Monday, November 10, 2025

 

HKUST unites international experts in CliMetS initiative to tackle climate threat of seabed methane seeps



A UN ocean decade-endorsed action advances global research with landmark workshops in Latin America and Africa




Hong Kong University of Science and Technology

A group photo at CliMetS-Central and South America Workshop 

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A group photo of Prof. QIAN Peiyuan (middle, in black suit), Chair Professor of the Department of Ocean Science at HKUST and the participants of the CliMetS-Central and South America Workshop, including Rear Admiral Hermann Aicardo LEÓN RINCÓN (second row, seventh right), Director of Maritime and River Interests of the Colombian Navy, and Prof. Paula Andrea ZAPATA RAMÍREZ (second row, sixth right from Universidad Pontificia Bolivariana, co-organizer of the workshop.

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Credit: HKUST





The Hong Kong University of Science and Technology (HKUST) has successfully launched the Global Climate Impact of Methane Seeps (CliMetS) Initiative through a pivotal collaboration with the Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (GML) and over 200 experts worldwide. Endorsed as a UN Ocean Decade Action, CliMetS is dedicated to mapping seabed methane seeps across the world’s oceans and quantifying their impact on global climate systems. Recently, HKUST co-led two milestone workshops in South America and Africa, galvanizing global efforts to address methane seep research gaps and fostering cross-continental partnerships.

Bridging the Gap: Knowledge Exchange and Capacity Sharing

Methane is a potent greenhouse gas, with a warming potential over 80 times that of carbon dioxide over a 20-year period. Vast reservoirs stored under the seabed could significantly accelerate climate change if released, yet the scale and processes of these seeps remain one of Earth’s most pressing scientific mysteries. To address this critical gap in understanding, Prof. QIAN Peiyuan, Chair Professor of the Department of Ocean Science at HKUST, Deputy Director of GML and Director of the Hong Kong Branch of GML, is spearheading CliMetS as its Program Director and Management Committee Chair, striving to transform fragmented and localized studies into a unified mission.

Prof. Qian highlighted the significance of the CliMetS initiative: “A core objective of CliMetS is to promote knowledge exchange and capacity sharing, particularly in Global South countries that often lack critical resources such as skilled talent, infrastructure, and advanced technologies. By leveraging the state-of-the-art research technologies and facilities from China and other developed countries, including China’s deep-sea research vessel Shen Hai Yi Hao and the manned submersible Jiaolong, we aim to organize international joint cruises for large-scale methane seep exploration across the globe.” He emphasized that regional research agendas must be co-designed and co-owned by regional stakeholders.

Regional Workshops Forge a Collaborative Path and Deliver Actionable Outcomes

Co-initiated by key institutions—including GML, HKUST, the South China Sea Institute of Oceanology of the Chinese Academy of Sciences, the China Deep Ocean Affairs Administration, the Federal University of Rio de Janeiro, and the University of Nairobi — CliMetS has gained significant momentum through a series of regional workshops, bringing together local experts to co-define research priorities and co-formulate actionable plans. To date, the initiative has united 217 scientists from 138 institutions across 53 countries, with nearly 80 new participants joining through recent workshops. These concerted efforts have successfully forged a cohesive global research community and delivered concrete outcomes.

Two landmark workshops, co-led by HKUST, were held in South America and Africa in October:

  • CliMetS-Central and South America Workshop in Colombia: This event brought together over 40 scholars, government officials, and business leaders from 12 countries across the Americas. Key outcomes included the development of a visionary research roadmap and the planning of a future CliMetS international research cruise dedicated to capacity sharing in Latin America. Participants identified the lack of regional coordination and infrastructure as the main obstacles to advancing methane seep research. They agreed that CliMetS would serve as a much-needed platform to unify regional efforts, foster collaboration between science and policy, and elevate the regional research to a new level.
  • CliMetS-Africa Workshop in Kenya: Following this success, the Africa workshop convened over 70 experts from 17 countries across the continent to take stock of the regional knowledge and capacity, define research priorities, and develop regional action plans to chart the way forward. The discussions yielded important results, including a comprehensive understanding of the current state of regional research and the opportunities to leverage the existing infrastructures built by IOC-UNESCO Africa and other UN agencies in the region. As a major step forward, participants identified key priority areas for future studies and promptly formed two groups, each electing a dedicated management team to oversee cruise planning and coordination.

Reflecting on the success of these gatherings, Prof. Qian added, "The overwhelmingly positive response and strong support from experts, and the active and enthusiastic engagement of IOC- UNESCO offices and governments in both regions underscored the global significance and transformative potential of CliMetS. All the participants agreed that CliMetS fills a critical void by integrating regional efforts and to promoting cross-boundary collaborations, extending its impact far beyond the scientific communities. They expressed deep appreciation for the leadership of GML and HKUST in spearheading and implementing the CliMetS initiative, reaffirming the value and importance of our efforts."

Looking Ahead: A Decade of Discovery

With a solid foundation established, CliMetS is now focused on an ambitious future agenda. The initiative plans to expand its global reach with workshops in other key regions, integrate the findings and priorities from the Americas and Africa into a consolidated global action plan, and drive forward large-scale campaigns, such as the development of a real-time, global methane seep observatory network, to decisively advance the field. The ultimate goal is to provide the robust scientific data needed to inform more accurate international climate models and policy decisions.

 

Dinosaur eggshells unlock a new way to tell time in the fossil record


An international team of geologists and paleontologists is pioneering a groundbreaking methodology to reliably determine the age of fossil-bearing rocks — by directly dating fossilized dinosaur eggshells.



Stellenbosch University

Artistic reconstruction of a newly hatched troodontid-like dinosaur 

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Artistic reconstruction of a newly hatched troodontid-like dinosaur resting among fragments of its eggshell (loosely based on Mongolian microtroodontid-type). These eggshells, when buried within ancient soil, interacted with meteoric waters, leading to early uranium incorporation into the eggshell calcite crystals.

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Credit: Eva Utsukiyouhei (宇津城遥平





An international team of geologists and paleontologists is pioneering a groundbreaking methodology to reliably determine the age of fossil-bearing rocks — by directly dating fossilized dinosaur eggshells.

The study, led by Dr Ryan Tucker from Stellenbosch University’s Department of Earth Sciences, was published in Communications Earth & Environment.

Many fossil sites around the world are only coarsely dated. Without precise information on the geologic age of fossils, paleontologists struggle to understand how different species and ecosystems relate across time and space. Usually, researchers rely on dating minerals such as zircon or apatite found associated with fossils, but those minerals aren’t always present. Attempts to date the fossils themselves, such as bones or teeth, have often produced uncertain results.

Dr Tucker’s team took a different approach. They used advanced uranium–lead (U–Pb) dating and elemental mapping to measure trace amounts of uranium and lead housed inside the calcite of fossilized dinosaur eggshells. These isotopes function like a natural clock, enabling scientists to determine when the eggs were buried.

View video on novel method.

Tests on dinosaur eggs from Utah (USA) and the Gobi Desert (Mongolia) showed that the eggshells record ages with an accuracy of about five percent relative to precise volcanic-ash dates. In Mongolia, the team determined the first-ever direct age — around 75 million years old — for a historic locality preserving dinosaur eggs and nests.

“Eggshell calcite is remarkably versatile,” says Dr Tucker. “It gives us a new way to date fossil sites where volcanic layers are missing, a challenge that has limited paleontology for decades.”

The work involved collaborators from the North Carolina Museum of Natural Sciences, North Carolina State University, Colorado School of Mines, Mongolian Academy of Sciences’ Institute of Paleontology, Universidade Federal de Ouro Preto (Brazil). Fieldwork in Mongolia was carried out through the Mongolian Alliance for Dinosaur Exploration (MADEx) and supported by the National Geographic Society and the National Science Foundation.

By showing that dinosaur eggshells can reliably record the passage of geologic time, the study links biology and Earth science in a new way — offering researchers a powerful tool to date fossil sites around the globe.

“Direct dating of fossils is a paleontologist’s dream,” says study co-author Lindsay Zanno, associate research professor at North Carolina State University and head of paleontology at the North Carolina Museum of Natural Sciences. “Armed with this new technique, we can unravel mysteries about dinosaur evolution that used to be insurmountable.”

The article “U–Pb calcite age dating of fossil eggshell as an accurate deep time geochronometer” was published in Communications Earth & Environment.


Novel method to age-date fossilized dinosaur eggs, using a MC-ICP-MS instrument [VIDEO] 


This team from Stellenbosch University (SU) developed a novel method to age-date fossilized dinosaur eggs, using a Neoma Multi-Collector, Inductively Coupled Plasma, Mass Spectrometer (MC-ICP-MS) instrument, hosted in the Elemental and Isotope Analysis Laboratory in SU’s Department of Earth Sciences. With its capacity to measure multiple isotopes simultaneously at very high precision and accuracy, the MC-ICP-MS is uniquely suited to addressing a wide range of research questions – from tracing fluid–rock interactions and quantifying elemental cycling in natural systems, to reconstructing ancient ocean chemistry and refining high-resolution geochronological frameworks.

Credit

Stefan Els, Stellenbosch University


Elemental map of the isotope strontium (Sr) from dinosaur eggshell collected from Teel Ulaan Chaltsai, Eastern Gobi Basin.  Elemental maps were used by the researchers to evaluate if the uptake of strontium (Sr) was uniformly distributed across the eggshell. A uniform distribution indicates that uptake of this and other isotopes occurred after burial but prior to fossilization.

This team from Stellenbosch University (SU) developed a novel method to age-date fossilized dinosaur eggs, using a Neoma Multi-Collector, Inductively Coupled Plasma, Mass Spectrometer (MC-ICP-MS) instrument, hosted in the Elemental and Isotope Analysis Laboratory in SU’s Department of Earth Sciences. They are, from left to right, Prof Chris Luna, MSc student Kira Venter, and Dr Ryan Tucker. With its capacity to measure multiple isotopes simultaneously at very high precision and accuracy, the MC-ICP-MS is uniquely suited to addressing a wide range of research questions – from tracing fluid–rock interactions and quantifying elemental cycling in natural systems, to reconstructing ancient ocean chemistry and refining high-resolution geochronological frameworks

Credit

Stefan Els

Neanderthal DNA helps explain how faces form




The Company of Biologists







Every human face is unique, allowing us to distinguish between individuals. We know little about how facial features are encoded in our DNA, but we may be able to learn more about how our faces develop by looking at our ancient relatives, the Neanderthals. Neanderthal faces were quite distinctive from our own, with large noses, pronounced brows and a robust lower jaw. Now, scientists from the MRC Human Genetics Unit in the Institute of Genetics and Cancer at the University of Edinburgh, UK, are using the DNA of our extinct distant relatives to learn more about how faces develop and evolve. Published today in the journal Development, they show how a region of Neanderthal DNA is better at activating a jaw-forming gene than the human counterpart, revealing one potential reason for Neanderthal’s larger lower jaws.

Hannah Long (University of Edinburgh, UK), who led the study, explains that scientists have sequenced the Neanderthal genome using DNA extracted from ancient bone and says, “The Neanderthal genome is 99.7% identical to the genome of modern-day humans and the differences between species are likely responsible for altering appearance”. Both human and Neanderthal genomes consist of about 3 billion letters that code for proteins and regulate how genes are used in the cell, which makes finding regions that impact appearance like looking for a needle in a haystack. Fortunately, Long and her colleagues had an informed idea where to look first: a region of the genome that is linked to Pierre Robin sequence, a syndrome in which the lower jaw is disproportionately small. “Some individuals with Pierre Robin sequence have large deletions or DNA rearrangements in this part of the genome that change face development and limit jaw formation. We predicted that smaller differences in the DNA might have more subtle effects on face shape,” said Long.

By comparing human and Neanderthal genomes, the team found that in this region, roughly 3000 letters in length, there were just three single-letter differences between the species. Although this region of DNA doesn’t contain any genes, it regulates how and when a gene is activated, specifically a gene called SOX9, a key coordinator of the process of face development. To demonstrate that these Neanderthal-specific differences are important for the development of the face, Long and colleagues needed to show that the Neanderthal region could activate genes in the right cells at the right time as the embryo develops. The researchers simultaneously inserted the Neanderthal and human versions of the region into the DNA of zebrafish and programmed the zebrafish cells to produce different colours of fluorescent protein depending on whether the human or Neanderthal region was active. Watching the zebrafish embryos develop, the researchers found that both the human and Neanderthal regions were active in the zebrafish cells that are involved in forming the lower jaw and the Neanderthal region was more active than the human version.

“It was very exciting when we first observed activity in the developing zebrafish face in a specific cell population close to the developing jaw, and even more so when we observed that the Neanderthal-specific differences could change its activity in development,” said Long. “This led us to think about what the consequences of these differences could be, and how to explore these experimentally.” Knowing that the Neanderthal sequence was more powerful at activating genes, Long and colleagues then asked if the resulting increased activity of its target, SOX9, might change the shape and function of the adult jaw. To test this theory, they provided the zebrafish embryos with extra SOX9 and found that cells that contribute to forming the jaw occupied a larger area.

“In our lab, we are interested in exploring the impact of additional DNA sequence differences, using a technique that mimics aspects of facial development in a dish. We hope this will inform our understanding of sequence changes in people with facial conditions and inform diagnosis,” says Long. This research shows that by studying extinct species we can learn how our own DNA contributes to face variation, development and evolution.

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