Carbon dioxide (CO), methane (CH), and nitrous oxide (NO) are the greenhouse gases largely responsible for anthropogenic climate change. Natural plant and microbial metabolic processes play a major role in the global atmospheric budget of each. We have been studying ecosystem-atmosphere trace gas exchange at a sub-boreal forest in the northeastern United States for over two decades. Historically our emphasis was on turbulent fluxes of CO and water vapor. In 2012 we embarked on an expanded campaign to also measure CH and NO. Here we present continuous tower-based measurements of the ecosystem-atmosphere exchange of CO and CH, recorded over the period 2012-2018 and reported at a 30-minute time step. Additionally, we describe a five-year (2012-2016) dataset of chamber-based measurements of soil fluxes of CO, CH, and NO (2013-2016 only), conducted each year from May to November. These data can be used for process studies, for biogeochemical and land surface model validation and benchmarking, and for regional-to-global upscaling and budgeting analyses.
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http://dx.doi.org/10.1038/s41597-019-0119-1 | DOI Listing |
Plants (Basel)
January 2023
Institute of Water and Ecology Problems FEB RAS, Khabarovsk Federal Research Center FEB RAS, 56 Dikopoltseva, 680000 Khabarovsk, Russia.
The study of the biodiversity of vegetation cover in the context of its genesis and development is an important task. The results of these studies are the basis for the development of ecological, biogeographical, evolutionary, and sociological research, such as modelling the dynamic processes of natural ecosystems, understanding the consequences of natural and anthropogenic changes for biodiversity, solving problems of biodiversity conservation, etc. Of particular interest from this point of view is the biodiversity of ecotones, which can serve as a model for studying the factors of the genesis of the plant cover structure in a dynamic environment.
View Article and Find Full Text PDFEnviron Sci Technol
December 2022
Department of Physical and Environmental Sciences, University of Toronto Scarborough, 1265 Military Trail, Scarborough, OntarioM1C 1A4, Canada.
Changes in sulfate (SO) deposition have been linked to changes in mercury (Hg) methylation in peatlands and water quality in freshwater catchments. There is little empirical evidence, however, of how quickly methyl-Hg (MeHg, a bioaccumulative neurotoxin) export from catchments might change with declining SO deposition. Here, we present responses in total Hg (THg), MeHg, total organic carbon, pH, and SO export from a peatland-dominated catchment as a function of changing SO deposition in a long-term (1998-2011), whole-ecosystem, control-impact experiment.
View Article and Find Full Text PDFPlant Soil
March 2022
Department of Forest and Conservation Sciences, Faculty of Forestry, The University of British Columbia, Vancouver, BC Canada.
Aims: Despite little soil development and organic matter accumulation, lodgepole pine () consistently shows vigorous growth on bare gravel substrate of aggregate mining pits in parts of Canadian sub-boreal forests. This study aimed to investigate the bacterial microbiome of lodgepole pine trees growing at an unreclaimed gravel pit in central British Columbia and suggest their potential role in tree growth and survival following mining activity.
Methods: We characterized the diversity, taxonomic composition, and relative abundance of bacterial communities in rhizosphere and endosphere niches of pine trees regenerating at the gravel pit along with comparing them with a nearby undisturbed forested site using 16S rRNA high-throughput sequencing.
Mol Ecol
November 2021
Département de Sciences Biologiques, Université de Montréal, Montréal, QC, Canada.
Periodic and spatially synchronous outbreaks of insect pests have dramatic consequences for boreal and sub-boreal forests. Within these multitrophic systems, parasitoids can be stabilizing agents by dispersing toward patches containing higher host density (the so-called birdfeeder effect). However, we know little about the dispersal abilities of parasitoids in continuous forested landscapes, limiting our understanding of the spatiotemporal dynamics of host-parasitoid systems, and constraining our ability to predict forest resilience in the context of global changes.
View Article and Find Full Text PDFAgric For Meteorol
January 2021
University of Minnesota - Dept. Soil, Water & Climate, St. Paul, MN, USA.
Eddy covariance (EC) measurements of ecosystem-atmosphere carbon dioxide (CO) exchange provide the most direct assessment of the terrestrial carbon cycle. Measurement biases for open-path (OP) CO concentration and flux measurements have been reported for over 30 years, but their origin and appropriate correction approach remain unresolved. Here, we quantify the impacts of OP biases on carbon and radiative forcing budgets for a sub-boreal wetland.
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