Newswise — A new study, using a first-of-its-kind approach to analyze satellite imagery from boreal forests over the last three decades, found that fire may be changing the face of the region in a way researchers did not previously anticipate.
Historically, fires in North American boreal forests have led to coniferous trees being supplanted by deciduous trees, which are faster growing, take up more carbon and reflect more light, leading to cooling of the climate and decreased likelihood of fire.
The study, led by Northern Arizona University and published today in Nature Climate Change, found that, surprisingly, while forests do become more deciduous, they don’t stay that way; a few decades later, the same forests gradually start to shift back toward coniferous trees. Researchers also found that the abrupt loss of coniferous forests caused by wildfire was offset by the gradual increase in coniferous forests in areas that had not recently burned, so there was no overall shift toward deciduous cover.
“We confirmed that fires clearly shift forests from conifer to deciduous cover, but when we look at those changes over many decades, we find deciduous trees begin to be replaced again by conifer trees three to four decades following fire,” said Scott Goetz, Regents’ professor in the School of Informatics, Computing, and Cyber Systems (SICCS) at Northern Arizona University and study co-author. “There are tremendous dynamics taking place, but when we tally those all up, the net feedbacks to climate were fairly small.”
“This was somewhat surprising because several recent studies suggested there were shifts toward deciduous forests at local to regional scales,” said Logan Berner, assistant research professor in SICCS and study co-author. “While our study indicates there have not been whole-sale shifts in forest composition during recent decades, we anticipate that continued climate warming and increased wildfire activity could lead to pronounced changes in forest composition over the coming decades.”
The researchers note this may not be permanent; recent decades have seen an uptick in fire disturbance in these forests, so in the future, the return to coniferous cover may take longer than it has in the past. As the climate continues to get warmer and drier, that also will affect how forests burn and how they recover.
“As we think about fire management approaches, including efforts to reduce carbon emissions and mitigate fire risk to local communities and infrastructure, this study provides a critical foundation for future research,” said Brendan Rogers, associate scientist at Woodwell Climate Research Center and study co-author. “Especially after a summer of record-breaking fires in Canada, understanding how the composition of these forests will shift and respond to fire over time is crucial to informing best management practices and protecting people and the planet.”
The team conducted the research as part of NASA’s Arctic Boreal Vulnerability Experiment (ABoVE), of which Goetz is the Science Team Lead. As part of their project within ABoVE, they used high-resolution satellite imagery of the boreal forests across Alaska and Canada captured by the Landsat series of satellites to quantify changes in forest composition, both in areas that have burned and those that haven’t. They also quantified the effects of changing forests using satellite measurements of surface reflectivity and calculated the feedback effects on climate.
The study was led by Richard Massey, a former postdoctoral scholar at Northern Arizona University, and co-authored by Goetz, Berner and Rogers, as well as Sol Cooperdock, research associate at Woodwell Climate; Michelle Mack, Regents’ professor in the Center for Ecosystem Science and Society (Ecoss) at NAU; and Xanthe Walker, assistant professor in NAU’s Ecoss.
Source: Northern Arizona University
Separating out signals recorded at the seafloor
Newswise — Blame it on plate tectonics. The deep ocean is never preserved, but instead is lost to time as the seafloor is subducted. Geologists are mostly left with shallower rocks from closer to the shoreline to inform their studies of Earth history.
“We have only a good record of the deep ocean for the last ~180 million years,” said David Fike, the Glassberg/Greensfelder Distinguished University Professor of Earth, Environmental, and Planetary Sciences in Arts & Sciences at Washington University in St. Louis. “Everything else is just shallow-water deposits. So it’s really important to understand the bias that might be present when we look at shallow-water deposits.”
One of the ways that scientists like Fike use deposits from the seafloor is to reconstruct timelines of past ecological and environmental change. Researchers are keenly interested in how and when oxygen began to build up in the oceans and atmosphere, making Earth more hospitable to life as we know it.
For decades they have relied on pyrite, the iron-sulfide mineral known as “fool’s gold,” as a sensitive recorder of conditions in the marine environment where it is formed. By measuring the bulk isotopic composition of sulfur in pyrite samples — the relative abundance of sulfur atoms with slightly different mass — scientists have tried to better understand ancient microbial activity and interpret global chemical cycles.
But the outlook for pyrite is not so shiny anymore. In a pair of companion papers published Nov. 24 in the journal Science, Fike and his collaborators show that variations in pyrite sulfur isotopes may not represent the global processes that have made them such popular targets of analysis.
Instead, Fike’s research demonstrates that pyritte responds predominantly to local processes that should not be taken as representative of the whole ocean. A new microanalysis approach developed at Washington University helped the researchers to separate out signals in pyrite that reveal the relative influence of microbes and that of local climate.
For the first study, Fike worked with Roger Bryant, who completed his graduate studies at Washington University, to examine the grain-level distribution of pyrite sulfur isotope compositions in a sample of recent glacial-interglacial sediments. They developed and used a cutting-edge analytical technique with the secondary-ion mass spectrometer (SIMS) in Fike’s laboratory.
“We analyzed every individual pyrite crystal that we could find and got isotopic values for each one,” Fike said. By considering the distribution of results from individual grains, rather than the average (or bulk) results, the scientists showed that it is possible to tease apart the role of the physical properties of the depositional environment, like the sedimentation rate and the porosity of the sediments, from the microbial activity in the seabed.
“We found that even when bulk pyrite sulfur isotopes changed a lot between glacials and interglacials, the minima of our single grain pyrite distributions remained broadly constant,” Bryant said. “This told us that microbial activity did not drive the changes in bulk pyrite sulfur isotopes and refuted one of our major hypotheses.”
“Using this framework, we’re able to go in and look at the separate roles of microbes and sediments in driving the signals,” Fike said. “That to me represents a huge step forward in being able to interpret what is recorded in these signals.”
In the second paper, led by Itay Halevy of the Weizmann Institute of Science and co-authored by Fike and Bryant, the scientists developed and explored a computer model of marine sediments, complete with mathematical representations of the microorganisms that degrade organic matter and turn sulfate into sulfide and the processes that trap that sulfide in pyrite.
“We found that variations in the isotopic composition of pyrite are mostly a function of the depositional environment in which the pyrite formed,” Halevy said. The new model shows that a range of parameters of the sedimentary environment affect the balance between sulfate and sulfide consumption and resupply, and that this balance is the major determinant of the sulfur isotope composition of pyrite.
“The rate of sediment deposition on the seafloor, the proportion of organic matter in that sediment, the proportion of reactive iron particles, the density of packing of the sediment as it settles to the seafloor — all of these properties affect the isotopic composition of pyrite in ways that we can now understand,” he said.
Importantly, none of these properties of the sedimentary environment are strongly linked to the global sulfur cycle, to the oxidation state of the global ocean, or essentially any other property that researchers have traditionally used pyrite sulfur isotopes to reconstruct, the scientists said.
“The really exciting aspect of this new work is that it gives us a predictive model for how we think other pyrite records should behave,” Fike said. “For example, if we can interpret other records — and better understand that they are driven by things like local changes in sedimentation, rather than global parameters about ocean oxygen state or microbial activity — then we can try to use this data to refine our understanding of sea level change in the past.”
Plastic-eating bacteria turn waste into useful starting materials for other products
Newswise — Mountains of used plastic bottles get thrown away every day, but microbes could potentially tackle this problem. Now, researchers in ACS Central Science report that they’ve developed a plastic-eating E. coli that can efficiently turn polyethylene terephthalate (PET) waste into adipic acid, which is used to make nylon materials, drugs and fragrances.
Previously, a team of researchers including Stephen Wallace engineered a strain of E. coli to transform the main component in old PET bottles, terephthalic acid, into something tastier and more valuable: the vanilla flavor compound vanillin. At the same time, other researchers engineered microbes to metabolize terephthalic acid into a variety of small molecules, including short acids. So, Wallace and a new team from the University of Edinburgh wanted to expand E. coli’s biosynthetic pathways to include the metabolism of terephthalic acid into adipic acid, a feedstock for many everyday products that’s typically generated from fossil fuels using energy-intensive processes.
The team developed a new E. coli strain that produced enzymes that could transform terephthalic acid into compounds such as muconic acid and adipic acid. Then, to transform the muconic acid into adipic acid, they used a second type of E. coli, which produced hydrogen gas, and a palladium catalyst. In experiments, the team found that attaching the engineered microbial cells to alginate hydrogel beads improved their efficiency, and up to 79% of the terephthalic acid was converted into adipic acid. Using real-world samples of terephthalic acid from a discarded bottle and a coating taken from waste packaging labels, the engineered E. coli system efficiently produced adipic acid. In the future, the researchers say they will look for pathways to biosynthesize additional higher-value products.
The authors acknowledge funding from the Carnegie Trust for the Universities of Scotland; the Industrial Biotechnology Innovation Centre; a Future Leaders Fellowship from UK Research and Innovation; and an Engineering and Physical Sciences Research Council Sustainable Manufacturing grant.
The paper’s abstract will be available on Nov. 1 at 8 a.m. Eastern time here: http://pubs.acs.org/doi/abs/10.1021/acscentsci.3c00414
The American Chemical Society (ACS) is a nonprofit organization chartered by the U.S. Congress. ACS’ mission is to advance the broader chemistry enterprise and its practitioners for the benefit of Earth and all its people. The Society is a global leader in promoting excellence in science education and providing access to chemistry-related information and research through its multiple research solutions, peer-reviewed journals, scientific conferences, eBooks and weekly news periodical Chemical & Engineering News. ACS journals are among the most cited, most trusted and most read within the scientific literature; however, ACS itself does not conduct chemical research. As a leader in scientific information solutions, its CAS division partners with global innovators to accelerate breakthroughs by curating, connecting and analyzing the world’s scientific knowledge. ACS’ main offices are in Washington, D.C., and Columbus, Ohio.
To automatically receive news releases from the American Chemical Society, contact [email protected].
Source: American Chemical Society (ACS)
State of Emergency in Iceland: Impending Volcanic Eruption Triggers Evacuation
Iceland declares state of emergency as volcanic eruption looms, thousands ordered to evacuate Grindavík. Tremors raise concerns at Fagradalsfjall volcano.
Iceland, known for its extraordinary landscapes and natural wonders, is currently facing a state of emergency as the Department of Civil Protection has ordered the mandatory evacuation of the city of Grindavík and the Svartsengi Power Station. The imminent threat of a volcanic eruption at Fagradalsfjall volcano has prompted this decisive action. With over 1,000 earthquakes reported in the past 24 hours and concerns about the underground movement of magma, authorities are taking swift measures to ensure the safety of the affected population.
A Troubled Region:
The recent surge in seismic activity has been primarily concentrated in Iceland’s Reykjanes Peninsula, an area that had remained dormant for 800 years until the eruption of Fagradalsfjall in 2021. The recurrence of tremors in this region has raised significant concerns among experts and prompted close monitoring by the Icelandic Met Office. The situation is further compounded by the possibility of substantial amounts of magma rising to the surface, intensifying the need for precautionary measures.
In response to the escalating threat, authorities have issued mandatory evacuation orders for the southwestern town of Grindavík, situated in proximity to the potential eruption site. The evacuation aims to relocate thousands of residents to safer areas, away from the imminent danger. Such measures are crucial to safeguard lives and minimize the potential impact of the volcanic activity on human settlements.
The Role of the Icelandic Met Office:
The Icelandic Met Office, responsible for monitoring natural phenomena in the region, plays a vital role in providing up-to-date information about seismic events, volcanic activity, and potential hazards. They have been closely observing the seismic patterns and underground movements to assess the likelihood and scale of an eruption. By issuing timely warnings and recommendations, they contribute to the coordinated response efforts of the authorities and assist in mitigating the risks associated with volcanic activity.
The Impact on Svartsengi Power Station:
The evacuation order also extends to the Svartsengi Power Station, a significant geothermal power plant located near Grindavík. This power station harnesses the volcanic energy of the area to generate electricity and provide district heating. However, the proximity to the potential eruption site poses an immediate risk to the facility and its personnel. The evacuation ensures the safety of the power station’s staff and prevents potential damage that could disrupt the region’s power supply.
Iceland’s declaration of a state of emergency and the subsequent evacuation orders in Grindavík and the Svartsengi Power Station reflect the country’s proactive approach to protecting its citizens in the face of natural disasters. The persistent seismic activity and the possibility of a volcanic eruption at Fagradalsfjall volcano have compelled authorities to take swift action. While the situation remains uncertain, the coordination between the Department of Civil Protection and the Icelandic Met Office provides hope in effectively managing the potential risks. As the affected residents seek shelter and support, the resilience and unity of the Icelandic community will undoubtedly play a crucial role in navigating this challenging period and recovering from its aftermath.
For more information, please refer to the story on EarthSky. https://earthsky.org/earth/iceland-braces-for-volcanic-eruption/
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