N.ha^–1 year^–1 respectively.     

The inventories of anthropogenic Ph,Zn, As,Cd, and the radionuclides 137Cs and excess 210Pb in lake sediments of the Adirondack region,USA

We determined the inventories of four anthropogenic trace elements, Pb, Zn, As, and Cd, and two radionuclides, ¹³⁷Cs and excess ²¹⁰Pb, in sediment cores collected from eight remote lakes in the Adirondack region of the northeastern United States. The inventories of all six substances vary considerably among the sediment cores, although the lakes and their associated catchments must have received similar cumulative per unit area atmospheric inputs of these substances. These variations are highly correlated, indicating that the trace elements and radionuclides are affected in a coherent way by the processes controlling their deposition to the sediments of these lakes. Assuming that the anthropogenic trace element inventories in each sediment core are enhanced or depleted relative to cumulative atmospheric deposition to the extent indicated by the sediment core inventories of either ¹³⁷Cs or excess ²¹⁰Pb, we produced estimates of the cumulative atmospheric inputs of the four anthropogenic trace elements to this region. Comparison of the excess ²¹⁰Pb normalized anthropogenic Pb, Zn, Cd inventories of the Adirondack sediment cores with excess ²¹⁰Pb normalized inventories of the same substances in a group of South Central Ontario lakes suggests that the Adirondack region has received greater cumulative anthropogenic inputs of Pb, Zn and Cd by a factor of 1.6, 4.5, and 2.9, respectively.     

Five decades of rapid forest spread in the Pieria Mountains (N. Greece) reconstructed by means of high-resolution pollen analysis and aerial photographs

The rapid spread of pine forests on the western side of the Pieria Mountains (N. Greece) began in 1945 and was facilitated by the recession of human activity and the siliceous geological substrate of the area. The pine expansion is visible not only in the vegetation maps for the years 1945, 1960 and 1992 but is also reflected in pollen data acquired from the high resolution analysis of a peat sequence covering the period 1945–1997, according to ²¹⁰Pb and ¹³⁷Cs dating. A possible inflation of the calculated PAR values due to discrepancies in the dating model is suspected and indirectly traced from the comparison of the Pinus mean PAR values for the most recent eight years of the monolith with those of a Tauber trap placed in the same mire. The presence of a high pollen producer such as pine enables the calculation of reliable PAR values, despite any discrepancies in the age-depth model. The Pinus PAR values “quantify” better the expansion of this timberline species, while pollen percentages reflect the same event in a “qualitative” way, i.e. as part of the general vegetation changes that take place in the area.     

13C natural abundance variations in carbonates and organic carbon from boreal forest wetlands

¹³C natural abundance variations were measured in peat soil and vegetation from two contrasting boreal forest wetlands: an upland watershed basin and a permanently saturated lowland mire. Evidence of methane oxidation was shown in the permanently saturated wetland with δ¹³C values as low as -97 ‰ in carbonate minerals found in floating peat mats. It is postulated that¹³C depleted CH₄ is oxidized in the mat and reacts with calcium ions to form calcite (identified through x-ray diffraction). Methane flux measurements during the summer of 1992 showed much lower fluxes in areas with floating peat mats relative to open water. Secondary carbonates in the basin peat have isotope compositions close to the δ¹³C values of the peat organic carbon (-25 ‰), indicating their origin from fermentation and possibly from sulfate-reduction. In the upland basin peat deposits, the δ¹³C_PDB values of organic C were constant with depth, while the permanently saturated mire had localities of¹³C enrichment in deeper layers of the peat. The¹³C enrichment may reflect areas of intense CH₄ production in which¹³C enriched residual substrate is left behind during the production of highly¹³C depleted CH₄.     

Changes of methane and nitrous oxide emissions in a transition bog in central Germany (German National Park Harz Mountains) after rewetting

During the last decades, various renaturation programmes have been initialized to recover nutrient sink and ecological functions of peatlands by rewetting. Rewetting, however, often results in the formation of hotspots for methane (CH₄) emissions and in temporal dieback of local vegetation. The present study aimed at quantifying changes of CH₄ and nitrous oxide (N₂O) emissions in a peatland currently under continuous rewetting conditions. Emissions where studied at a permanently flooded site and a non-flooded peat site with fluctuating water tables by using common closed chamber method. The permanently flooded site revealed extremely high CH₄ emissions (up to 1195 mg C m^?2 d^?1) which were positively correlated with temperature, nutrient content, dissolved organic carbon and nitrogen concentration of the peat soil water. In contrast, the non-flooded peat site, with lower and fluctuating water tables (WT), showed significantly lower CH₄ emissions and an increasing trend of CH₄ release associated with a generally increasing WT caused by the progressing rewetting process. Lower N₂O emissions (<24 µg N m^?2 d^?1) were observed at the flooded site. By contrast, the non-flooded peat site with fluctuating WT showed significantly higher N₂O emissions (up to 4178 µg N m^?2 d^?1), in particular at high temperatures during summer time. The present results indicate that permanently flooded conditions during rewetting processes might cause higher CH₄ emissions compared to fluctuating WT which in contrast might enhance N₂O emissions. In total, however, no decreasing trend for CH₄ emissions throughout the five-year renaturation period could be found. At least for N₂O we observed a decreasing trend during rewetting.     

Organic acids enhance the uptake of lead by wheat roots

The uptake and bioavailability of lead (Pb) in soil–plant systems remain poorly understood. This study indicates that acetic and malic acids enhance the uptake of Pb by wheat (Triticum aestivum L.) roots under hydroponic conditions. The net concentration-dependent uptake influx of Pb in the presence and absence of organic acids was characterized by Michaelis–Menten type nonsaturating kinetic curves that could be resolved into linear and saturable components. Fitted maximum uptake rates (V _max) of the Michaelis–Menton saturable component in the presence of acetic and malic acids were, respectively, 2.45 and 1.63 times those of the control, while the Michaelis–Menten K _m values of 5.5, 3.7 and 2.2 μM, respectively, remained unchanged. Enhanced Pb uptake by organic acids was partially mediated by Ca²⁺ and K⁺ channels, and also depended upon the physiological function of the plasma membrane P-type ATPase. Uptake may have been further enhanced by an effectively thinner unstirred layer of Pb adjacent to the roots, leading to more rapid diffusion towards roots. X-ray absorption spectroscopic studies provided evidence that the coordination environment of Pb in wheat roots was similar to that of Pb(CH₃COO)₂·3H₂O in that one Pb atom was coordinated to four oxygen atoms via the carboxylate group.     

The influence of the diel activity pattern of the larvae of Sericostoma personatum (Kirby & Spence) (Trichoptera) on organic matter distribution in stream-bed sediments — a laboratory study

Diel patterns in mobility and feeding behaviour of the larvae of the stream-dwelling trichopteran Sericostoma personatum larvae were investigated. Larvae fed at night on coarse particulate organic matter (CPOM) at the sediment surface. In the daytime they rested a few cm below the sediment surface, during which time their defaecation activity effected a release of fine particulate organic matter (FPOM) into the sediment. The amount of faeces (mean particle size = 0.1 ± 0.044 mm, x ± SD, n = 500) introduced into the sediment by the larvae, evaluated in two experiments, was 0.4–0.56 mg day^–1. This amount did not differ significantly from the organic input resulting from bacterial activity (0.36–0.64 mg day^–1). The presence of S. personatum larvae increased the sediment organic content by 42.9 mg (75.8 %) and 59.8 mg (185.6%) AFDW per 16 cm³ sediment over a 90-day period, as compared with control systems containing no larvae.     

Development of photosynthetic apparatus and respiration in pea seedlings during greening as influenced by toxic concentration of lead

Detached leaves of 14 day-old dark-grown pea seedlings were immersed with their cut ends either in water (control) or in 20 mM Pb(NO₃)₂ solution. They were exposed to continuous illumination during 24 and 48 h. The formation of PSII primary photochemistry in thylakoids was determined in vivo by measuring changes in values of parameters of chlorophyll a fast fluorescence kinetics: Fo, Fm, Fv, Fv/Fm and t 1/2. The amount of lead accumulation in leaves, content of chlorophylls and carotenoids and rates of CO₂ uptake in light and evolution in darkness (Pn-net photosynthesis and DR - dark respiration respectively) were determined. It has been found that with the exception of Fo, values of Fv, Fm and Fv/Fm were reduced by Pb²⁺. The values of t 1/2 were significantly larger in Pb²⁺ treated leaves. Decrease in the chlorophyll a fluorescence parameters was paralleled with the strong inhibition by this metal the biosynthesis of chlorophyll a and b but less of the carotenoids. Pb²⁺ drastically reduced Pn but had a stimulatory action on DR after 24 h and small inhibition of DR after 48 h exposure of leaves to this metal. As a consequence, after 48 h of greening the ratio of DR/Pn of control leaves was 0.45 whereas in Pb²⁺ treated leaves 2.7. It is proposed that DR in leaves plays a protective role against damage of Pn by Pb²⁺. Protection can be due to the supply the respiratory derived reductant and ATP to carry out cell metabolism upon reduced photosynthesis.     

Plutonium,241Am,90sr,and137cs concentrations in some antarctic matrices

A radioecological survey in Antarctica shows that the^239+240Pu,²³⁸Pu,²⁴¹Am,⁹⁰Sr, and¹³⁷Cs activities were detectable in nearly all the samples. The activity level of^239+240Pu,²⁴¹Am, and¹³⁷Cs in antarctic sediments was about 5–20 times lower than in the northern Adriatic Sea sediments, but the²³⁸Pu activities were relatively high. It was interesting to note that the⁹⁰Sr concentrations in all the sediments tended to be low, which could be the result of the easier exchangeable behavior of⁹⁰Sr in water. High concentrations were detected in mosses and lichens and their activity levels were comparable to those in central Italy. The radionuclide ratio analyses show that the major part of^239+240Pu,²⁴¹Am,⁹⁰Sr, and¹³⁷Cs was a result of nuclear weapon tests. The higher²⁴¹Am/^239+240Pu ratio was observed and it could perhaps be the result of fallout of nuclear weapon tests prior to 1962. The²³⁸Pu/^239+240Pu ratio in the antarctic matrices was about seven times higher than in the Northern hemisphere and it could be inferred that the major part of²³⁸Pu was originating from the SNAP-9A satellite accident.     

Properties of polyphosphatase ofAcinetobacter johnsonii 210A

Polyphosphatase, an enzyme which hydrolyses highly polymeric polyphosphates to P_i, was purified 77-fold fromAcinetobacter johnsonii 210A by Q-Sepharose, hydroxylapatite and Mono-Q column chromatography. The native molecular mass estimated by gel filtration and native gel electrophoresis was 55 kDa. SDS-polyacrylamide gel electrophoresis indicated that polyphosphatase ofAcinetobacter johnsonii 210A is a monomer. The enzyme was specific for highly polymeric polyphosphates and showed no activity towards pyrophosphate and organic phosphate esters. The enzyme was inhibited by iodoacetamide and in the presence of 10 mM Mg²⁺ by pyro- and triphosphate. The apparent K_m-value for polyphosphate with an average chain length of 64 residues was 5.9 µM and for tetraphosphate 1.2 mM. Polyphosphate chains were degraded to short chain polymers by a processive mechanism. Polyphosphatase activity was maximal in the presence of Mg²⁺ and K⁺.     

Adsorption of lead(II) from aqueous solution onto Hydrilla verticillata

The adsorption of Pb(II) onto Hydrilla verticillata was examined in aqueous solution with parameters of pH, adsorbent dosage, contact time and temperature. The linear Langmuir and Freundlich models were applied to describe equilibrium isotherms, and both models fitted well. The monolayer adsorption capacity of Pb(II) was found as 104.2 mg/g at pH 4 and 25°C. Dubinin–Radushkevich (D–R) isotherm model was also applied to the equilibrium data. The mean free energy of adsorption (15.81 kJ/mol) indicated that the adsorption of Pb(II) onto H. verticillata may be carried out via chemical ion-exchange mechanism. Thermodynamic parameters, free energy (ΔG ⁰), enthalpy (ΔH ⁰) and entropy (ΔS ⁰) of adsorption were also calculated. These parameters showed that the adsorption of Pb(II) onto H. verticillata was a feasible, spontaneous and exothermic process in nature. The influence of Cd²⁺, Cu²⁺ and Ni²⁺ on adsorption of Pb²⁺ onto H. verticillata was studied, too. In the investigated range of operating conditions, it was found that the existence of Cd ²⁺, Cu ²⁺ and Ni ²⁺ had no impact on the adsorption of Pb²⁺.     

Fate of urine nitrogen on mineral and peat soils in New Zealand

A field lysimeter experiment was conducted over 150 days to examine the fate of synthetic urinary nitrogen (N) applied to peat and mineral soils, with and without a water table. At the start of the winter season, synthetic urine labelled with ¹⁵N, was applied at 500 kg N ha^–1. Plant uptake, leaching losses and nitrous oxide (N₂O) fluxes were monitored. Total plant uptake ranged from 11% to 35% of the urine-N applied depending on soil type and treatment. Plant uptake of applied N was greater in the presence of a water table in the mineral soil. Nitrate-N (NO₃ ^--N) was only detected in leachates from the mineral soil, at concentrations up to 146 g NO₃ ^--N mL^–1. Presence of a water table in the mineral soil reduced leaching losses (as inorganic-N) from 47% to 6%, incrased plant uptake and doubled apparent denitrification losses. In the peat soils leaching losses of applied urine-N as inorganic-N were low (<5%). Losses of N as N₂O were greater in the mineral soil than in the peat soils, with losses of 3% and <1% of N applied respectively after 100 days. Apparent denitrification losses far exceeded N₂O losses and it is postulated that the difference could be due to dinitrogen (N₂) loss and soil entrapment of N₂.     

Vernal sedimentation trends in north Norwegian fjords: temporary anomaly in 234Th particulate fluxes related to Phaeocystis pouchetii proliferation

We report data of a naturally occurring radionuclide, ²³⁴Th, an in situ tracer, to investigate vertical export of biogenic matter during a vernal bloom of Phaeocystis pouchetii in the fjords of northern Norway. To optimise sampling of different stages of the bloom, three fjords with increasing oceanic influence (Balsfjord, Malangen fjord and Ullsfjord, respectively) were investigated in April 1997. Contrasting situations were encountered between the three fjords: the proliferation of P. pouchetii in Ullsfjord surface waters coincided with a drastic reduction of particulate ²³⁴Th fluxes in traps, although particulate organic carbon (POC) and dimethylsulphoniopropionate (DMSP) were exported and ²³⁴Th was available in surface waters. When large colonies make up a significant fraction of the vertical flux, as observed in Ullsfjord in April 1997, there may be a large and rapid change in the POC/²³⁴Th ratio, further complicating the use of ²³⁴Th as a tracer for POC export. The results suggest that the proliferation of Phaeocystis pouchetii during vernal bloom could temporary increase OC/²³⁴Th ratio of particles and delay the particulate export of ²³⁴Th, and probably of other particle-reactive species, from surface waters.