270 points by speckx 5 days ago | 111 comments | View on ycombinator
nilkn 5 days ago |
buildsjets 5 days ago |
https://maps.app.goo.gl/pJYr6qiZnMdVwLJS6
stymaar 5 days ago |
accrual 5 days ago |
This has me excited for missions to Europa and Enceladus. Vast quantities of tidal energy flexing unseen ocean floors for millennia is bound to produce some interesting chemistry, if not life.
contingencies 5 days ago |
Theory on the emergence of photosynthesis whereby chlorophyll-like structures first evolved from harvesting heat rather than light: https://www.inaturalist.org/journal/mjpapay/45240-the-first-...
emsign 5 days ago |
MarkusQ 5 days ago |
The disequilibrium (sugars and free O₂) were produced by living organisms, and this is just the gradual drift back to a lower energy state. CO₂ is common in the universe, and not at all a sign of life. O₂ and sugars are rare.
greenbit 5 days ago |
georgecmu 4 days ago |
The present study challenges the traditional view that the *respiration of
organic carbon to CO2* is an exclusively intracellular process, revealing that
*organic compound respiration can occur spontaneously in an extracellular
context in soils*.
On the surface, it looks like they rediscovered that oxidation of organic / carbonaceous compounds occurs at low temperatures independently of presence of living organisms. The real contribution of the paper would be in elucidation of the specific mechanisms of oxidation of these organic compounds (e.g. via abiotic catalysis).Compare to this paper from 2003:
https://sci-hub.kvnp.top/10.1016/s0360-1285(03)00042-x
Coal oxidation at low temperatures is the major heat source responsible for
the self-heating and spontaneous combustion of coal and is an important source
of greenhouse gas emissions. This review focuses on the chemical reactions
occurring during low-temperature oxidation of coal. Current understanding
indicates that this process involves consumption of O2, formation of solid
oxygenated complexes, thermal decomposition of solid oxygenated complexes and
generation of gaseous oxidation products. Parameters, such as mass change,
heat release, oxygen consumption, and formation of oxidation products in the
gas or solid phase, have been used to qualitatively and quantitatively
describe the oxidation process. Reaction mechanisms have been proposed to
explain the characteristics of consumption of O2, and formation of oxidation
products in the gas and solid phases. Various kinetic models have also been
developed to describe the rate of oxygen consumption and the rates of
formation of gaseous oxidation products in terms of the rate parameters of the
relevant reactions, oxidation time, temperature, and initial concentration of
oxygen in the oxidising medium.metalman 5 days ago |
FjordWarden 5 days ago |
ps3udo 4 days ago |
Shitty-kitty 5 days ago |
j16sdiz 5 days ago |
mparramon 5 days ago |
BigTTYGothGF 5 days ago |
rbanffy 4 days ago |
trentnix 5 days ago |
Then the Lord God formed a man from the dust of the ground and breathed into his nostrils the breath of life, and the man became a living being.
JackFr 5 days ago |
nelox 5 days ago |
foota 5 days ago |
pslab 5 days ago |
bitwize 5 days ago |
I like to think of the Earth as a supercomputer running a vast self-interactive chemical computation of unfathomable scale for an unfathomably long amount of time. In this view, the Earth is roughly a ~10^38 ops/sec dissipative self-modifying search engine, of which life captures roughly ~10^35 ops/sec into metabolism, heredity, ecological competition, and evolutionary search. Once proper biological evolution kicked in, with some bumps along the road, it has had a general tendency to reallocate that immense compute capacity in a way that increases search adaptivity per joule by finding and stacking "search accelerators" (prebiotic geochemistry/biochemistry, replicators, cells, DNA/RNA/protein systems, mitochondria, sexual reproduction, multicellularity, nervous systems, intelligence / brains, language / culture, science / technology, ?).