Peat multi-proxy data from Mannikjarve bog as indicators of late Holocene climate changes in Estonia

As part of a wider project on European climate change over the past 4500 years, a 4.5-m peat core was taken from a lawn microform on Mannikjarve bog, Estonia. Several methods were used to yield proxy-climate data: (i) a quadrat and leaf-count method for plant macrofossil data, (ii) testate amoebae analysis, and (iii) colorimetric determination of peat humification. These data are provided with an exceptionally high resolution and precise chronology. Changes in bog surface wetness were inferred using Detrended Correspondence Analysis (DCA) and zonation of macrofossil data, particularly concerning the occurrence of Sphagnum balticum, and a transfer function for water-table depth for testate amoebae data. Based on the results, periods of high bog surface wetness appear to have occurred at c. 3100, 3010-2990, 2300, 1750-1610, 1510, 14 10, 1110, 540 and 3 10 cal. yr BP, during four longer periods between c. 3170 and 2850 cal. yr BP, 2450 and 2000 cal. yr BP, 1770 and 1530 cal. yr BP and in the period from 880 cal. yr BP until the present. In the period between 1770 and 1530 cal. yr BP. the extension or initiation of a hollow microtope occurred, which corresponds with other research results from Mannikjarve bog. This and other changes towards increasing bog surface wetness may be the responses to colder temperatures and the predominance of a more continental climate in the region, which favoured the development of bog microdepressions and a complex bog microtopography. Located in the border zone of oceanic and continental climatic sectors, in an area almost without land uplift, this study site may provide valuable information about changes in palaeohydrological and palaeoclimatological conditions in the northern parts of the eastern Baltic Sea region.

Carbon accumulation in peatlands of West Siberia over the last 2000 years

We use a network of cores from 77 peatland sites to determine controls on peat C content and peat C accumulation over the last 2000 years (since 2 ka) across Russia's West Siberian Lowland (WSL), the world's largest wetland region. Our results show a significant influence of fossil plant composition on peat C content, with peats dominated by Sphagnum having a lower C content. Radiocarbon-derived C accumulation since 2 ka at 23 sites is highly variable from site to site, but displays a significant N–S trend of decreasing accumulation at higher latitudes. Northern WSL peatlands show relatively small C accumulation of 7 to 35 kg C m-2 since 2 ka. In contrast, peatlands south of 60°N show larger accumulation of 42 to 88 kg C m-2. Carbon accumulation since 2 ka varies significantly with modern mean annual air temperature, with maximum C accumulation found between -1 and 0°C. Rates of apparent C accumulation since 2 ka show no significant relationship to long-term Holocene averages based on total C accumulation. A GIS-based extrapolation of our site data suggests that a substantial amount (~40%) of total WSL peat C has accumulated since 2 ka, with much of this accumulation south of 60°N. The large peatlands in the southern WSL may be an important component of the Eurasian terrestrial C sink, and future warming could result in a shift northward in long-term WSL C sequestration.

Testate amoebae as indicators of hydroseral change: an 8,500 year record from Mer Bleue Bog, eastern Ontario, Canada.

Testate amoebae have been used widely as a proxy of hydrological change in ombrotrophic peatlands, although their response to abiotic controls in other types of mire and fenland palaeo-environments is less well understood. This paper examines the response of testate amoebae to hydroseral and other environmental changes at Mer Bleue Bog, Ontario, Canada, a large ombrotrophic peatland, which evolved from a brackish-water embayment in the early Holocene. Sediments, plant macrofossils and diatoms examined from a 5.99 m core collected from the dome of the bog record six stages of development: i) a quiet, brackish-water riverine phase (prior to ca. 8500 cal BP); ii) a shallow lake (ca. 8500–8200 cal BP); iii) fen (8200–7600 cal BP); iv) transitional mire (7600–6900 cal BP); v) pioneer raised mire (6900–4450 cal BP); and vi) ombrotrophic bog (4450 cal BP-present).

Testate amoebae, notably small (<25 µm diameter) specimens of Centropyxis aculeata type, first appear in low abundances in sediments ascribed to the lacustrine phase. Diatoms from the same horizons record a shallowing in water depth, a decline in salinity and the development of emergent macrophytic vegetation, which may have provided favourable conditions for testate amoeba colonization. The testate amoeba communities of the inferred fen phase are more diverse and include centropyxids, cyclopyxids, Arcellidae and Hyalospheniidae, although the assemblages show some differences to those recently reported in modern European fen environments. The Fen–Bog Transition (FBT) is also dominated by C. aculeata type. The change in testate amoeba communities around this key transition is apparent in the results of Detrended Correspondence Analysis (DCA), and appears to reflect a latent nutrient gradient and a secondary moisture gradient. DCA analyses of plant macrofossil remains around the FBT show a similar trend, although the sensitivity of the two proxies to the inferred environmental changes differs. Comparisons with other regional mid-Holocene peatland records confirm the important influence of reduced effective precipitation on the testate amoeba communities during the initiation and development of Sphagnum-dominated, raised bog communities.

A millennial record of environmental change in peat deposits from the Misten bog (East Belgium)

In this study, palaeoenvironmental changes recorded in the top metre of a peat profile (Misten bog, East Belgium) were investigated using a multiproxy approach. Proxies include bulk density, Ti and Si content, pollen, macrofossils, d13C on specific Sphagnum stems, and d13C–d18O on Sphagnum leaves. A high-resolution chronology was generated using 210Pb measurements and 22 14C AMS dates on carefully selected Sphagnum macrofossils. d13C only records large change in mire surface wetness. This is partly due to the fact that the core was taken from the edge of a hummock, which may make it difficult to track small isotopic changes. The d13C signal seems to be dependent upon the Sphagnum species composition. For example, a change between Sphagnum section Cuspidata towards Sphagnum imbricatum causes a significant drop in the d13C values. On the whole, the C and O isotopes record two shallow pool phases during the 8th–9th and the 13th centuries. Pollen and atmospheric soil dust (ASD) fluxes records increased human occupation in the area. There may be some climatic signals in the ASD flux, but they are difficult to decipher from the increasing human impact (land clearance, agriculture) during the last millennium. The variations in the proxies are not always synchronous, suggesting different triggering factors (temperature, wetness, windiness) for each proxy. This study also emphasizes that, compared to studies dealing with pollution using geochemical proxies, palaeoclimatic inferences from peat bogs need as many proxies as possible, together with highly accurate and precise age-models, in order to better understand climate variability and their consequences during the Holocene.

Ecology of testate amoebae in an Amazonian peatland and development of a transfer function for palaeohydrological reconstruction

Tropical peatlands represent globally important carbon sinks with a unique biodiversity and are currently threatened by climate change and human activities. It is now imperative that proxy methods are developed to understand the ecohydrological dynamics of these systems and for testing peatland development models. Testate amoebae have been used as environmental indicators in ecological and palaeoecological studies of peatlands, primarily in ombrotrophic Sphagnum-dominated peatlands in the mid- and high-latitudes. We present the first ecological analysis of testate amoebae in a tropical peatland, a nutrient-poor domed bog in western (Peruvian) Amazonia. Litter samples were collected from different hydrological microforms (hummock to pool) along a transect from the edge to the interior of the peatland. We recorded 47 taxa from 21 genera. The most common taxa are Cryptodifflugia oviformis, Euglypha rotunda type, Phryganella acropodia, Pseudodifflugia fulva type and Trinema lineare. One species found only in the southern hemisphere, Argynnia spicata, is present. Arcella spp., Centropyxis aculeata and Lesqueresia spiralis are indicators of pools containing standing water. Canonical correspondence analysis and non-metric multidimensional scaling illustrate that water table depth is a significant control on the distribution of testate amoebae, similar to the results from mid- and high-latitude peatlands. A transfer function model for water table based on weighted averaging partial least-squares (WAPLS) regression is presented and performs well under cross-validation (r 2apparent=0.76,RMSE=4.29;r2jack=0.68,RMSEP=5.18. The transfer function was applied to a 1-m peat core, and sample-specific reconstruction errors were generated using bootstrapping. The reconstruction generally suggests near-surface water tables over the last 3,000 years, with a shift to drier conditions at c. cal. 1218-1273 AD

Compostagem e caracterização de resíduos vegetais para utilização como substratos hortícolas

O objectivo deste trabalho foi estudar a utilização de 5 compostos de resíduos de origem vegetal, como componentes de substratos hortícolas. Estudaram-se os processos de compostagem de bagaço de azeitona, bagaço de uva, polpa de alfarroba, casca de eucalipto e casca de pinheiro, caracterizaram-se os compostos obtidos e testou-se a sua aptidão agronómica, como substratos para viveiro de tomate (Lycopersicum esculentum Mill.) em placas alveoladas e cultura de pelargónio (Pelargonium x hortorum) em vaso. Após uma preparação prévia, que em alguns dos resíduos vegetais constou de moenda, suplemento de azoto e aumento do teor de humidade, efectuou-se a sua compostagem em caixas com 1200 L de capacidade, isoladas termicamente, com arejamento por volteio manual. Depois foram analisadas as suas características físicas e químicas e testados na sua aptidão como constituintes únicos de substratos e em misturas com turfa de sphagnum. A maioria dos processos de compostagem apresentou uma evolução habitual da temperatura, com a máxima aproximando-se ou ultrapassando 60 oC. Como excepções, verificou-se um período de compostagem muito longo em bagaço de azeitona; o atraso da fase termofílica em polpa de alfarroba e, na 1ª compostagem de casca de pinheiro, a temperatura não alcançou a zona termofílica. A maioria dos resíduos manifestaram uma acentuada resistência à degradação durante a compostagem, à excepção da polpa de alfarroba e da casca de eucalipto. Contudo, a nível físico-químico e químico registaram-se evoluções acentuadas, sobretudo nas variáveis relacionadas com alterações da superfície das partículas, como por exemplo, a capacidade de troca catiónica. Outras variáveis apresentaram uma evolução interessante para o acompanhamento do processo e o conhecimento do grau de estabilidade do composto final. Foi apreciável o efeito proporcionado pela adição de lamas de estação de tratamento de águas residuais urbanas, como suplemento azotado, a nível das propriedades físicas dos compostos, do aumento da velocidade do processo de compostagem e do enriquecimento dos compostos em macro e micronutrientes. A compostagem não conduziu à melhoria significativa das propriedades físicas dos materiais, excepto em casca de eucalipto. Os compostos caracterizaram-se fundamentalmente por uma reduzida capacidade de retenção de água e uma elevada capacidade de arejamento. Os compostos obtidos com incorporação de lamas apresentaram os valores mais baixos de capacidade de arejamento, mesmo assim dentro dos limites satisfatórios e, os valores mais altos de capacidade de retenção de água. Na cultura em placas alveoladas, o comportamento de muitas das misturas com compostos não se diferenciou do da testemunha, observando-se uma flutuação sazonal do comportamento das misturas nos dois viveiros de cada ano, associada às condições ambientais mais exigentes do ponto de vista da disponibilidade de água. Observou-se um maior número de correlações significativas entre as características dos substratos e as variáveis relativas ao crescimento das plantas nos viveiros efectuados mais tarde, sob condições de maior evapotranspiração. As plantas obtidas no segundo viveiro de tomate foram instaladas em cultura. As características das plantas do viveiro, apresentaram elevada correlação com as respectivas produções obtidas no campo, evidenciando a importância da qualidade das plantas de viveiro, na produção. Nos ensaios de pelargónio em vaso, também se observaram comportamentos idênticos ao da testemunha em muitas das misturas com compostos. Observou-se no 2º ensaio, um maior número de tratamentos com resultados idênticos aos da testemunha, resultante das condições de menor exigência hídrica, as quais fizeram sobressair menos as diferenças de propriedades físicas das misturas. Contudo, a diferença de crescimento obtido em algumas misturas, atribuiu-se também à interferência da continuidade capilar entre o vaso de papel com a estaca enraizada e a mistura em estudo. O trabalho presente mostrou que é possível obter compostos a partir de resíduos orgânicos, com boas características e a preço competitivo para utilização como substratos hortícolas. O processo de compostagem sendo um elemento chave, é fácil de controlar se houver uma regulação eficaz do arejamento e do teor de humidade durante o processo. Apesar de alguns resíduos, como a polpa de alfarroba, serem caros, se tomarmos em consideração o custo da sua eliminação, poderão conduzir a substratos comercialmente viáveis. Em condições ambientais que favoreçam uma maior evapotranspiração ou, em culturas com maior exigência hídrica, pode ser aconselhável a mistura dos compostos estudados com turfa de sphagnum pouco decomposta para melhorar a capacidade de retenção de água.

Platanthera blephariglottis : une espèce indicatrice de l’intégrité écologique des tourbières ombrotrophes au Québec

Ce mémoire visait à déterminer si la platanthère à gorge frangée (Platanthera blephariglottis var. blephariglottis), une orchidée, est une espèce indicatrice de l’intégrité écologique des tourbières ombrotrophes. Les indicateurs d’intégrité écologique sont des outils indispensables pour évaluer efficacement les composantes d’un écosystème. Les résultats indiquent que l’abondance de la platanthère est fortement liée à l’indice de qualité floristique (FQAI). Le FQAI est aussi un excellent prédicateur de la présence de l’espèce, avec un taux de succès à 87%. D’autre part, l’abondance de l’orchidée est négativement affectée par les activités anthropiques et la matrice environnante. D’un point de vue descriptif, les habitats renfermant une grande abondance d’orchidées sont caractérisés par une faible microtopographie de surface et un recouvrement important de bryophytes et d’éricacées de petite taille. Globalement, ce mémoire a montré que la platanthère renferme un potentiel pour être indicatrice de l’intégrité écologique des tourbières ombrotrophes au Québec.

Dynamique des communautés végétales et impacts des perturbations humaines sur la végétation des tourbières.

Ce mémoire visait à comprendre la dynamique temporelle et les patrons floristiques actuels de deux tourbières du sud-ouest du Québec (Small et Large Tea Field) et à identifier les facteurs anthropiques, environnementaux et spatiaux sous-jacents. Pour répondre aux objectifs, des inventaires floristiques anciens (1985) ont d’abord été comparés à des inventaires récents (2012) puis les patrons actuels et les facteurs sous-jacents ont été identifiés à l’aide d’analyses multi-variables. Mes résultats montrent d’abord qu’un boisement important s’est produit au cours des 30 dernières années dans les tourbières à l’étude, probablement en lien avec le drainage des terres agricoles avoisinantes, diminuant la hauteur de la nappe phréatique. Simultanément, les sphaignes ont proliférées dans le centre des sites s’expliquant par une recolonisation des secteurs ayant brûlés en 1983. D’autre part, mes analyses ont montré que les patrons floristiques actuels étaient surtout liés aux variables environnementales (pH et conductivité de l’eau, épaisseur des dépôts), bien que la variance associée aux activités humaines était aussi significative, notamment dans la tourbière Large (18.6%). Les patrons floristiques ainsi que les variables environnementales et anthropiques explicatives étaient aussi fortement structurés dans l’espace, notamment selon un gradient bordure-centre. Enfin, la diversité béta actuelle était surtout liée à la présence d’espèces non-tourbicoles ou exotiques. Globalement, cette étude a montré que les perturbations humaines passées et actuelles avaient un impact important sur la dynamique et la distribution de la végétation des tourbières Small et Large Tea Field.

Dynamique végétale récente du complexe tourbeux des Tourbières-de-Lanoraie (Québec).

Les milieux humides sont parmi les écosystèmes les plus menacés de la planète que ce soit par le drainage, l’exploitation des ressources naturelles ou les changements climatiques. Dans une optique de conservation, il est primordial de comprendre la part des facteurs autogènes et allogènes dans la dynamique temporelle de ces écosystèmes. Dans ce contexte, les objectifs de cette étude étaient de : 1) reconstituer la dynamique des communautés végétales de deux secteurs ombrotrophes du complexe de milieux humides des Tourbières-de-Lanoraie au cours des trois derniers millénaires et 2) déterminer l’impact des activités humaines depuis les 500 dernières années sur cette dynamique. Pour ce faire, une approche paléoécologique pluridisciplinaire a été utilisée. La dynamique végétale a été semblable dans les deux secteurs étudiés. Elle a d’abord été caractérisée par une ombrotrophication des systèmes tourbeux puis par une transformation graduelle d’une tourbière ombrotrophe ouverte, dominées par les sphaignes et les éricacées, vers des tourbières ombrotrophes forestières. L’ombrotrophication se serait amorcée peu avant le Petit-Âge glaciaire (1570-1850 AD), période associée à des conditions plus fraiches et plus sèches. Le développement de la phase forestière serait beaucoup plus récent (début 1900) et semble être associé à une période d’intensification de l’empreinte anthropique dans le paysage, notamment du drainage. Ce travail montre que les perturbations anthropiques constituent depuis le début du XXème siècle le moteur principal de la dynamique de la végétation des deux secteurs étudiés.

Effect of drainage and wildfire on peat hydrophysical properties

Consecutive multiple disturbances to northern peatlands can dramatically impact peat hydrophysical properties. We examine the impact of a double disturbance (drainage and wildfire) on the hydrophysical and moisture retention properties of peat, a key regulator of peatland ecohydrological resilience, and compare this with the impact to each individual disturbance (drainage and wildfire). The compound effect of drainage and wildfire resulted in a shift of the surface datum down the peat profile, revealing denser peat. Less-dense near-surface peats that regulate water-table position and near-surface moisture content, both favourable to Sphagnum recolonization, were lost. At a drained peatland that was then subject to wildfire, peat bulk density increased by 14.1%, von Post humification class increased by two categories and water retention increased by 15.6%, compared with an adjacent burned but undrained (single disturbance) portion of the fen. We discuss the key hydrophysical metrics of peatland vulnerability and outline how they are affected by the isolated impacts of drainage and wildfire, as well as their combined effects. We demonstrate that multiple peatland disturbances have likely led to an increase in hydrological limitations to Sphagnum recovery, which may impact peatland ecohydrological resilience.

Simulated climate change impact on summer dissolved organic carbon release from peat and surface vegetation: implications for drinking water treatment

Uncertainty regarding changes in dissolved organic carbon (DOC) quantity and quality has created interest in managing peatlands for their ecosystem services such as drinking water provision. The evidence base for such interventions is, however, sometimes contradictory. We performed a laboratory climate manipulation using a factorial design on two dominant peatland vegetation types (Calluna vulgaris and Sphagnum Spp.) and a peat soil collected from a drinking water catchment in Exmoor National Park, UK. Temperature and rainfall were set to represent baseline and future conditions under the UKCP09 2080s high emissions scenario for July and August. DOC leachate then underwent standard water treatment of coagulation/flocculation before chlorination. C. vulgaris leached more DOC than Sphagnum Spp. (7.17 versus 3.00 mg g−1) with higher specific ultraviolet (SUVA) values and a greater sensitivity to climate, leaching more DOC under simulated future conditions. The peat soil leached less DOC (0.37 mg g−1) than the vegetation and was less sensitive to climate. Differences in coagulation removal efficiency between the DOC sources appears to be driven by relative solubilisation of protein-like DOC, observed through the fluorescence peak C/T. Post-coagulation only differences between vegetation types were detected for the regulated disinfection by-products (DBPs), suggesting climate change influence at this scale can be removed via coagulation. Our results suggest current biodiversity restoration programmes to encourage Sphagnum Spp. will result in lower DOC concentrations and SUVA values, particularly with warmer and drier summers.

First evidence of insect attraction by a Southern Hemisphere Splachnaceae: The case of Tayloria dubyi Broth. in the Reserve Biosphere Cape Horn, Chile

The moss Tayloria dubyi (Splachnaceae) is endemic to the subantarctic Magallanes ecoregion where it grows exclusively on bird dung and perhaps only on feces of the goose Chloephaga picta, a unique habitat among Splachnaceae. Some species of Splachnaceae from the Northern Hemisphere are known to recruit coprophilous flies as a vector to disperse their spores by releasing intense odors mimicking fresh clung or decaying corpses. The flies land on the capsule, and may get in contact with the protruding mass of spores that stick to the insect body. The dispersal strategy relies on the spores falling off when the insect reaches fresh droppings or carrion. Germination is thought to be rapid and a new population is quickly established over the entire substrate. The objectives of this investigation were to determine whether the coprophilous T. dubyi attracts flies and to assess the taxonomic diversity of the flies visiting this moss. For this, fly traps were set up above mature sporophyte bearing populations in two peatlands on Navarino Island. We captured 64 flies belonging to the Muscidae (Palpibracus chilensis), Tachinidae (Dasyuromyia sp) and Sarcophagidae (not identified to species) above sporophytes of T. dubyi, whereas no flies were captured in control traps set up above Sphagnum mats nearby.

Interferência da palhada de capim-braquiária, sobre o crescimento inicial de eucalipto

O presente trabalho foi conduzido com o objetivo de avaliar os possíveis efeitos da interferência, particularmente a alelopática, da palhada de Brachiaria decumbens (BRADC), resultante de controle químico com glyphosate (1440 g e.a./ha), sobre o crescimento inicial de plantas de Eucalyptus grandis. Os tratamentos experimentais foram os seguintes: eucalipto convivendo com a BRADC até 230 dias após o transplante (D.A.T.); eucalipto convivendo com BRADC, mas sendo essa controlada aos 106 D.A.T. com capina manual ou com uso de glyphosate; eucalipto sem convivência com BRADC, mas com simulação dos controles aos 106 D.A.T.; eucalipto sem conviver com BRADC e recebendo a palhada da planta daninha obtida em área tratada com os dois métodos de controle, adotando como testemunha a cobertura com Sphagnum. Ao final do período experimental (230 D.A.T.) constatou-se que as plantas de eucalipto que cresceram em convivência com BRADC apresentaram reduções significativas na altura, diâmetro do caule, número de folhas e de ramos e área foliar quando comparadas com as plantas que cresceram nos recipientes que receberam a cobertura morta de BRADC, independente do método de controle empregado. Observou-se, que tanto o controle químico como a capina manual, não afetaram o crescimento inicial das plantas de eucalipto, independentemente da situação de convivência ou de simulação. Com base nesses resultados, pode-se concluir que o capim-braquiária, quando controlado quimicamente com glyphosate, não exerceu efeito sobre o crescimento inicial do eucalipto.

Efeitos de substratos e temperaturas na germinação de sementes de tamareira-anã (Phoenix roebelenii O'Brien)

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Influence of the substrate in germination of lychee seeds

A lichia é considerada em todo o mundo como a rainha das frutas, por sua aparência e sabor delicado. Atualmente, a cultura vem despertando interesse, principalmente no Estado de São Paulo, onde, em virtude dos problemas enfrentados pelos agricultores, destacando-se os de laranja e cana-de-açúcar, a procura por alternativas agrícolas vem se intensificando ainda mais. A propagação através de sementes não é recomendada comercialmente, pois as plantas de pé-franco são geneticamente muito desuniformes e apresentam período juvenil muito longo, demorando até 10 anos para entrar em produção; no entanto, a semente pode ser utilizada para a obtenção de porta-enxertos. Observou-se que a germinação de sementes de lichia ocorre rapidamente, reforçando a importância do uso de um substrato adequado. Pela análise dos resultados obtidos, verifica-se que o substrato que aparentemente permitiu as melhores combinações de água e disponibilidade de oxigênio para as sementes - casca de arroz carbonizada e areia lavada, foi o que proporcionou valores de germinação mais rápidos e mais altos.