Operation Lightning dismantled SocksEscort proxy botnet exploiting 369,000 IPs in 163 countries, disrupting fraud networks and freezing $3.5M crypto.
🚱Plants face various environmental stresses, to which they respond in different ways. Due to climate change, it is expected that plants will encounter increased phases of drought and changes in herbivory.
🐛This study thus aimed to evaluate the intra-individual variation in responses, that is phenotypic plasticity, to single and combined stresses, including drought and insect herbivory. Authors used plants of the aromatic species Tanacetum vulgare, which are characterized by distinct terpenoid chemotypes and metabolic fingerprints shaped by maternal origin. Clones were exposed to no stress, drought, herbivory, or a combination of both.
⚗️The impacts of these treatments were determined in terms of aboveground biomass as well as emission rates or concentrations, richness, and functional Hill diversity (FHD) of volatile organic compounds (VOCs), stored leaf and root terpenoids, and leaf metabolic fingerprints.
📊Drought resulted in lower plant aboveground biomass, VOC richness, and VOC FHD. Herbivory had no effect on biomass, but increased the VOC emission rates and richness, also in combination with drought. The treatment significantly affected the phenotypic plasticity of the aboveground biomass and VOC emission.
👉These findings highlight the importance of studying intra-individual variation in plant responses to different stresses and their combinations to fully comprehend the finely tuned chemodiversity.
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The reef is a home and feeding ground for dozens of species that depend on it the way a woodland creature depends on trees. It has survived ice ages – but whether it will survive increasing pressures from industrial fishing, deep-sea mining and climate change is, in part, a question about data. If we don’t know it exists, how can we protect it?
A new project called Deep Vision could fundamentally transform our understanding of the deep ocean by digging into pictures and videos sat largely unexamined in research archives around the world. By using AI, thousands of hours of seafloor footage can be analysed to produce the first comprehensive maps of vulnerable marine ecosystems across the entire Atlantic basin.
Over the past two decades, robotic and autonomous underwater vehicles have collected vast quantities of footage from the deep sea. This represents an extraordinary resource – a record of ecosystems that most humans will never see.
Our planet plunged into one of the most dramatic climate states in its long history, approximately 720–635 million years ago. During a period geologists call Snowball Earth, ice sheets crept from the poles all the way to the tropics, covering the oceans and continents in a nearly global freeze.
Evidence for this extreme climate comes from rock formations around the world that bear the signatures of ancient glaciers at low latitudes—signs that Earth’s surface was encased in ice far beyond what we see in today’s polar regions.
Scientists have long studied how a feedback process known as ice-albedo helped lock in and amplify this deep chill. Albedo is a measure of how much sunlight a surface reflects; snow and ice are bright and reflect most of the sun’s energy back into space, cooling the planet further as more of it spreads across the surface.
While sifting through the extensive data collected by NASA’s Mars Atmosphere and Volatile Evolution (MAVEN) spacecraft over the last decade, scientists discovered a familiar type of electromagnetic signal commonly caused by lightning. This rare find represents the first direct indication of lightning activity on Mars. The team recently published their findings in Science Advances, where they describe the event and why it’s so difficult to detect lightning-like activity on Mars.
Whistler waves are low-frequency radio wave signals generated by lightning, which create an impulse that propagates through a planet’s magnetosphere, following along the magnetic field lines. The whistler waves disperse due to the slower velocity of the lower frequencies through the plasma of the ionosphere and magnetosphere. These waves are typical on Earth, but have also been observed on Jupiter, Saturn and Neptune. All of these planets all possess strong magnetic fields and corresponding magnetospheres, facilitating the movement of whistler waves.
Mars, on the other hand, does not have a global, Earth-like magnetic field. This is because the internal activity that causes these magnetic fields ceased on Mars billions of years ago. This may contribute to the fact that lightning-like discharges in the Martian atmosphere have not yet been observed. But lightning-like activity on Mars is not impossible.
Greenland’s largest glacier, Jakobshavn Glacier, may be edging closer to a critical threshold as meltwater runoff from the Greenland Ice Sheet accelerates in ways not seen in over a century, according to new research published in Climate of the Past. The study reconstructs more than 100 years of freshwater discharge flowing from the ice sheet into Disko Bay in western Greenland, revealing a striking and sustained change that began in the early 2000s.
Researchers from Kiel University, Germany, and colleagues found that runoff did not increase gradually, but instead shifted into sharp acceleration. By 2007, the volume of freshwater entering the ocean had permanently exceeded the range of natural variability seen throughout the 20th century. Simply put, the system appears to have moved into a new state, one characterized by consistently higher meltwater output. This pattern suggests the ice sheet may be approaching what scientists call a “tipping point”—a threshold beyond which changes become self-reinforcing and potentially difficult to reverse.
Some solid materials can cool down or heat up when pressure is applied or released. This behavior enables cooling and heating technologies that do not rely on climate-damaging refrigerant gases. In practice, however, a major obstacle remains: many materials behave differently during heating and cooling, which makes their response difficult to use reliably in real devices. In a study published in the journal Communications Materials, researchers investigate a solid material known for its exceptionally large cooling/heating response (thermal response) under pressure and ask a simple question: can this response be made more reliable? They show that a very small change in composition leads to a clear improvement and use neutron experiments to explain why this improvement occurs.
“If you don’t know exactly how much emissions you have, then it’s really difficult to make effective policies or technologies or methods to reduce the emissions,” said Dr. Z. Jason Ren. [ https://www.labroots.com/trending/earth-and-the-environment/…-reports-2](https://www.labroots.com/trending/earth-and-the-environment/…-reports-2)
Are national climate reports missing crucial data points regarding wastewater greenhouse gas (GHG) emissions? This is what a recent study published in Nature Climate Change hopes to address as a team of researchers investigated the accuracy of national inventory reports (NIRs) for wastewater GHG. This study has the potential to help researchers, climate scientists, legislators, and the public better understand the methods for tracking climate change and steps that can be taken to fill the gaps in report lapses.
For the study, the researchers obtained data from 38 countries regarding wastewater GHG emissions with the goal of ascertaining existing data gaps in NIRs. The motivation of this study comes from the lack of consistent data methods and large changes that occur over many years and in global regions. The overarching goal of the study was to ascertain where the data gaps exist and how to fill them.
In the end, the researchers discovered massive data gaps in wastewater GHG emissions, including an unreported gap of 52.0–73.2 million metric tons (MMT) of CO2-equivalent (CO2e) annually across the 38 countries. Additionally, they found that global gap of 94–150 MMT CO2e annually.
Fifteen years ago, I wrote something that annoyed many techno-optimists.
Ten years ago, I filmed it as a podcast.
Today it feels less controversial — and more urgent.
Technology is NOT Enough.
We have the science to feed everyone. We have the tech to provide clean water. We understand climate change. We know how to reduce suffering.
And yet we don’t act.