...from recent issues of "Science":

(1)  Apr. 26 (pg. 647-8): "Salty water is a comforting home for life today,
but it probably was too harsh for the first cells.  That's the surprising
conclusion of new lab studies, which found that primitive membranes and
chains of basic genetic material assemble far more easily in fresh water.
The research suggests that life arose in ponds on the earliest continents,
rather than in tide pools or the deep sea, as many researchers have
assumed."  This is not good news for the prospects of Europan life, given
the likelihood that its ocean is far brinier than Earth's ocean has ever
been.  (That's especially so when combined with conclusion in Europa Focus
Group that high acidity is also fatally destructive to the initial evolution
of life out of prebiotic molecules.)

(2)  May 10 (pg. 1056-8):  Geologists have "said that 'probably the top few
kilometers of the entire basaltic ocean crust is alive with microbes.'...
The recognition of pervasive, all-enduring life has sparked visions of alien
life just waiting to be found beneath the inhospitable surface of Mars.
Researchers exploring the deep subsurface here on Earth -- continental
crust, marine sediments, and ocean crust -- are not so optimistic, however.
They are finding deep life, but it mostly seems to be living indirectly off
the eenrgy of sunlight rather than using local, less tempting sources of
energy, such as the rock itself.  Even when feeding off organic matter that
trickles down from plant life at the surface, deep microbes are usually
starved into apparent dormancy; when cut off from photosynthetic fuel
supplies, they simply disappear... What deep life they are finding [even
when temperatures allow it] is living 'very, very slowly'. "

(3)  May 24 (pg. 1384-5): "What lingering traces -- a smudged imprint in
rock, an oddly composed bit of organic matter, or distinctively imbalanced
isotopes -- might show that life existed eons before?  For almost two
centuries, paleontologists wrestling with that problem have pushed the
earliest known life back in time... [using] wormy squiggles in the mud and
vanishingly small fossils.  And in the past few years, egged on by a claim
for traces of life in a 4.5-billion-year-old rock from Mars, researchers
have explored new kinds of biomarkers -- molecules and isotopes -- in very
ancient rocks.  But interpreting both new and old kinds of markers has
proven more complicated than many had hoped, and the results have sparked
several heated debates.

"In this issue of 'Science', for example, two geologists challenge a
startling claim for the first signs of life: that the skewed isotopic
composition of graphite in rock from an island off Greenland shows that life
existed 3.85 billion years or more ago, when huge, globe-sterilzing impacts
were still battering the planet.  The debate highlights the growing
realization that as analyses become ever more high-tech, relying on tinier
samples and subtler traces, it becomes more important to understand the
[geological] environment in which a presumed biomarker formed... 'We had a
very optimistic view of how easy it was going to be to recognize the signs
of life,' says meteoriticist Harry McSween... 'We have a lot of work to
do.'...

"Such setbacks are reminding researchers that life usually doesn't leave a
unique trace; in many cases, what organisms do, inorganic chemistry can too.
'It's not enough to say, 'Here's a biomarker that organisms produce", ' says
meteoriticist Ralph Harvey.. 'You have to say, "Here's why it can't be
produced other ways."  That's a much bigger problem.'... 'If the specialists
cannot agree on the quality of evidence from terrestrial rocks,' asks
Queensland's Balz Kamber, 'what hope is there to agree on evidence from tiny
meteoritic fragments or returned samples?'.. [However], with the impetus
from ALH84001 and [an increased] commitment to the interdisciplinary
investigation of geological context, biosignatures could work, researchers
say."

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