Showing posts with label isotope. Show all posts
Showing posts with label isotope. Show all posts

Friday, August 07, 2026

A Magnetic Clue to Life’s Origins Chemistry

Amazing stuff!

"... Their study, recently published in Chem, offers a possible missing link in a theory proposing that life first emerged on magnetic surfaces, such as the beds of shallow lakes rich in magnetic minerals. ...

an experiment ... used right- and left-handed versions of methionine – an amino acid that typically initiates protein synthesis – and passed a solution containing this amino acid through a paper filter embedded with micron-sized magnetic particles.

To track the molecules, the researchers incorporated two carbon isotopes – atoms of the same element with different weights – into the amino acid.
In some experiments, right-handed molecules contained the more common, lighter carbon-12 isotope and left-handed ones the heavier carbon-13;
in others, the assignment was reversed. The direction of magnetization was also switched: In different iterations of the experiment, the magnets first pointed toward the solution with one of their poles, north or south, then with the other. After filtering the solution, the scientists used mass spectrometry to measure the ratio of isotopes and the balance between the two chiral forms.

The result was unexpected. The magnetic filter appeared to separate methionine not only by chirality but also by isotope composition. Molecules containing the heavier carbon isotope – regardless of their handedness – showed a stronger attraction to particles magnetized in one direction over the other. ..."

From the highlights and abstract:
"The bigger picture
Isotopic fractionation in biomolecules provides key insight into chemical and biochemical formation pathways, yet the mechanisms underlying isotope selectivity in chiral molecular systems remain poorly understood.
This work demonstrates a direct experimental connection between spin-dependent interactions and isotopic effects in a chiral amino acid, showing that molecules differing only in their carbon isotope composition interact differently with oppositely magnetized surfaces. These findings reveal a previously unexplored contribution of electronic spin polarization to isotopic behavior in molecular systems.
More broadly, the results introduce spin selectivity as a new physical dimension in isotope chemistry.
In the longer term, such spin- and chirality-dependent interactions may enable new approaches for isotope discrimination or separation in chiral chemical environments, with potential relevance to analytical chemistry and materials design.
By linking magnetic interactions, molecular chirality, and isotope effects, this study establishes a framework for investigating how subtle spin-mediated processes can influence isotopic outcomes in complex molecular systems.

Highlights
• Spin-polarized magnetic filters induce carbon isotope fractionation in L-methionine
• Volume-resolved elution reveals metastable spin-dependent interactions
• Chirality couples electronic spin selectivity to isotope chemistry
• Spin-dependent effects may shape isotopic signatures in early biomolecules

Summary
Distinct isotopic fractionation in biomolecules, compared with atmospheric values, reflects their biosynthetic origin.
Monitoring these fractionation changes offers a valuable approach for probing early metabolic networks.
A key question in the study of life’s origins is the role of electronic spin and magnetic surfaces in symmetry breaking and the emergence of homochirality.
Here, we used magnetic filters to show that the dynamical interaction with the magnetic surfaces changes the isotope fractions of 13C L-methionine compared with 12C L-methionine.
Specifically, mass spectrometry analysis reveals that the isotopic fractionation of both natural and ¹³C-enriched L-methionine is influenced by electron spin-dependent interactions."

A Magnetic Clue to Life’s Origins - Chemistry | Weizmann Wonder Wander - News, Features and Discoveries "Study suggests that magnetic surfaces may influence not only the handedness of biological molecules but also their isotope composition – thus connecting two fundamental fingerprints of life"

Spin-dependent isotopic fractionation of L-methionine (no public access, appeared in March 2026)


Graphical abstract


Tuesday, January 27, 2026

143–million-year seawater osmium (Os) isotopic record

Amazing stuff!

"One underused isotopic tracker is osmium, a dense, rare, and stable metal. The ratio between different osmium isotopes in seawater depends on how much of the metal leached out from the continents, the mantle, or even extraterrestrial sources such as asteroids, at any given time. To better understand osmium, a team of researchers collected and analyzed rocks containing the element from the Mid-Pacific Mountains, the Indian Ocean, and central Italy. They then combined these and existing data to reconstruct an isotopic record of osmium from the present all the way back to the Cretaceous, when dinosaurs roamed the Earth.

The record clearly tracks large-scale changes to Earth, such as when the Atlantic Ocean opened up, when the Himalaya mountains formed, and when the planet became covered with ice. It also followed less flashy changes, like the supercontinent Gondwana slowly weathering. ..."

From the editor's summary and abstract:
"Editor’s summary
Osmium occurs in Earth’s crust at the low, low rate of 50 parts per trillion. Even so, its isotopes are sensitive measures of environmental change over Earth’s history because they get variably transferred to seawater through volcanoes, rivers, and even extraterrestrial impacts. Matsumoto et al. collected 187Os/188Os data from outcrops in Italy and deep-sea cores in the Pacific and Indian oceans.
They compiled these with existing data to make a highly resolved marine osmium-isotopic record over the past 143 million years. The record shows cycles related to large Cretaceous eruptions, opening of the Atlantic Ocean, and changing Cenozoic climate. ...

Abstract
Tectonic events and volcanic pulses forming large igneous provinces (LIPs) have altered Earth’s paleoclimate. Osmium (Os) and strontium (Sr) isotopic ratios are key tracers of past continental weathering and LIP eruptions. However, limited Cretaceous seawater Os and riverine Os–Sr data have hindered quantitative reconstructions.
In this study, we present a long-term Os isotopic record from the Cretaceous to the present, revealing ~10– to 20–million-year cycles during the Cretaceous that align with rhythmic LIP eruptions.
Seawater Os–Sr isotopic trends indicate transitions in continental weathering patterns during the Late Cretaceous [~90 million years ago (Ma)] and Paleogene (~35 Ma) ascribed to intensified weathering of interior Gondwana during the opening of the Atlantic Ocean and the uplift and glaciation of the Himalaya, respectively.
Our Os isotopic record highlights its utility in tracing long-term LIP cycles and identifying major paleogeographic turning points."

ScienceAdviser