Outputs from the team
* indicates publication from LowPerm sites
*Hodson et al., 2017. Climatically sensitive transfer of iron to maritime Antarctic ecosystems by surface runoff. Nature Communcations, DOI:10.1038/ncomms14499
Iron supplied by glacial weathering results in pronounced hotspots of biological production in an otherwise iron-limited Southern Ocean Ecosystem. However, glacial iron inputs are thought to be dominated by icebergs. Here we show that surface runoff from three island groups of the maritime Antarctic exports more filterable (<0.45 μm) iron (6–81 kg km−2 a−1) than icebergs (0.0–1.2 kg km−2 a−1). Glacier-fed streams also export more acid-soluble iron (27.0–18,500 kg km−2 a−1) associated with suspended sediment than icebergs (0–241 kg km−2 a−1). Significant fluxes of filterable and sediment-derived iron (1–10 Gg a−1 and 100–1,000 Gg a−1, respectively) are therefore likely to be delivered by runoff from the Antarctic continent. Although estuarine removal processes will greatly reduce their availability to coastal ecosystems, our results clearly indicate that riverine iron fluxes need to be accounted for as the volume of Antarctic melt increases in response to 21st century climate change.
*O'Neill et al., 2017. Near-surface ground ice variation in ice-wedge polygons in Adventdalen, Svalbard. Arctic Science Summit Week 2017 (Poster), Prague, Czech Republic
Near-surface ground ice is a characteristic feature of permafrsot, and its thaw may lead to ground subsidence, which can damage infrastructure and change landscape hydrology and ecology. The thaw of upper permafrost also mobilizes previously-frozen organic carbon. Little data exist on the distribution of ground ice in the top of permafrost in the high Arcitc archipelago of Svalbard. Polygonal terrain is widely distibuted on Svalbard, and hosts both wedge ice and segregated ice in fine-grained sediment. Here we present early results from part of the LowPerm project, which broadly seeks to understand nutrient transport in permafrost landscapes that may lead to changes in GHG produciton and fertilization of the Arctic Ocean.
*Bak et al., 2017. Electron acceptor-based regulation of microbial greenhouse gas production from thawing permafrost. EGU 2017 (Poster), Vienna, Austria
Permafrost contains about 35% of the global soil organic carbon (0-3 m depth). As a consequence of global warming, the active layer thickness is steadily increasing and its organic carbon is becoming available for degradation, causing a concomitant release of CO2 and CH4. The climate forcing feedbacks of permafrost thaw are determined by the rate of organic carbon degradation and to which degree it is released as CO2 or CH4. Methane is produced under anoxic conditions, but the factors that regulate its production are poorly constrained.
*Jones et al., 2017. Redox and biogeochemical processes inferred from permafrost porewater extractions. EGU 2017 (Poster), Vienna, Austria
Climate change is causing permafrost to thaw in the Arctic coastal lowlands. The resulting release of stored organic carbon and nutrients leads to increased greenhouse gas (GHG) emissions in Arctic wetlands.
• In Svalbard (fig. 1), isostatic rebound during the last 10,000 years has created coastal wetlands by exposing more land area.
• The redox evolution of these wetlands influences methane release, as methanogenesis occurs once alternative electron acceptors for the microbial oxidation of organic matter have been depleted.
• It is crucial to understand the redox evolution of these environments in order to accurately predict the timing and magnitude of methane release.
*Hodson et al., 2015. Glacial and periglacial floodplain sediments regulate hydrologic transfer of reactive iron to a high arctic fjord. Hydrological Processes, DOI: 10.1002/hyp.10701
The transport of reactive iron (i.e. colloidal and dissolved) by a glacier-fed stream system draining a high relief periglacial landscape in the high Arctic archipelago of Svalbard is described. A negative, non-linear relationship between discharge and iron concentration is found, indicative of increased iron acquisition along baseflow pathways. Because the glaciers are cold-based and there are no intra- or sub-permafrost groundwater springs, baseflow is principally supplied by the active layer and the colluvial and alluvial sediments in the lower valley. Collectively, these environments increase the flux of iron in the stream by 40% over a floodplain length of just 8 km, resulting in 6 kg Fe km2a1 of reactive iron export for a 20% glacierized watershed. We show that pyrite oxidation in shallow-groundwater flowpaths of the floodplain is the most important source of reactive iron, although it is far less influential in the upper parts of the catchment where other sources are significant (including ironstone and secondary oxide coatings). Microbial catalysis of the pyrite oxidation occurs in the floodplain, enabling rapid, hyporheic water exchange to enhance the iron fluxes at high discharge and cause the non-linear relationship between discharge and reactive iron concentrations. Furthermore, because the pyrite oxidation is tightly coupled to carbonate and silicate mineral weathering, other nutrients such as base cations and silica are also released to the stream system. Our work therefore shows that high Arctic floodplains should be regarded as critically important regulators of terrestrial nutrient fluxes to coastal ecosystems from glacial and periglacial sources.
*Mallon et al., 2015. LowPerm: quantifying thaw-driven biogas production and nutrient export from Eurasian Arctic lowlands. Arctic Science Conference 2015 (Poster), Sheffield, UK
The surface energy budget of coastal lowlands in the Eurasian Arctic is very sensitive to atmospheric and oceanic warming, prompting the early onset of permafrost thaw, increased active layer thickness, and enhanced microbial metabolism. Although Arctic permafrost holds vast amounts of carbon, we still lack the tools to accurately forecast how changes in these processes influence permafrost biogeochemistry and feedback to climate change. Here we present early progress from the LowPerm project and describe a key site established in an ice-wedged polygonal landscape in Adventdalen, Svalbard. The environmental history of the site is explained and in situ data describing the hydrological and biogeochemical conditions during active layer development in 2015 are shown.
Nowak et al., 2015. On the biogeochemical response of a glacierized High Arctic watershed to climate change: revealing patterns, processes and heterogeneity among micro-catchments. Hydrological Processes, 29, 1588-1603
Our novel study examines landscape biogeochemical evolution following deglaciation and permafrost change in Svalbard by looking at the productivity of various micro-catchments existing within one watershed. It also sheds light on how moraine, talus and soil environments contribute to solute export from the entire watershed into the downstream marine ecosystem. We find that solute dynamics in different micro-catchments are sensitive to abiotic factors such as runoff volume, water temperature, geology, geomorphological controls upon hydrological flowpaths and landscape evolution following sea level and glacial changes. Biotic factors influence the anionic composition of runoff because of the importance of microbial SO42 and NO3 production. The legacy of glaciation and its impact upon sea level changes is shown to influence local hydrochemistry, allowing Cl to be used as a tracer of thawing permafrost that has marine origins. However, we show that a ‘glacial signal’ dominates solute export from the watershed. Therefore, although climatically driven change in the proglacial area has an influence on local ecosystems, the biogeochemical response of the entire watershed is dominated by glacially derived products of rapid chemical weathering. Consequently, only the study of micro-catchments existing within watersheds can uncover the landscape response to contemporary climate change.