Ice cycles may have driven the emergence of the first cells on early Earth

Lago congelado

Lago congelado - andriipiskarov/ shutterstock.com

Pesquisadores of Instituto of Ciências of Terra and Vida (ELSI) in Tóquio discovered evidence that icy environments may have played a crucial role in the emergence of the first cellular structures. Experimentos simulating conditions of primitive Terra show that repeated cycles of freezing and thawing favored the fusion of primitive molecular compartments and the retention of DNA. The study opens new perspectives on how complex life may have evolved from extremely simple systems.

The research focused on lipid vesicles — small bubbles formed by fatty membranes — and how different chemical compositions affected their behavior under heat stress. Descobertas indicate that more fluid membranes, with a greater degree of lipid unsaturation, facilitated the fusion of compartments and the mixing of essential molecules. Esse process would have created environments conducive to complex chemical reactions in the early days of the planet.

Protocélulas constructed with different lipid compositions

The team of researchers created small spherical compartments called large unilamellar vesicles (LUVs) using three different types of phospholipids. Cada type had distinct structural features that influenced the behavior of the membranes.

  • POPC(1-palmitoyl-2-oleoyl-glycero-3-phosphocholine): an unsaturated acyl chain with a single double bond, producing more rigid membranes
  • PLPC(1-palmitoyl-2-linoleoyl-sn-glycero-3-phosphocholine): an unsaturated acyl chain with two double bonds, generating greater fluidity
  • DOPC(1,2-di-oleoyl-sn-glycero-3-phosphocholine): two unsaturated acyl chains, each with a double bond, providing maximum fluidity

Segundo Tatsuya Shinoda, PhD student at ELSI and lead author of the work, the choice of phosphatidylcholine as a membrane component was due to its structural continuity with modern cells, potential availability in prebiotic conditions and ability to retain essential contents. Essas molecules, although similar in appearance, differ in subtle but significant aspects that determine the flexibility of the structures.

Fusão and growth driven by freeze cycles

The researchers exposed the vesicles to repeated cycles of freezing and thawing, simulating temperature variations that occurred in the primitive Terra. Após only three cycles, clear differences emerged between compartments. Vesículas rich in POPC grouped together without completely merging, maintaining their original structure. In contrast, those containing PLPC or DOPC merged into significantly larger compartments. Quanto, the higher the concentration of PLPC present in the membrane, the greater the probability of fusion and growth of the structures.

Esse behavior highlights the fundamental role of membrane chemistry in the evolution of protocells. Lipídios with more unsaturated bonds makes the membranes less compact and structurally more flexible. Natsumi Noda, an ELSI researcher, observed that under the stress of ice crystal formation, membranes can become unstable or fragmented, requiring structural reorganization after thawing. The less compact lateral organization, resulting from the greater degree of unsaturation, exposes more hydrophobic regions during membrane reconstruction, facilitating interactions with adjacent vesicles and making fusion energetically favorable.

Captura and retention of genetic material

Compartment fusion is especially important because it allows the contents of separate vesicles to mix. Na Terra primitive, where organic molecules were dispersed in the environment, this type of mixture could have brought together essential ingredients for more complex chemical reactions. The team also tested the vesicles’ ability to capture and retain DNA, comparing structures made entirely from POPC with those made from PLPC. The results showed that PLPC vesicles captured DNA with greater efficiency, even before freezing and thawing cycles. Após repeated cycles continued to retain significantly more genetic material than POPC vesicles, suggesting that the lipid composition not only favored fusion but also protected important molecules.

Ambientes ice cream as the cradle of life

Tradicionalmente, scientists have focused on environments such as land-based ice pools or underwater hydrothermal vents as possible places of origin of life. Este study adds different perspective, suggesting that large-scale icy environments also played a significant role. In primitive Na Terra, freeze-thaw cycles could have occurred repeatedly over extensive geological periods. As the water froze, expanding ice crystals pushed dissolved molecules into the remaining liquid, concentrating them in small spaces. Esse process would increase the probability of interactions between molecules and vesicles, creating an environment conducive to prebiotic chemistry.

Simultaneamente, membranes composed of more unsaturated phospholipids would be more prone to fusion, promoting the mixing of different contents. Existe, however, an important counterpart. Embora fluid membranes favor fusion, they can also become unstable during stress induced by freezing and thawing, leading to leaks that compromise the retention of essential molecules. Para the primitive protocells, maintaining balance between structural stability and permeability would have been absolutely crucial for their survival and continued evolution.

The path to the first complex cells

Tomoaki Matsuura, ELSI professor and principal investigator of the study, suggests that a recursive selection of grown vesicles induced by freezing and thawing over successive generations could have been accomplished by integrating fission mechanisms such as osmotic pressure or mechanical shear. With increasing molecular complexity, the intravesicular system — that is, the function encoded by genes — could ultimately take control of protocellular fitness. Isso would lead to the emergence of a primordial cell capable of Darwinian evolution. The most successful membrane compositions likely depended on the specific environmental conditions at each place of origin of life.

Taken together, the findings suggest that simple physical processes such as freezing and thawing may have helped guide the transition from basic molecular compartments to the first evolving cells. The research not only provides a clearer answer to the centuries-old question of how life began, but also demonstrates that extreme environments may have been a catalyst for biological complexity, opening new lines of investigation into the resilience of primitive molecular structures.