W. Berry Lyons
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View article: The influence of plantation forest legacy on blanket bog hydrology
The influence of plantation forest legacy on blanket bog hydrology Open
View article: Irish surface water response to the 2018 drought
Irish surface water response to the 2018 drought Open
Intense weather events are projected to increase as a consequence of climate change. The summer 2018 drought in Europe impacted human health, ecosystems, and economic prosperity. Even locations with an abundance of fresh water, like Irelan…
View article: Nutrient concentrations and nitrogen speciation in tropical watersheds of central Panama
Nutrient concentrations and nitrogen speciation in tropical watersheds of central Panama Open
We present chemical analyses from rivers and streams in five partly to near-fully forested watersheds in the humid tropics of central Panama. Contrary to the situation observed for temperate watersheds in the Northern Hemisphere, the conce…
View article: Change at 85 degrees south: Shackleton Glacier region proglacial lakes from 1960 to 2020
Change at 85 degrees south: Shackleton Glacier region proglacial lakes from 1960 to 2020 Open
Over the last two decades, anomalous warming events have been observed in coastal Antarctic regions. While these events have been documented in the Ross Sea sector, the Antarctic interior is believed to have been buffered from warming. In …
View article: Grand Challenges in environmental geochemistry
Grand Challenges in environmental geochemistry Open
SPECIALTY GRAND CHALLENGE article Front. Geochem., 05 April 2023Sec. Environmental Geochemistry Volume 1 - 2023 | https://doi.org/10.3389/fgeoc.2023.1154473
View article: Strong Dispersal Limitation of Microbial Communities at Shackleton Glacier, Antarctica
Strong Dispersal Limitation of Microbial Communities at Shackleton Glacier, Antarctica Open
Because of their diversity and ubiquity, microbes provide an excellent means to tease apart how natural communities are structured. In general, ecologists believe that stochastic assembly processes, like random drift and dispersal, should …
View article: Biogeochemical and historical drivers of microbial community composition and structure in sediments from Mercer Subglacial Lake, West Antarctica
Biogeochemical and historical drivers of microbial community composition and structure in sediments from Mercer Subglacial Lake, West Antarctica Open
Ice streams that flow into Ross Ice Shelf are underlain by water-saturated sediments, a dynamic hydrological system, and subglacial lakes that intermittently discharge water downstream across grounding zones of West Antarctic Ice Sheet (WA…
View article: Isotopic signature of massive, buried ice in eastern Taylor Valley, Antarctica: Implications for its origin
Isotopic signature of massive, buried ice in eastern Taylor Valley, Antarctica: Implications for its origin Open
The coastal regions of the McMurdo Dry Valleys, Antarctica, contain deposits of the Ross Sea Drift, sedimentary material left from the Ross Sea ice sheet from the advance of the West Antarctic ice sheet during the Last Glacial Maximum. Muc…
View article: Elevational Constraints on the Composition and Genomic Attributes of Microbial Communities in Antarctic Soils
Elevational Constraints on the Composition and Genomic Attributes of Microbial Communities in Antarctic Soils Open
Antarctic soils represent an ideal system to study how environmental properties shape the taxonomic and functional diversity of microbial communities given the relatively low diversity of Antarctic soil microbial communities and the pronou…
View article: Barotropic seiches in a perennially <scp>ice‐covered</scp> lake, East Antarctica
Barotropic seiches in a perennially <span>ice‐covered</span> lake, East Antarctica Open
Water movement in ice‐covered lakes is known to be driven by wind, sediment heat flux, solar radiation, saline density flows, and advective stream discharge. In large ice‐covered lakes, wind‐induced oscillations have been found to play a m…
View article: Response of Antarctic soil fauna to climate‐driven changes since the Last Glacial Maximum
Response of Antarctic soil fauna to climate‐driven changes since the Last Glacial Maximum Open
Understanding how terrestrial biotic communities have responded to glacial recession since the Last Glacial Maximum (LGM) can inform present and future responses of biota to climate change. In Antarctica, the Transantarctic Mountains (TAM)…
View article: Relationship between meteoric <sup>10</sup> Be and NO <sub>3</sub> <sup>−</sup> concentrations in soils along Shackleton Glacier, Antarctica
Relationship between meteoric <sup>10</sup> Be and NO <sub>3</sub> <sup>−</sup> concentrations in soils along Shackleton Glacier, Antarctica Open
Outlet glaciers that flow through the Transantarctic Mountains (TAM) experienced changes in ice thickness greater than other coastal regions of Antarctica during glacial maxima. As a result, ice-free areas that are currently exposed may ha…
View article: The geochemistry of Irish rivers
The geochemistry of Irish rivers Open
Study region: Ireland Study focus: Multiple studies have established that catchment geology and weathering regime strongly influence surface water chemistry, and that geochemical cycling can vary due to seasonal climatic conditions. Howeve…
View article: Scientific access into Mercer Subglacial Lake: scientific objectives, drilling operations and initial observations
Scientific access into Mercer Subglacial Lake: scientific objectives, drilling operations and initial observations Open
The Subglacial Antarctic Lakes Scientific Access (SALSA) Project accessed Mercer Subglacial Lake using environmentally clean hot-water drilling to examine interactions among ice, water, sediment, rock, microbes and carbon reservoirs within…
View article: Exploring the Boundaries of Microbial Habitability in Soil
Exploring the Boundaries of Microbial Habitability in Soil Open
Microbes are widely assumed to be capable of colonizing even the most challenging terrestrial surface environments on Earth given enough time. We would not expect to find surface soils uninhabited by microbes as soils typically harbor dive…
View article: Geochemical zones and environmental gradients for soils from the central Transantarctic Mountains, Antarctica
Geochemical zones and environmental gradients for soils from the central Transantarctic Mountains, Antarctica Open
Previous studies have established links between biodiversity and soil geochemistry in the McMurdo Dry Valleys, Antarctica, where environmental gradients are important determinants of soil biodiversity. However, these gradients are not well…
View article: Enhanced trace element mobilization by Earth’s ice sheets
Enhanced trace element mobilization by Earth’s ice sheets Open
Significance Trace elements are integral to biogeochemical processes at the Earth’s surface and play an important role in the carbon cycle as micronutrients to support biological productivity. We present data from the Greenland and Antarct…
View article: Stable Isotopes of Nitrate, Sulfate, and Carbonate in Soils From the Transantarctic Mountains, Antarctica: A Record of Atmospheric Deposition and Chemical Weathering
Stable Isotopes of Nitrate, Sulfate, and Carbonate in Soils From the Transantarctic Mountains, Antarctica: A Record of Atmospheric Deposition and Chemical Weathering Open
Soils in ice-free areas in Antarctica are recognized for their high salt concentrations and persistent arid conditions. While previous studies have investigated the distribution of salts and potential sources in the McMurdo Dry Valleys, lo…
View article: Genetic diversity of soil invertebrates corroborates timing estimates for past collapses of the West Antarctic Ice Sheet
Genetic diversity of soil invertebrates corroborates timing estimates for past collapses of the West Antarctic Ice Sheet Open
Significance Changes in the extent of ice sheets through evolutionary timescales have influenced the connectivity of soil invertebrate populations across the Antarctic landscape. We use genetic divergences to estimate isolation times for s…
View article: Exploring the boundaries of microbial habitability in soil
Exploring the boundaries of microbial habitability in soil Open
Microbes are widely assumed to be capable of colonizing even the most challenging terrestrial surface environments on Earth given enough time. We would not expect to find surface soils uninhabited by microbes as soils typically harbor dive…
View article: Silicon Isotopic Composition of Dry and Wet-Based Glaciers in Antarctica
Silicon Isotopic Composition of Dry and Wet-Based Glaciers in Antarctica Open
Glaciers and ice sheets export significant amounts of silicon (Si) to downstream ecosystems, impacting local and potentially global biogeochemical cycles. Recent studies have shown Si in Arctic glacial meltwaters to have an isotopically di…
View article: Relative terrestrial exposure ages inferred from meteoric <sup>10</sup> Be and NO <sub>3</sub> <sup>−</sup> concentrations in soils along the Shackleton Glacier, Antarctica
Relative terrestrial exposure ages inferred from meteoric <sup>10</sup> Be and NO <sub>3</sub> <sup>−</sup> concentrations in soils along the Shackleton Glacier, Antarctica Open
Modeling studies and field mapping show that increases in ice thickness during glacial periods were not uniform across Antarctica. Rather, outlet glaciers that flow through the Transantarctic Mountains (TAM) experienced the greatest change…
View article: Silicon Isotopes Reveal a Non-glacial Source of Silicon to Crescent Stream, McMurdo Dry Valleys, Antarctica
Silicon Isotopes Reveal a Non-glacial Source of Silicon to Crescent Stream, McMurdo Dry Valleys, Antarctica Open
In high latitude environments, silicon is supplied to river waters by both glacial and nonglacial chemical weathering. The signal of these two end-members is often obscured by biological uptake and/or groundwater input in the river catchme…
View article: An Introduction to “Microbial Biogeochemistry: A Special Issue of Aquatic Geochemistry Honoring Mark Hines”
An Introduction to “Microbial Biogeochemistry: A Special Issue of Aquatic Geochemistry Honoring Mark Hines” Open
View article: Uranium in Ohio, USA Surface Waters: Implications for a Fertilizer Source in Waters Draining Agricultural lands
Uranium in Ohio, USA Surface Waters: Implications for a Fertilizer Source in Waters Draining Agricultural lands Open
Synthetic fertilizer is a potential source of uranium to natural waters, yet evidence is lacking. We analyzed dissolved uranium concentrations in lakes, reservoirs, and rivers in Ohio, USA during the summer of 2017. All water bodies drain …
View article: The hydrogeochemistry of shallow groundwater from Lut Desert, Iran: The hottest place on Earth
The hydrogeochemistry of shallow groundwater from Lut Desert, Iran: The hottest place on Earth Open
View article: Validation of sampling antarctic subglacial hypersaline waters with an electrothermal ice melting probe (IceMole) for environmental analytical geochemistry
Validation of sampling antarctic subglacial hypersaline waters with an electrothermal ice melting probe (IceMole) for environmental analytical geochemistry Open
Geochemical characterisation of hypersaline waters is difficult as high concentrations of salts hinder the analysis of constituents at low concentrations, such as trace metals, and the collection of samples for trace metal analysis in natu…
View article: The Hydroecology of an Ephemeral Wetland in the McMurdo Dry Valleys, Antarctica
The Hydroecology of an Ephemeral Wetland in the McMurdo Dry Valleys, Antarctica Open
The McMurdo Dry Valleys is a polar desert on the coast of East Antarctica where ephemeral wetlands become hydrologically active during warm and sunny summers when subsurface flows are generated from melting snowfields. To understand the st…
View article: Groundwater discharge to the western Antarctic coastal ocean
Groundwater discharge to the western Antarctic coastal ocean Open
Submarine groundwater discharge (SGD) measurements have been limited along the Antarctic coast, although groundwater discharge is becoming recognized as an important process in the Antarctic. Quantifying this meltwater path-way is importan…
View article: The Geochemistry of Englacial Brine From Taylor Glacier, Antarctica
The Geochemistry of Englacial Brine From Taylor Glacier, Antarctica Open
Blood Falls is a hypersaline, iron‐rich discharge at the terminus of the Taylor Glacier in the McMurdo Dry Valleys, Antarctica. In November 2014, brine in a conduit within the glacier was penetrated and sampled using clean‐entry techniques…