a rigid layer of the Earth's crust that is believed to drift slowly
It’s been argued that on the early
Earth, crustal plates, floating on a heat-softened
layer of material beneath, would have
simply been too thick and buoyant to get
dragged beneath each other as they are today.
movement of the edge of one tectonic plate under another
Three components, most agreed,
were key: there must be rigid plates at the surface
of the Earth; those plates must move apart
through ocean spreading, with new crust
being made where the sea floor pulls apart;
and the plates must on occasion dive beneath
of or relating to the earliest known rocks formed during the Precambrian Eon
Most geologists
have never seen a komatiite; they are
found almost exclusively among rocks of the
Archaean era, which are more than 2.5 billion
years old and thus very rare.
a grey tetravalent metallic element that resembles zirconium chemically and is found in zirconium minerals; used in filaments for its ready emission of electrons
The evidence
comes in the form of hafnium isotope ratios in
the zircon crystals, which preserve signals of
the lighter minerals typical of continental crust.
of or relating to or characteristic of the crust of the earth or moon
It’s been argued that on the early
Earth, crustal plates, floating on a heat-softened
layer of material beneath, would have
simply been too thick and buoyant to get
dragged beneath each other as they are today.
a geologist who uses physical principles to study the properties of the earth
But ice floes on a polar sea move in the same
way, points out geophysicist Don Anderson of
the California Institute of Technology in
Pasadena — and those ice floes aren’t experiencing
plate tectonics.
relating to or occurring or living in or frequenting the open ocean
Subduction requires rigid plates, and
as it involves the destruction of crust, new
crust must be created elsewhere, presumably
at oceanic spreading ridges (see graphic); otherwise,
continental crust would eventually disappear.
the process of covering the earth with glaciers or masses of ice
And between 780 million and 580
million years ago, Stern says, there was a series
of glaciations, some very extreme — giving rise
to the term ‘snowball Earth’.
For example, explanations for different
sorts of volcanism in different settings
also explain why the mineral make-up of continental
crust and the crust beneath the oceans
is so different.
pertaining to the structure or movement of the earth's crust
It contains some geochemical
markers that suggest subduction, but they
could just as easily be explained by hot
upwellings of rock known as mantle plumes or
other non-tectonic phenomena.
atom with same atomic number, different number of neutrons
The evidence
comes in the form of hafnium isotope ratios in
the zircon crystals, which preserve signals of
the lighter minerals typical of continental crust.
Three components, most agreed,
were key: there must be rigid plates at the surface
of the Earth; those plates must move apart
through ocean spreading, with new crust
being made where the sea floor pulls apart;
and the plates must on occasion dive b
There are geochemical signatures that
cannot be explained by other factors, and the
Clues to the past: zircon crystals (inset) in the Jack Hills of Western Australia have been used to argue for an early start to plate tectonics.
And the greater temperature of the early Earth’s
innards would probably have made them move
in very different patterns from those typical of
today’s tectonics.
But then along came Julian Pearce of Cardiff
University in Wales, who argued that each of
the geochemical markers in the western Pilbara
can be explained by other phenomena,
such as magmas with an unusual amount of
water in them, or crustal materia
But ice floes on a polar sea move in the same
way, points out geophysicist Don Anderson of
the California Institute of Technology in
Pasadena — and those ice floes aren’t experiencing
plate tectonics.
having undergone transformation by pressure, heat, etc.
Metamorphic
rocks called blueschists, produced by
squeezing the basalt from which oceanic crust
is made at high pressures but not very high
temperatures, are being made in today’s subduction
zones; none, Stern says, has been
found that is more than
He argues that there’s
plenty of evidence for plate tectonics stretching
back at least 3.1 billion years2 — including
geochemical work, seismic images of the
‘sutures’ where colliding continents join and,
indeed, a few ancient ophiolites.
He argues that there’s
plenty of evidence for plate tectonics stretching
back at least 3.1 billion years2 — including
geochemical work, seismic images of the
‘sutures’ where colliding continents join and,
indeed, a few ancient ophiolites.
the act of imitating the behavior of some situation
But new simulations, using more
sophisticated calculations, suggest that the
crust may have been thinner than once
thought3 — as thin as 4 kilometres or less —
which would be thinner than today’s crust.
For example, explanations for different
sorts of volcanism in different settings
also explain why the mineral make-up of continental
crust and the crust beneath the oceans
is so different.
subject to or caused by an earthquake or earth vibration
He argues that there’s
plenty of evidence for plate tectonics stretching
back at least 3.1 billion years2 — including
geochemical work, seismic images of the
‘sutures’ where colliding continents join and,
indeed, a few ancient ophiolites.
The scene brings home the difficulties of trying
to study the early Earth — there aren’t many
old rocks to look at, and those that are around
are often so altered, chemically and physically,
as to be nearly indecipherable.
As
far back as there has been complex life — and
perhaps even before — continents have come
together and moved apart in a dance that has
altered climates and geographies, opening up
new possibilities for life and sometimes closing
down old ones.
tending to float on a liquid or rise in air or gas
It’s been argued that on the early
Earth, crustal plates, floating on a heat-softened
layer of material beneath, would have
simply been too thick and buoyant to get
dragged beneath each other as they are today.
Geoff Davies, a
modeller at Australian National University in
Canberra, presented work suggesting that one
of the biggest stumbling blocks to an early start
may have been removed.
Fragments of zircon crystals dated even earlier
NEWS FEATURE NATURE|Vol 442|13 July 2006
128
Plate tectonics has created oceans and pushed up mountain ranges.
The material left behind as the melt is
creamed off — denser than it was before the
distillation — then detaches itself from the
crust and sinks back into the mantle.
Three components, most agreed,
were key: there must be rigid plates at the surface
of the Earth; those plates must move apart
through ocean spreading, with new crust
being made where the sea floor pulls apart;
and the plates must on occasion dive beneath
An ‘intermittent approach’ would be a wonderful
way to reconcile things — but it takes
geology even further from the comforting
realm of uniformitarianism, into a world
where the most basic principles come and go
in fits and starts.
Three components, most agreed,
were key: there must be rigid plates at the surface
of the Earth; those plates must move apart
through ocean spreading, with new crust
being made where the sea floor pulls apart;
and the plates must on occasion dive b
the degree of hotness or coldness of a body or environment
And the greater temperature of the early Earth’s
innards would probably have made them move
in very different patterns from those typical of
today’s tectonics.
Wilde argues that the zircons
should be interpreted more conservatively
— that the evidence points to there being some
continental crust, but not plate tectonics and its
associated recycling, by 4.4 billion years ago6.
The specific aim of the meeting
was to try to fix a date for the onset of plate
tectonics: the earliest possibility is pretty
much straight after the planet formed, about
4.5 billion years ago; the latest is just
1 billion years ago.
Geoff Davies, a
modeller at Australian National University in
Canberra, presented work suggesting that one
of the biggest stumbling blocks to an early start
may have been removed.
one of the individual parts making up a larger entity
Three components, most agreed,
were key: there must be rigid plates at the surface
of the Earth; those plates must move apart
through ocean spreading, with new crust
being made where the sea floor pulls apart;
and the plates must on occasion dive b
exhibiting the qualities that identify a group or kind
And the greater temperature of the early Earth’s
innards would probably have made them move
in very different patterns from those typical of
today’s tectonics.
On the basis that dramatic effects
require dramatic causes, he argues that the
introduction of plate tectonics, and with it an
increase in planet-cooling volcanic eruptions,
might have precipitated the great glaciations.
On the basis that dramatic effects
require dramatic causes, he argues that the
introduction of plate tectonics, and with it an
increase in planet-cooling volcanic eruptions,
might have precipitated the great glaciations.
The scene brings home the difficulties of trying
to study the early Earth — there aren’t many
old rocks to look at, and those that are around
are often so altered, chemically and physically,
as to be nearly indecipherable.
It contains some geochemical
markers that suggest subduction, but they
could just as easily be explained by hot
upwellings of rock known as mantle plumes or
other non-tectonic phenomena.
a disciple of Saint Paul who became the leader of the Christian community at Ephesus
Timothy Kusky of St Louis University in
Missouri, who led the original study, says that
Zhao took samples from a part of the rock
already known to be much younger than the
main part of the ophiolite.
But new simulations, using more
sophisticated calculations, suggest that the
crust may have been thinner than once
thought3 — as thin as 4 kilometres or less —
which would be thinner than today’s crust.
of or existing within the Arctic or Antarctic Circles
But ice floes on a polar sea move in the same
way, points out geophysicist Don Anderson of
the California Institute of Technology in
Pasadena — and those ice floes aren’t experiencing
plate tectonics.
a fissure in the earth's crust through which gases erupt
In 2001, a
team reported that an ophiolite from Dongwanzi,
China, was 2.5 billion years old — mak-
Subducting oceanic plate
Passive continental
margin (no subduction)
Mantle
upwelling
Oceanic
spreading ridge
Continental
plate
Volcano
THE DRIVING FO
the practical application of science to commerce or industry
But ice floes on a polar sea move in the same
way, points out geophysicist Don Anderson of
the California Institute of Technology in
Pasadena — and those ice floes aren’t experiencing
plate tectonics.
An ‘intermittent approach’ would be a wonderful
way to reconcile things — but it takes
geology even further from the comforting
realm of uniformitarianism, into a world
where the most basic principles come and go
in fits and starts.
changed in form or character without becoming something else
The scene brings home the difficulties of trying
to study the early Earth — there aren’t many
old rocks to look at, and those that are around
are often so altered, chemically and physically,
as to be nearly indecipherable.
Fragments of zircon crystals dated even earlier
NEWS FEATURE NATURE|Vol 442|13 July 2006
128
Plate tectonics has created oceans and pushed up mountain ranges.
But how can that approach hold up when
a science from a world where plate tectonics
explains more or less everything is applied to a
world that may have lacked it?
Hugh
Smithies of the Geological Survey of Western
Australia says that the eastern part of the Pilbara,
between 3.5 billion and 3.2 billion years
old, “shows no clear evidence for modern-style
plate tectonics”.
Last year in Science5, geochemist Mark Harrison
of the University of California, Los Angeles,
and colleagues used the Jack Hills zircons to
argue that continental crust was present 4.4 billion
to 4.5 billion years ago.
a document listing the alternatives that is used in voting
At the end, a closing ballot
showed that many had begun to push their
thinking further back into the past; a majority
of attendees voted for plate tectonics having
started between 3 billion and 4 billion years ago.
But ice floes on a polar sea move in the same
way, points out geophysicist Don Anderson of
the California Institute of Technology in
Pasadena — and those ice floes aren’t experiencing
plate tectonics.
Hugh
Smithies of the Geological Survey of Western
Australia says that the eastern part of the Pilbara,
between 3.5 billion and 3.2 billion years
old, “shows no clear evidence for modern-style
plate tectonics”.
Subduction requires rigid plates, and
as it involves the destruction of crust, new
crust must be created elsewhere, presumably
at oceanic spreading ridges (see graphic); otherwise,
continental crust would eventually disappear.
relation with respect to comparative quantity or magnitude
The evidence
comes in the form of hafnium isotope ratios in
the zircon crystals, which preserve signals of
the lighter minerals typical of continental crust.
In 2001, a
team reported that an ophiolite from Dongwanzi,
China, was 2.5 billion years old — mak-
Subducting oceanic plate
Passive continental
margin (no subduction)
Mantle
upwelling
Oceanic
spreading ridge
Continental
plate
Volcano
THE DRIVING FO
The scene brings home the difficulties of trying
to study the early Earth — there aren’t many
old rocks to look at, and those that are around
are often so altered, chemically and physically,
as to be nearly indecipherable.
Subduction requires rigid plates, and
as it involves the destruction of crust, new
crust must be created elsewhere, presumably
at oceanic spreading ridges (see graphic); otherwise,
continental crust would eventually disappear.
In a paper published last year,
he took an extreme position, proposing that
Earth has been free of plate tectonics for
almost four-fifths of its life, with the system we
see today starting up only a billion years ago1.
be on or below a liquid surface and not sink to the bottom
It’s been argued that on the early
Earth, crustal plates, floating on a heat-softened
layer of material beneath, would have
simply been too thick and buoyant to get
dragged beneath each other as they are today.
It contains some geochemical
markers that suggest subduction, but they
could just as easily be explained by hot
upwellings of rock known as mantle plumes or
other non-tectonic phenomena.
Since the
early nineteenth century, geology has been
ruled by the principle of uniformitarianism —
that the planet operates on unchanging laws,
and that the present can be used as a key to the
past.
The problem is that Earth could display one
or even two of these properties without necessarily
having a system like that described by
modern plate tectonics (see ‘A world without
tectonics’).
a branch of study or knowledge involving the observation, investigation, and discovery of general laws or truths that can be tested systematically
But how can that approach hold up when
a science from a world where plate tectonics
explains more or less everything is applied to a
world that may have lacked it?
Since the
early nineteenth century, geology has been
ruled by the principle of uniformitarianism —
that the planet operates on unchanging laws,
and that the present can be used as a key to the
past.
Most geologists
have never seen a komatiite; they are
found almost exclusively among rocks of the
Archaean era, which are more than 2.5 billion
years old and thus very rare.
Most geologists
have never seen a komatiite; they are
found almost exclusively among rocks of the
Archaean era, which are more than 2.5 billion
years old and thus very rare.
It contains some geochemical
markers that suggest subduction, but they
could just as easily be explained by hot
upwellings of rock known as mantle plumes or
other non-tectonic phenomena.
Today, Earth’s interior is too
cool to produce this particular rock; 2.7 billion
years ago, the hot lava would have run like
water over the barren landscapes.
Wilde argues that the zircons
should be interpreted more conservatively
— that the evidence points to there being some
continental crust, but not plate tectonics and its
associated recycling, by 4.4 billion years ago6.
the boundary line or area immediately inside the boundary
In 2001, a
team reported that an ophiolite from Dongwanzi,
China, was 2.5 billion years old — mak-
Subducting oceanic plate
Passive continental
margin (no subduction)
Mantle
upwelling
Oceanic
spreading ridge
Continental
plate
Volcano
THE DRIVING FO
Subduction requires rigid plates, and
as it involves the destruction of crust, new
crust must be created elsewhere, presumably
at oceanic spreading ridges (see graphic); otherwise,
continental crust would eventually disappear.
An ‘intermittent approach’ would be a wonderful
way to reconcile things — but it takes
geology even further from the comforting
realm of uniformitarianism, into a world
where the most basic principles come and go
in fits and starts.
The material left behind as the melt is
creamed off — denser than it was before the
distillation — then detaches itself from the
crust and sinks back into the mantle.
There are geochemical signatures that
cannot be explained by other factors, and the
Clues to the past: zircon crystals (inset) in the Jack Hills of Western Australia have been used to argue for an early start to plate tectonics.
And the greater temperature of the early Earth’s
innards would probably have made them move
in very different patterns from those typical of
today’s tectonics.
For a while
two independent groups have been quietly
warring over the significance of a pile of
ancient zircons from the Jack Hills region of
Western Australia.
At the end, a closing ballot
showed that many had begun to push their
thinking further back into the past; a majority
of attendees voted for plate tectonics having
started between 3 billion and 4 billion years ago.
The material left behind as the melt is
creamed off — denser than it was before the
distillation — then detaches itself from the
crust and sinks back into the mantle.
He argues that there’s
plenty of evidence for plate tectonics stretching
back at least 3.1 billion years2 — including
geochemical work, seismic images of the
‘sutures’ where colliding continents join and,
indeed, a few ancient ophiolites.
a machine for performing calculations automatically
In the early 1990s,
computer models created by Davies and others
suggested that the crust on the early Earth
would have been too thick and buoyant to get
dragged down beneath another plate during
subduction.
The specific aim of the meeting
was to try to fix a date for the onset of plate
tectonics: the earliest possibility is pretty
much straight after the planet formed, about
4.5 billion years ago; the latest is just
1 billion years ago.
Since the
early nineteenth century, geology has been
ruled by the principle of uniformitarianism —
that the planet operates on unchanging laws,
and that the present can be used as a key to the
past.
As
far back as there has been complex life — and
perhaps even before — continents have come
together and moved apart in a dance that has
altered climates and geographies, opening up
new possibilities for life and sometimes closing
down old ones.
For a while
two independent groups have been quietly
warring over the significance of a pile of
ancient zircons from the Jack Hills region of
Western Australia.
Today, Earth’s interior is too
cool to produce this particular rock; 2.7 billion
years ago, the hot lava would have run like
water over the barren landscapes.
It’s been argued that on the early
Earth, crustal plates, floating on a heat-softened
layer of material beneath, would have
simply been too thick and buoyant to get
dragged beneath each other as they are today.
keep in safety and protect from harm, loss, or destruction
The evidence
comes in the form of hafnium isotope ratios in
the zircon crystals, which preserve signals of
the lighter minerals typical of continental crust.
something intended to communicate a particular impression
The problem is that Earth could display one
or even two of these properties without necessarily
having a system like that described by
modern plate tectonics (see ‘A world without
tectonics’).
a custom that has been an important feature of some group
Geophysicist Paul Silver, of the Carnegie
Institution of Washington, raised the notion
that plate tectonics may have started and
stopped several times during Earth’s history.
after an unspecified period of time or a long delay
Subduction requires rigid plates, and
as it involves the destruction of crust, new
crust must be created elsewhere, presumably
at oceanic spreading ridges (see graphic); otherwise,
continental crust would eventually disappear.
Evidence
for the earlier style, he says, comes from
minerals that are typical of higher-temperature,
lower-pressure environments; these suggest
a hotter Earth where plates did not
subduct beneath each other to great depths
and pressures.
The problem is that Earth could display one
or even two of these properties without necessarily
having a system like that described by
modern plate tectonics (see ‘A world without
tectonics’).
the opposition or dissimilarity of things that are compared
In contrast, looking at the western part of the
Pilbara — which is 3.3 billion to 3.0 billion years
old — Smithies sees plenty of evidence for plate
tectonics.
Geophysicist Paul Silver, of the Carnegie
Institution of Washington, raised the notion
that plate tectonics may have started and
stopped several times during Earth’s history.
take something away as by lifting, pushing, or taking off
Geoff Davies, a
modeller at Australian National University in
Canberra, presented work suggesting that one
of the biggest stumbling blocks to an early start
may have been removed.
The evidence
comes in the form of hafnium isotope ratios in
the zircon crystals, which preserve signals of
the lighter minerals typical of continental crust.
the weather in some location averaged over a period of time
As
far back as there has been complex life — and
perhaps even before — continents have come
together and moved apart in a dance that has
altered climates and geographies, opening up
new possibilities for life and sometimes closing
down old ones.
He argues that there’s
plenty of evidence for plate tectonics stretching
back at least 3.1 billion years2 — including
geochemical work, seismic images of the
‘sutures’ where colliding continents join and,
indeed, a few ancient ophiolites.
something a little different from others of the same type
In a paper in press in Geology8, Brown
suggests that there have been two styles of
plate tectonics: the modern kind that we see
today, and an earlier version that lasted from
about 2.7 billion to 700 million years ago.
Smithies thinks the
western Pilbara contains the remains of an
oceanic arc — the sort of line of islands, such as
the Aleutians of Alaska, that are characteristic
of some oceanic subduction zones7.
He argues that there’s
plenty of evidence for plate tectonics stretching
back at least 3.1 billion years2 — including
geochemical work, seismic images of the
‘sutures’ where colliding continents join and,
indeed, a few ancient ophiolites.
For a while
two independent groups have been quietly
warring over the significance of a pile of
ancient zircons from the Jack Hills region of
Western Australia.
the state of needing something that is absent or unavailable
But how can that approach hold up when
a science from a world where plate tectonics
explains more or less everything is applied to a
world that may have lacked it?
Most geologists
have never seen a komatiite; they are
found almost exclusively among rocks of the
Archaean era, which are more than 2.5 billion
years old and thus very rare.
Geophysicist Paul Silver, of the Carnegie
Institution of Washington, raised the notion
that plate tectonics may have started and
stopped several times during Earth’s history.
For a while
two independent groups have been quietly
warring over the significance of a pile of
ancient zircons from the Jack Hills region of
Western Australia.
Fragments of zircon crystals dated even earlier
NEWS FEATURE NATURE|Vol 442|13 July 2006
128
Plate tectonics has created oceans and pushed up mountain ranges.
Most geologists
have never seen a komatiite; they are
found almost exclusively among rocks of the
Archaean era, which are more than 2.5 billion
years old and thus very rare.
An ‘intermittent approach’ would be a wonderful
way to reconcile things — but it takes
geology even further from the comforting
realm of uniformitarianism, into a world
where the most basic principles come and go
in fits and starts.
Geoff Davies, a
modeller at Australian National University in
Canberra, presented work suggesting that one
of the biggest stumbling blocks to an early start
may have been removed.
a process of becoming larger or longer or more numerous
On the basis that dramatic effects
require dramatic causes, he argues that the
introduction of plate tectonics, and with it an
increase in planet-cooling volcanic eruptions,
might have precipitated the great glaciations.
an item of information that is typical of a class or group
For instance, another Australian geologist
presented seemingly convincing evidence that
plate tectonics had begun by 3.3 billion years
ago in Western Australia, based on the very
different histories of two sections of an ancient
rock formation call
In a paper published last year,
he took an extreme position, proposing that
Earth has been free of plate tectonics for
almost four-fifths of its life, with the system we
see today starting up only a billion years ago1.
similar things placed in order or one after another
And between 780 million and 580
million years ago, Stern says, there was a series
of glaciations, some very extreme — giving rise
to the term ‘snowball Earth’.
having the same or nearly the same characteristics
The data also suggest, Harrison argues, that
that crust was being recycled down into the
mantle by 4.4 billion years ago — perhaps
though a process similar to plate tectonics.
Three components, most agreed,
were key: there must be rigid plates at the surface
of the Earth; those plates must move apart
through ocean spreading, with new crust
being made where the sea floor pulls apart;
and the plates must on occasion dive b
The specific aim of the meeting
was to try to fix a date for the onset of plate
tectonics: the earliest possibility is pretty
much straight after the planet formed, about
4.5 billion years ago; the latest is just
1 billion years ago.
In 2001, a
team reported that an ophiolite from Dongwanzi,
China, was 2.5 billion years old — mak-
Subducting oceanic plate
Passive continental
margin (no subduction)
Mantle
upwelling
Oceanic
spreading ridge
Continental
plate
Volcano
THE DRIVING FO
Since the
early nineteenth century, geology has been
ruled by the principle of uniformitarianism —
that the planet operates on unchanging laws,
and that the present can be used as a key to the
past.
the content of observation or participation in an event
But ice floes on a polar sea move in the same
way, points out geophysicist Don Anderson of
the California Institute of Technology in
Pasadena — and those ice floes aren’t experiencing
plate tectonics.
Geophysicist Paul Silver, of the Carnegie
Institution of Washington, raised the notion
that plate tectonics may have started and
stopped several times during Earth’s history.
a phenomenon that is caused by some previous phenomenon
On the basis that dramatic effects
require dramatic causes, he argues that the
introduction of plate tectonics, and with it an
increase in planet-cooling volcanic eruptions,
might have precipitated the great glaciations.
Hugh
Smithies of the Geological Survey of Western
Australia says that the eastern part of the Pilbara,
between 3.5 billion and 3.2 billion years
old, “shows no clear evidence for modern-style
plate tectonics”.
Created on Sun Nov 06 11:23:21 EST 2011
(updated Sun Nov 06 11:23:42 EST 2011)
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