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8 results for "iron-sulfur catalysis"
Q_4_20 — Catalysis: From Haber-Bosch to Asymmetric Synthesis
Catalysis — the acceleration of a chemical reaction by a substance (the catalyst) that is not consumed in the process — accounts for over 90% of all industrial chemical processes and has earned more Nobel Prizes than any
INTERDOC_61 — Hydrothermal Vent Chemistry: From Abiogenesis to Modern Energy Technology
Life originated at alkaline hydrothermal vents where serpentinization of olivine produced hydrogen, heat, and a natural pH gradient across porous iron-sulfur mineral membranes — structurally identical to the proton-motiv
G_3_05 — Self-Organization and Emergence
Self-organization is the process by which global order arises from local interactions among components of an initially disordered system, without external direction or centralized control. Emergence is the closely relate
G_3_13 — Self-Organization from Atoms to Civilizations
Self-organization is the process by which ordered, complex structures emerge spontaneously from simpler components without centralized control or external direction — driven by local interactions among parts that collect
R_1_01 — Abiogenesis & Origin of Life Theories
Abiogenesis — the emergence of life from non-living chemistry — remains one of the deepest unsolved problems in science. The oldest confirmed microfossils date to ~3.5 billion years ago (Pilbara, Western Australia), with
R_1_05 — Quantum Biology
Until recently, quantum effects were thought impossible in warm, wet biological systems. The standard assumption held that thermal noise at physiological temperatures (~310 K) would destroy quantum coherence within femto
R_1_15 — The Chirality Problem: Why Life Uses Left-Handed Amino Acids
One of the deepest unsolved problems in the origin of life is homochirality — the fact that all known life on Earth uses almost exclusively L-amino acids (left-handed) for proteins and D-sugars (right-handed) for nucleic
R_1_19 — Deep-Sea Hydrothermal Vent Origin of Life
The deep-sea hydrothermal vent hypothesis for the origin of life proposes that life on Earth began at submarine hydrothermal systems — either high-temperature black smoker vents (>350°C, acidic, rich in transition metals
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