Monday, March 10, 2025

 

Decoding the neural basis of affective empathy: how the brain feels others' pain



Advanced brain imaging sheds light on how we encode others' pain



Institute for Basic Science

Figure 1 

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Experimental setup for observational fear testing and calcium imaging in observer mice. The observer mouse witnesses the demonstrator mouse receiving electric shocks, enabling the assessment of observational fear. During the experiment, miniature endoscopic calcium imaging is used to monitor neuronal activity in the observer's anterior cingulate cortex (ACC). Green-labeled neurons indicate cells expressing calcium indicators (GCamp6f), while white-labeled neurons represent activated cells observed through calcium imaging (Raw). The observed behaviors in the observational fear experiment include observer freezing (OB-freezing; pink), demonstrator pain response (DM-reaction; blue), and demonstrator freezing (DM-freezing; yellow). Lastly, examples of GCamp6f signals from neurons associated with each behavior are presented.

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Credit: Institute for Basic Science




Empathy—the ability to share and understand the emotions of others—is a cornerstone of human social interactions. When we witness someone in pain, we often experience a mirrored emotional response, a phenomenon known as affect sharing. While this ability is essential for social bonding and survival, the precise neural mechanisms behind empathy remain largely unknown.

A research team led by Dr. KEUM Sehoon at the Center for Cognition and Sociality (CCS) within the Institute for Basic Science (IBS) in South Korea has uncovered key insights into how the brain processes others’ distress. Using miniature endoscopic calcium imaging, the researchers identified specific neural ensembles in the anterior cingulate cortex (ACC) that encode empathic freezing, a behavioral response in which an observer reacts with fear when witnessing distress in others.

To investigate this phenomenon, the team conducted a series of real-time brain imaging experiments in mice, tracking individual neurons as they observed another mouse experiencing mild foot shocks. The results showed that specific ACC neurons were activated both when the observer experienced pain firsthand and when they witnessed another in pain, reinforcing the idea that observing distress triggers a neural response similar to direct pain experience.

The study further revealed that ACC population activity during empathic freezing closely resembles the neural representation of affective—rather than sensory—aspects of direct pain experiences. This suggests that witnessing another’s pain triggers activation in the ACC as if the observer were experiencing pain themselves, highlighting the ACC’s specialized role in processing the emotional aspects of pain.

Further analysis revealed that ACC neurons projecting to the periaqueductal gray (PAG), a brain region involved in fear and pain regulation, selectively conveyed emotional pain information. The researchers used optogenetics, a technique that enables precise control of neural activity with light, to manipulate this pathway. When they inhibited the ACC-to-PAG circuit, empathic freezing, and pain avoidance behaviors were significantly reduced. This confirms that this pathway transforms perceived distress into behavioral responses, reinforcing its crucial role in affective empathy.

Unlike previous studies that focused on animals with prior pain experience, this study used naïve observer mice with no previous exposure to pain, allowing the researchers to examine pure emotional contagion without the influence of past experiences. This approach provides new insights into the fundamental neural mechanisms of affective empathy.

Understanding how the brain encodes empathy could have major implications for mental health research. Conditions such as autism spectrum disorder (ASD), antisocial personality disorder, PTSD, and schizophrenia often involve difficulties in processing social and emotional cues. By identifying the specific brain circuits involved in affect sharing, scientists may develop new strategies for treating these disorders.

Dr. Keum stated, "Our findings pinpoint the specific brain circuits involved in processing others’ pain emotionally, offering a foundation for new approaches to studying empathy-related neuropsychiatric disorders."

This study was published online on February 25 in the journal Nature Communications.

The boundaries of drainage basins shifted faster during past episodes of climate change, according to a new theory by Ben-Gurion University geologists



They present first ever time dependent record of drainage divide migration rates




Ben-Gurion University of the Negev





BEER-SHEVA, Israel, March 10, 2025 – Using a unique field site in the Negev, Ben-Gurion University of the Negev geologists have presented the first-ever time-dependent record of drainage divide migration rates. Prof. Liran Goren, her student Elhanan Harel, and co-authors from the University of Pittsburgh and the Geological Survey of Israel, further demonstrate that episodes of rapid divide migration coincide with past climate changes in the Negev over the last 230,000 years (unrelated to present-day climate change).

It is an astounding achievement that will accelerate our understanding of how climate affects the Earth's surface.

Their findings were just published in PNAS (Proceedings of the National Academy of Sciences).

The researchers focused on the migration rate of drainage divides—the topographic boundaries separating neighboring drainage basins. Drainage basins are hydrologic units that accumulate surface water into a single outlet. As divides shift, they reshape basin boundaries and redistribute surface water, rock particles, and ecological niches across landscapes. Until now, the state of the art has been limited to long-term average divide migration rates.

However, a unique site presenting a sequence of terraces in the Negev desert of Israel has provided the first traceable record of divide location at different snapshots in time, constraining a time series of divide migration rate. Combining field observations, river terrace dating, and numerical simulations, they were able to infer divide migration dynamics in the Negev Desert, over the last 230,000 years. By doing so, they discovered for the first time that episodes of accelerated migration, more than twice the rate of other episodes, coincide with regional climate fluctuations indicated by regional paleoclimate proxies.

"It's an exciting discovery," says Prof. Liran Goren of the Department of Earth and Environmental Sciences, "We were not expecting to discover the correlation with climate fluctuations nor the speed with which the divide shifted during that time. It adds to our knowledge of the drivers affecting the Earth's surface evolution in fascinating ways."

"I think what’s fascinating about this research is that a small channel in the Negev desert, which at first glance doesn’t seem particularly remarkable, can actually hold such an impressive record of drainage divide migration along its course," says Elhanan Harel. "The findings from this study are important for better understanding the nature of divide migration, while also contributing to the ongoing scientific discussion about the climatic history of the Negev."

Additional researchers include Onn Crouvi and Naomi Porat of the Geological Survey of Israel, Tianyue Qu and Eitan Shelef, of the University of Pittsburgh, and Hanan Ginat of the Dead Sea and Arava Science Center.

This research was supported by the United States–Israel Binational Science Foundation (BSF), grant number 2019656 and the United States National Science Foundation (NSF-Geomorphology and Land-use Dynamics), grant number 1946253.

 

New study reveals why students reject ChatGPT feedback in academic writing



Research highlights several challenges in ChatGPT-generated feedback acceptance among second-language learners





ECNU Review of Education

Challenges in accepting ChatGPT feedback 

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A second-language student evaluating ChatGPT feedback on their academic writing, highlighting the factors leading to the acceptance or rejection of AI-generative content

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Credit: Jernej Furman from Wikimedia Commons Image Source Link: https://openverse.org/image/8dbf3f94-a659-4589-9ae0-a13861df47eb?q=CHATGPT&p=20




Generative AI tools like ChatGPT present extraordinary potential in promoting better language learning and teaching practice, such as timely feedback, ease of use, personalized support, simulations of the learning environment, and individualized recommendations on learning materials. However, a team of researchers in Hong Kong and Macao found that 45.9% of ChatGPT-generated feedback was rejected by second-language students, higher rejection rates for content-focused feedback (58.7%) than form-focused (41.3%).

To investigate why second-language learners reject feedback generated by ChatGPT. A team of researchers in Hong Kong and Macao, led by Associate Professor Wei Wei, from Macao Polytechnic University analyzed 45 Computer Science undergraduates tasked with revising argumentative essays using ChatGPT feedback. This study was published online on January 7, 2025, in the ECNU Review of Education.  Through mixed-method analysis of self-reflection and actual revision behaviors, the team identified four key factors driving rejection:

 

  1. Mismatched expectations: Feedback often misinterpreted student intent or lacked clarity.
  2. High workload: Overwhelming or vague suggestions discouraged engagement.
  3. Conflicts with external references: Discrepancies between AI advice and teacher/peer feedback caused distrust.
  4. Impeding conditions: Limited emotional support and non-personalized responses hindered usability.

 

Notably, content-focused feedback (e.g., argument structure, evidence quality) faced higher rejection due to its subjective nature, while form-focused feedback (e.g., grammar, vocabulary) was more readily accepted but still challenged by effort-related barriers. 

Our findings reveal that students aren’t dismissing AI feedback outright - they’re struggling with its relevance and practicality,” explains Prof. Wei. “For content-related suggestions, misalignment with their goals or external standards often leads to rejection. Meanwhile, even straightforward grammar tips can feel burdensome if not contextualized.

The study also highlights a critical paradox: while ChatGPT’s accessibility is praised, its inability to provide emotionally supportive or proficiency-tailored feedback limits its effectiveness. “Students need more than raw suggestions; they require scaffolding to interpret and apply AI-generated insights,” Prof. Wei adds.

***

Reference

Titles of original papers: Unpacking the Rejection of L2 Students Toward ChatGPT-Generated

Feedback: An Explanatory Research

Journal: ECNU Review of Education

DOI: 10.1177/20965311241305140

 

Are volcanoes behind the oxygen we breathe?



New research suggests volcanic activity billions of years ago set the stage for the oxygen-rich atmosphere all life on Earth depends upon




University of Tokyo

Biogeochemical cycles billions of years ago 

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A complex web of interactions between geological features including volcanoes, subsurface mantle, oceans and the atmosphere created the chemical mixture necessary for early life to oxygenate our atmosphere.

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Credit: ©2025 Watanabe et al. CC-BY-ND




It is widely believed that Earth’s atmosphere has been rich in oxygen for about 2.5 billion years due to a relatively rapid increase in microorganisms capable of performing photosynthesis. Researchers, including those from the University of Tokyo, provide a mechanism to explain precursor oxygenation events, or “whiffs,” which may have opened the door for this to occur. Their findings suggest volcanic activity altered conditions enough to accelerate oxygenation, and the whiffs are an indication of this taking place.

Take a deep breath. Do you ever think about the air entering your lungs? It’s mostly inert nitrogen, and the valuable oxygen our lives depend on only accounts for 21%. But this hasn’t always been the case; in fact, several mass extinction events correspond to times when this figure changed dramatically. And if you go back far enough, you’ll find that before about 3 billion years ago, there was hardly any oxygen at all. So what changed, and how did it happen?

The scientific consensus is that about 2.5 billion years ago, the Great Oxygenation Event (GOE) took place, most likely due to a proliferation of microorganisms exploiting favorable conditions and facing little competition. They would have essentially converted the carbon dioxide-rich atmosphere into an oxygen-rich one, and following that came complex life, which favored this new abundance of oxygen. But it seems there were some precursor oxygenation events prior to the GOE that may indicate the exact nature and timing of changes in the conditions necessary for the GOE to begin.

“Activity of microorganisms in the ocean played a central role in the evolution of atmospheric oxygen. However, we think this would not have immediately led to atmospheric oxygenation because the amount of nutrients such as phosphate in the ocean at that time was limited, restricting activity of cyanobacteria, a group of bacteria capable of photosynthesis,” said Professor Eiichi Tajika from the Department of Earth and Planetary Science at the University of Tokyo. “It likely took some massive geological events to seed the oceans with nutrients, including the growth of the continents and, as we suggest in our paper, intense volcanic activity, which we know to have occurred.”

Tajika and his team used a numerical model to simulate key aspects of biological, geological and chemical changes during the late Archean eon (3.0-2.5 billion years ago) of Earth’s geologic history. They found that large-scale volcanic activity increased atmospheric carbon dioxide, thereby warming the climate, and increased nutrient supply to the ocean, thus feeding marine life, which in turn temporarily increased atmospheric oxygen. The increase in oxygen was not very steady, though, and came and went in bursts now known as whiffs.

“Understanding the whiffs is critical for constraining the timing of the emergence of photosynthetic microorganisms. The occurrences are inferred from concentrations of elements sensitive to atmospheric oxygen levels in the geologic record,” said visiting research associate Yasuto Watanabe. “The biggest challenge was to develop a numerical model that could simulate the complex, dynamic behavior of biogeochemical cycles under late Archean conditions. We built upon our shared experience with using similar models for other times and purposes, refining and coupling different components together to simulate the dynamic behavior of the late-Archean Earth system in the aftermath of the volatile volcanic events.”

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Journal article:

Yasuto Watanabe, Kazumi Ozaki, Mariko Harada, Hironao Matsumoto & Eiichi Tajika, “Mechanistic links between intense volcanism and the transient oxygenation of the Archean atmosphere”, Communications Earth & Environment, DOI: 10.1038/s43247-025-02090-x, https://doi.org/10.1038/s43247-025-02090-x


Funding: This work is supported by Grant-in-aid for JSPS KAKENHI Grants Number 24H00267 (K.O.), and JST FOREST Program (Grant JPMJFR2274, Japan) (K.O.).


Useful links:
Department of Earth and Planetary Science - https://www.eps.s.u-tokyo.ac.jp/en/
Graduate School of Science - https://www.s.u-tokyo.ac.jp/en/index.html

Research contact:
Professor Eiichi Tajika
Department of Earth and Planetary Science, The University of Tokyo,
7-3-1 Hongo, Bunkyo-ku, Tokyo, 113-0033, Japan
tajika@eps.s.u-tokyo.ac.jp

Press contact:
Mr. Rohan Mehra
Public Relations Group, The University of Tokyo,
7-3-1 Hongo, Bunkyo-ku, Tokyo, 113-8656, Japan
press-releases.adm@gs.mail.u-tokyo.ac.jp

 

About The University of Tokyo:

The University of Tokyo is Japan's leading university and one of the world's top research universities. The vast research output of some 6,000 researchers is published in the world's top journals across the arts and sciences. Our vibrant student body of around 15,000 undergraduate and 15,000 graduate students includes over 4,000 international students. Find out more at www.u-tokyo.ac.jp/en/ or follow us on X (formerly Twitter) at @UTokyo_News_en.

 

Japan’s Antarctic Meteorite Collection earns global recognition as IUGS Geo-collection


Collection holds 17,400 meteorites



Research Organization of Information and Systems

Japanese Antarctic Meteorite Collection 

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The Antarctic Meteorite Collection at the National Institute of Polar Research in Japan houses 17,400 meteorites.

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Credit: Atsushi Takenouchi




The Antarctic Meteorite Collection at the National Institute of Polar Research (NIPR) in Japan has been recognized as a Geo-collection by the International Union of Geological Sciences (IUGS). An IUGS Geo-collection is a museum collection of global importance because of its particularly high scientific, historical, or educational relevance for geological sciences. With over 17,400 meteorites, the Antarctic Meteorite Collection offers invaluable insights into the early solar system, planetary bodies, the Moon, and Mars. Carefully classified and stored, these samples complement space mission findings, advancing global research on planetary evolution and solar system history.

These meteorites play a unique role in advancing planetary science because they are minimally altered extraterrestrial samples. “Antarctic meteorites are invaluable for understanding the origins, evolution, and diversity of solar system materials. Their pristine preservation and wide variety offer unique insights into planetary formation and processes, highlighting their critical scientific, historical, and educational value,” said Associate Professor Akira Yamaguchi from NIPR.

Meteorites are solid fragments of extraterrestrial materials, larger than ~2 millimeter, that have traveled from space to land on the Earth. When they enter Earth's atmosphere, their surface experiences intense heat, causing the surface to melt and then solidify. This process results in a characteristic black fusion crust. 

Many meteorites are unique in that their formation ages are commonly as old as 4.6 billion years. Earth's rocks never reach this age because of continuous igneous activity that occurs with plate tectonics. Because of their significant age, meteorites are among the most ancient materials available for scientific study.

Scientists believe that most meteorites originate from small bodies in the asteroid belt between the orbits of Mars and Jupiter. Large-scale volcanic activity does not occur in these small bodies, so they preserve their primitive nature and the formation age of the early solar system.

NIPR houses over 17,400 Antarctic meteorites, primarily recovered from blue ice fields near the Yamato and Sør Rondane Mountains during Japanese Antarctic research expeditions. In 1969, a Japanese Antarctic research expedition discovered nine meteorites while investigating the ice sheet near the Yamato Mountains. Since then, they have discovered 17,400 meteorites in 24 expeditions.

At NIPR, the Antarctic meteorites are classified, cataloged, and stored under strict clean-room conditions to minimize weathering. Researchers have classified more than 13,000 meteorites, with data shared globally. Originating from diverse bodies in the solar system, these samples complement space mission findings and advance the understanding of planetary evolution.

“The National Institute of Polar Research's mission as a shared-use facility has received international recognition, emphasizing its significant role in advancing planetary science through global collaboration. Being part of the inaugural designation by IUGS Geo-collection, alongside prestigious collections like the Vienna Natural History Museum, further underscores the exceptional value and importance of the Antarctic meteorite collection,” said Yamaguchi.

With its 17,400 meteorites, the Japanese Meteorite Collection is one of the largest collections of extraterrestrial material in the world. By distributing these meteorite samples to researchers all over the world, the organization contributes to the development of planetary sciences. Beyond their extensive collections, the Antarctic Meteorite Research Center actively collaborates with asteroid sample return missions and leading domestic and international research institutions to provide a comprehensive approach to the study of extraterrestrial materials.

Looking ahead, NIPR hopes to continue the detailed analysis of Antarctic meteorites, focusing on their mineralogical, petrological, chemical, and isotopic properties to uncover further insights into the early solar system's formation processes. NIPR also seeks to expand collaborative research and enhance the accessibility of these samples to the global scientific community. “The ultimate goal is to build a comprehensive understanding of solar system evolution, including the differentiation of planetesimals and the formation of planets, while preserving the scientific and educational value of Antarctic meteorite collections for future generations,” said Yamaguchi.

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IUGS Geo-collection
An IUGS Geo-collection is a museum collection or part of a museum collection of global importance because of its particularly high scientific, historical, or educational relevance for geological sciences.
Website: https://iugs-geoheritage.org/designations-geo-collections/

Antarctic Meteorite Research Center, National Institute of Polar Research
The Antarctic Meteorite Research Center stores meteorites collected by the Japanese Antarctic Research Expeditions. The total number of meteorites held is approximately 17,400 (including unregistered meteorites), making it one of the largest collections of extraterrestrial material in the world. By distributing these meteorite samples to researchers all over the world, the organization contributes to the development of planetary sciences. As well as our extensive collections, we actively collaborate with asteroid sample return missions and leading domestic and international research institutions to provide a comprehensive approach to the study of extraterrestrial materials.
https://yamato.nipr.ac.jp/english/

About National Institute of Polar Research (NIPR)
The NIPR engages in comprehensive research via observation stations in Arctic and Antarctica. As a member of the Research Organization of Information and Systems (ROIS), the NIPR provides researchers throughout Japan with infrastructure support for Arctic and Antarctic observations, plans and implements Japan's Antarctic observation projects, and conducts Arctic researches of various scientific fields such as the atmosphere, ice sheets, the ecosystem, the upper atmosphere, the aurora and the Earth's magnetic field. In addition to the research projects, the NIPR also organizes the Japanese Antarctic Research Expedition and manages samples and data obtained during such expeditions and projects. As a core institution in researches of the polar regions, the NIPR also offers graduate students with a global perspective on originality through its doctoral program. For more information about the NIPR, please visit: https://www.nipr.ac.jp/english/

About the Research Organization of Information and Systems (ROIS)
ROIS is a parent organization of four national institutes (National Institute of Polar Research, National Institute of Informatics, the Institute of Statistical Mathematics and National Institute of Genetics) and the Joint Support-Center for Data Science Research. It is ROIS's mission to promote integrated, cutting-edge research that goes beyond the barriers of these institutions, in addition to facilitating their research activities, as members of inter-university research institutes.