NTU Scientists Unlock Secret of Earth's Missing Lead

NTU's Groundbreaking Discovery Resolves Decades-Old Geological Puzzle

Nanyang Technological University (NTU) in Singapore has made headlines with a revolutionary study that finally explains one of Earth's longest-standing geochemical mysteries: the location of the planet's 'missing lead.' For over 50 years, scientists have puzzled over why the lead isotopes in Earth's accessible rocks do not match those in ancient meteorites, suggesting a deficit of primordial lead. Led by Professor Simon Redfern from NTU's Asian School of the Environment, the research reveals that this lead is sequestered deep within the mantle in stable, high-pressure compounds.

This breakthrough not only rewrites our understanding of Earth's interior but also highlights NTU's prowess in computational geochemistry, positioning Singapore as a hub for cutting-edge Earth sciences research.

The Missing Lead Paradox Explained

Lead isotopes serve as a clock for Earth's history. Primordial lead-204 is non-radiogenic, while lead-206, 207, and 208 form from the decay of uranium and thorium. When geochemists compare Earth's surface rocks to chondritic meteorites—the building blocks of our planet—they find an imbalance. Earth's mantle appears enriched in 'young' radiogenic lead and depleted in ancient lead-204, implying the planet is younger than its 4.5-billion-year age derived from meteorites.

Previous theories suggested the missing lead sank into the core during Earth's differentiation, but lacked a mechanism for its isolation from uranium and thorium in the silicate Earth. NTU's study provides the missing piece: hidden reservoirs in the deep mantle stabilized by extreme pressures.

NTU Team's Innovative Computational Approach

The NTU researchers employed advanced first-principles simulations using the CALYPSO software—a crystal structure prediction tool based on particle swarm optimization. Density functional theory (DFT) calculations, run on supercomputers, modeled lead-sulfur interactions at pressures up to 150 gigapascals (GPa) and temperatures exceeding 5,000°C, mimicking conditions near the core-mantle boundary (about 135 GPa and 4,000°C).

Ab initio molecular dynamics simulated melting behaviors, while phonon calculations confirmed phase stability. This computational mineral physics approach bypassed the impossibility of direct sampling from Earth's depths, predicting novel Pb-S phases: PbS (stable to CMB), PbS₂ (upper mantle solid), and PbS₃ (potential liquid under sulfur-rich conditions).

• CALYPSO predicted structures for Pb_xS_y (x=1-4, y=1-4).
• DFT with VASP used PBE functional and PAW potentials.
• Quasi-harmonic approximation for Gibbs free energies.

Key Findings: PbS₃ and Hidden Mantle Reservoirs

The simulations revealed PbS remains solid across mantle conditions, forming early during planetary differentiation and trapping primordial lead away from decaying parents. In sulfur-enriched regions—plausible given sulfur's abundance—PbS reacts to form polysulfides. PbS₂ stays solid, but PbS₃ melts at lower temperatures, allowing episodic upward migration as melts that 'leak' ancient lead into the crust, matching signatures in ocean island basalts.

These reservoirs explain isotopic heterogeneity without core sequestration, linking mantle redox state and sulfur cycling to Earth's evolution.Read the full Nature Communications paper.

Implications for Earth's Formation and Differentiation

Earth formed 4.5 billion years ago from chondritic material. As it differentiated into core, mantle, and crust, metals like lead partitioned. The NTU model suggests lead-sulfur bonds dominate under reducing mantle conditions, preventing core loss. This refines models of the magma ocean phase, where sulfur influenced metal-silicate partitioning.

Episodic PbS₃ melts could source enriched mantle plumes, explaining hotspots like Hawaii. For planetary science, it predicts similar processes on super-Earths or Venus, where high pressures stabilize exotic minerals.

Photo by Shalone Cason on Unsplash

NTU's Asian School of the Environment: A Research Powerhouse

NTU's Asian School of the Environment (ASE) integrates Earth, atmospheric, and ocean sciences with sustainability. Home to world-class facilities like supercomputing clusters and high-pressure labs, ASE fosters interdisciplinary work. This study exemplifies NTU's investment in computational geodynamics, supported by Singapore's National Research Foundation.

ASE's contributions extend to geothermal mapping in Singapore and paleotsunami research, underscoring NTU's role in addressing regional geohazards.Explore ASE research.

Spotlight on Professor Simon Redfern and the Research Team

Prof. Simon Redfern, Dean of NTU's College of Science and President's Chair in Earth Sciences, brings expertise from Cambridge and extensive high-pressure mineralogy. Co-authors Dr. Siyu Liu (lead author, now independent), Dr. Meng Guo (HKU/NTU), and Dr. Shidong Yu leveraged ASE's computational resources.

"This discovery changes our understanding of planetary chemistry," notes Prof. Redfern. The team's work, published February 18, 2026, in Nature Communications, has garnered global attention, affirming Singapore's talent pipeline in STEM.

Reactions from the Global Scientific Community

Geochemists hail the study as a 'major moment for geology.' Dr. Maya Lagos (ETH Zurich) praises its mechanistic insight over core hypotheses. Posts on platforms like LinkedIn highlight its resolution of the 50-year paradox, with calls for experimental validation using diamond anvil cells.

Singapore's research ecosystem benefits, boosting NTU's QS rankings (11th globally 2026). This positions local graduates for planetary science careers.Phys.org coverage.

Singapore's Investment in Geoscience Research Pays Off

Singapore, despite lacking natural resources, invests heavily in R&D—over S$20 billion annually. NTU receives significant funding via A*STAR and NRF, enabling such breakthroughs. This study exemplifies how public-private partnerships drive high-impact science, training PhDs for global roles.

In higher education, it inspires curricula in computational Earth sciences, aligning with Singapore's Smart Nation initiative.

Future Directions: From Simulations to Lab Confirmation

Next, NTU plans high-pressure experiments to synthesize PbS₃, using synchrotron X-rays for validation. Seismic tomography may detect low-velocity zones signaling these reservoirs. Broader applications include modeling exoplanet interiors and resource exploration (lead in deep crust).

Photo by Alexey Taktarov on Unsplash

• Laboratory synthesis under mantle conditions.
• Seismic imaging of sulfur-enriched zones.
• Comparative studies for Mars/Venus.

Why This Matters for Higher Education in Singapore

NTU's success attracts top talent, with programs like Earth Systems PhD drawing international students. It underscores the value of interdisciplinary training—merging materials science, geochemistry, and computing. For aspiring researchers, opportunities abound in faculty positions and postdocs.NTU research hub.

This positions Singapore universities as leaders in solving grand challenges, from climate to planetary habitability.