Today's Antarctic region once as hot as California, Florida

From Yale University, where that means that even though Earth 40-50 million years ago had a completely different arrangement of continents and climate, it still somehow will “underscore the potential for increased warmth at Earth’s poles and the associated risk of melting polar ice and rising sea levels”. Note that in this paleoreconstruction below, there is still a southern ice cap.

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The PR reads:  Parts of ancient Antarctica were as warm as today’s California coast, and polar regions of the southern Pacific Ocean registered 21st-century Florida heat, according to scientists using a new way to measure past temperatures.

The findings, published the week of April 21 in the Proceedings of the National Academy of Sciences, underscore the potential for increased warmth at Earth’s poles and the associated risk of melting polar ice and rising sea levels, the researchers said.

Led by scientists at Yale, the study focused on Antarctica during the Eocene epoch, 40-50 million years ago, a period with high concentrations of atmospheric CO2 and consequently a greenhouse climate. Today, Antarctica is year-round one of the coldest places on Earth, and the continent’s interior is the coldest place, with annual average land temperatures far below zero degrees Fahrenheit.

But it wasn’t always that way, and the new measurements can help improve climate models used for predicting future climate, according to co-author Hagit Affek of Yale, associate professor of geology & geophysics.

“Quantifying past temperatures helps us understand the sensitivity of the climate system to greenhouse gases, and especially the amplification of global warming in polar regions,” Affek said.

The paper’s lead author, Peter M.J. Douglas, performed the research as a graduate student in Affek’s Yale laboratory. He is now a postdoctoral scholar at the California Institute of Technology. The research team included paleontologists, geochemists, and a climate physicist.

By measuring concentrations of rare isotopes in ancient fossil shells, the scientists found that temperatures in parts of Antarctica reached as high as 17 degrees Celsius (63F) during the Eocene, with an average of 14 degrees Celsius (57F) — similar to the average annual temperature off the coast of California today.

Eocene temperatures in parts of the southern Pacific Ocean measured 22 degrees Centigrade (or about 72F), researchers said — similar to seawater temperatures near Florida today.

Today the average annual South Pacific sea temperature near Antarctica is about 0 degrees Celsius.

These ancient ocean temperatures were not uniformly distributed throughout the Antarctic ocean regions — they were higher on the South Pacific side of Antarctica — and researchers say this finding suggests that ocean currents led to a temperature difference.

“By measuring past temperatures in different parts of Antarctica, this study gives us a clearer perspective of just how warm Antarctica was when the Earth’s atmosphere contained much more CO2 than it does today,” said Douglas. “We now know that it was warm across the continent, but also that some parts were considerably warmer than others. This provides strong evidence that global warming is especially pronounced close to the Earth’s poles. Warming in these regions has significant consequences for climate well beyond the high latitudes due to ocean circulation and melting of polar ice that leads to sea level rise.”

To determine the ancient temperatures, the scientists measured the abundance of two rare isotopes bound to each other in fossil bivalve shells collected by co-author Linda Ivany of Syracuse University at Seymour Island, a small island off the northeast side of the Antarctic Peninsula. The concentration of bonds between carbon-13 and oxygen-18 reflect the temperature in which the shells grew, the researchers said. They combined these results with other geo-thermometers and model simulations.

The new measurement technique is called carbonate clumped isotope thermometry.

“We managed to combine data from a variety of geochemical techniques on past environmental conditions with climate model simulations to learn something new about how the Earth’s climate system works under conditions different from its current state,” Affek said. “This combined result provides a fuller picture than either approach could on its own.”

###

The paper is titled:

Pronounced zonal heterogeneity in Eocene southern high-latitude sea surface temperatures.

Significance

Reconstructions of ancient high-latitude climates can help to constrain the amplification of global warming in polar environments. Climate models cannot reproduce the elevated high-latitude temperature estimates in the Eocene epoch, possibly indicating problems in simulating polar climate change. Widely divergent near-Antarctic Eocene sea surface temperature (SST) estimates, however, question the evidence for extreme warmth. Our analysis of multiple temperature proxies near the Antarctic Peninsula improves intersite comparisons and indicates a substantial zonal SST gradient between the southwest Pacific and South Atlantic. Simulations of Eocene ocean temperatures imply that the formation of deep water in the southwest Pacific partly accounts for this SST gradient, suggesting that climate models underestimate Eocene SSTs in regions where the thermohaline circulation leads to relatively high temperatures.

Abstract

Paleoclimate studies suggest that increased global warmth during the Eocene epoch was greatly amplified at high latitudes, a state that climate models cannot fully reproduce. However, proxy estimates of Eocene near-Antarctic sea surface temperatures (SSTs) have produced widely divergent results at similar latitudes, with SSTs above 20 °C in the southwest Pacific contrasting with SSTs between 5 and 15 °C in the South Atlantic. Validation of this zonal temperature difference has been impeded by uncertainties inherent to the individual paleotemperature proxies applied at these sites. Here, we present multiproxy data from Seymour Island, near the Antarctic Peninsula, that provides well-constrained evidence for annual SSTs of 10–17 °C (1σ SD) during the middle and late Eocene. Comparison of the same paleotemperature proxy at Seymour Island and at the East Tasman Plateau indicate the presence of a large and consistent middle-to-late Eocene SST gradient of ∼7 °C between these two sites located at similar paleolatitudes. Intermediate-complexity climate model simulations suggest that enhanced oceanic heat transport in the South Pacific, driven by deep-water formation in the Ross Sea, was largely responsible for the observed SST gradient. These results indicate that very warm SSTs, in excess of 18 °C, did not extend uniformly across the Eocene southern high latitudes, and suggest that thermohaline circulation may partially control the distribution of high-latitude ocean temperatures in greenhouse climates. The pronounced zonal SST heterogeneity evident in the Eocene cautions against inferring past meridional temperature gradients using spatially limited data within given latitudinal bands.

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April 22, 2014 12:07 am

That’s old news. I read a report 20 years ago they found dinosaur fossils under 10,000 feet of ice. The Med Sea was a desert 5 million years ago.
Someone didn’t do their pre-research, literature research and abstract research to Sherlock Holmes detail.

ren
April 22, 2014 12:13 am
norah4you
April 22, 2014 12:19 am

Hm.. as Paul Pierett say above That’s old news” I am 64 years old. When I was in 6th grade long ago that’s was to be read in books we had….
Bye the way – under the ice sheet there is a large sea with open water….
When do they ever learn? The so called experts and scholars of today…

ren
April 22, 2014 12:22 am

Does not apply to now because the Antarctic ice sheet is a record.
http://arctic.atmos.uiuc.edu/cryosphere/antarctic.sea.ice.interactive.html

bushbunny
April 22, 2014 1:02 am

Antarctica was part of Gonnawana land before the continents separated. Sorry about the spelling, I am tired. And it ain’t news.

Twobob
April 22, 2014 1:14 am

Chill Man!
Antarctica was hot now it’s cool.
Its just drift in around.

george e. smith
April 22, 2014 1:20 am

I see that their earth has zero axis tilt back then; and of course all the land masses are in different places.
They don’t say what the Temperatures were like back then in California, and Florida.
When earth gets back to those conditions, we will probably have to live in some different places.
I don’t mind moving.
Nyquist is having an epileptic seizure, while contemplating their global sampling methodology.

SAMURAI
April 22, 2014 1:48 am

Hmmmmm… Perhaps that piece of Earth’s crust where they took the shell samples was positioned in a warm area of the globe 60 million years ago, but the real question is WHERE was that piece of crust located 60 million years ago….
If it was located on the same latitude as Brazil is now, who cares?….
Paleoclimatology research, like real estate, is all about three things: location, location, location. If it’s in the wrong location, it isn’t worth much…

April 22, 2014 1:52 am

And the taxpayers funded this.

April 22, 2014 1:57 am

“Led by scientists at Yale, the study focused on Antarctica during the Eocene epoch, 40-50 million years ago, a period with high concentrations of atmospheric CO2”
That raises the matter of how much was the latter actually so. For instance, Pearson et al 1999 has calculated from proxy data that CO2 during the mid Eocene (sampling 43 million years ago) was only 370 to 400 ppm (best estimate, with the data judged to constrain it to somewhere between 170ppm and 570ppm): http://www.geol.umd.edu/~kaufman/ppt/G436/G436_PDF_library/Pearson_99.pdf
Additionally, separate from the CO2 level in itself is the matter of whether it was more a consequence of the temperature than a temperature driver, with warmer oceans outgassing more (and influenced by other factors like volcanic activity).
Pearson et al. also remark:
If our estimate of middle Eocene pCO2 is correct, then it implies either that Earth’s climate is very sensitive to small changes in pCO2, or that the global cooling since the Eocene was not driven primarily by changes in pCO2, but rather reflects reorganization of ocean circulation resulting from tectonic opening and closing of oceanic gateways (2).
Of course, the former scenario doesn’t fit other evidence, such as how going from pre-industrial levels of CO2 to the 400 ppm of CO2 now hasn’t caused more than low tenths of a degree temperature change at most (since the bulk of warming since the LIA is already explainable by another cause far better matching its pattern).

johnmarshall
April 22, 2014 2:14 am

I do not quite see why the warm poles 50Ma ago prove it could happen today. The continents are completely different with totally different ocean currents. Look at the map they provide above.
It does show that Plate Tectonics are a climate driver, though slower than sunshine.

johnmarshall
April 22, 2014 2:17 am

If the atmospheric CO2 content fell below 200ppmv all plant life would hav e died out. This did not happen so my bet is that the CO2 levels were well above this figure.
CO2 DOES NOT DRIVE CLIMATE.

Admin
April 22, 2014 2:21 am

A long time ago, Someone I knew was involved with a software migration project. When they finished the specification for the next item, They were told to delete the work and start again. The whole project was a massive ripoff.
Can’t think of why this paper reminds me of that project.

NDJ
April 22, 2014 2:25 am

“the Eocene epoch … a period with high concentrations of atmospheric CO2 and consequently a greenhouse climate”
So, water vapour was not a greenhouse gas back then?

H.R.
April 22, 2014 2:48 am

Paul Pierett says:
April 22, 2014 at 12:07 am
“That’s old news. […]”
===============================
Ahhh, good ol’ WUWT commenters. Paul got it in the first comment and in the first three words.
Who’s to blame the researchers for taking advantage of the fact that the people approving grant applications don’t do any extensive literature search, if they search at all?

Kano
April 22, 2014 2:53 am

Was the climate warmer because of CO2, or was CO2 more abundant because it was warmer

FrankK
April 22, 2014 3:09 am

The main issue as always is with the assumption that higher CO2 caused higher temperatures rather than higher CO2 caused by the higher temperatures that existed between the end of the Paleocence (65 to 55 MY) and the beginning of the Eocene (55 to 35 MY). Natural CO2 increase follows temperature not the reverse as demonstrated by ice cores in the longer-term and also at shorter time periods. In much of the Eocene there was a cooling trend. Also although during the Paleocene/Eocene periods the Antarctica continent was well separated from a Gondwanaland and therefore Australia and had its southern part within the south pole region, its northern part extended further north than the present Antarctic circle at latitude 66.59 degrees south of the equator.

cedarhill
April 22, 2014 3:19 am

The key parts of the PR:
“… the new measurements can help improve climate models used for predicting future climate… Quantifying past temperatures helps us understand the sensitivity of the climate system to greenhouse gases, and especially the amplification of global warming in polar regions…”
AND
“…the study focused on Antarctica during the Eocene epoch, 40-50 million years ago, a period with high concentrations of atmospheric CO2 and consequently a greenhouse climate…”
Even that outstanding climate physist journal, Mother Earth, had this to say about the area studied
http://elainemeinelsupkis.typepad.com/earth_news/2006/04/antarctica_froz.html
While minor events like volanoes, rifting, continents moving from North to South, the oceans in what must have been near castrophic changes, the science boys and girls alwasy imply CO2 and greenhouse gases are major drivers. CO2 has evolved, just like Baal of ancient times as the great weather god of Western (Political) Science.
And, if, as phillipbratby said at April 22, 2014 at 1:52 am. “And the taxpayers funded this”, emmense offerings are made by everyone, to the CO2 god.

richard
April 22, 2014 3:42 am

Yale are a bit slow of the mark.
http://www.belspo.be/belspo/bepoles/file/459.pdf
Back at the turn of the century 20th century Shackleton on his expedition to the Antarctic found seams of coal, impressions of leaves in sandstone boulders and fossilized wood from coniferous trees.

wws
April 22, 2014 4:04 am

I couldn’t help but notice their map has a little England and ireland off the coast of proto-europe; even though it’s now agreed that the English Channel wasn’t carved out until the end of the last ice age, about 12K years ago.

Micula
April 22, 2014 4:12 am

The Antarctic only became fully ice covered at the end if the Eocene and into the Oligocene when it was split away from South America and the circum-Antarctic currents developed. This isolated Antarctica and allowed the major cooling. It was tectonics and nothing much else.

Editor
April 22, 2014 4:13 am

Led by scientists at Yale, the study focused on Antarctica during the Eocene epoch, 40-50 million years ago, a period with high concentrations of atmospheric CO2 and consequently a greenhouse climate.“. A comment on the Middle Eocene Climatic Optimum (MECO) noted “ just how large the natural buildup of atmospheric CO2 may have been—as much as 50 times modern levels. Yet even at these levels Earth was still quite livable.“.
http://theresilientearth.com/?q=content/co2-temperature-during-middle-eocene-climatic-optimum
’50 times’ is well over five doublings.
This provides strong evidence that global warming is especially pronounced close to the Earth’s poles.“. Like antarctica close to the South Pole today?

April 22, 2014 4:18 am

@bushbunny – People forget that the continents were not always in the exact position they are today. And someone posted a short video showing what they would be like in another 100 million years (I doubt man will be wise enough to still be around then).
So there may have been ice caps during the Eocene. But Antarctica was not under them.

Steve Keohane
April 22, 2014 5:01 am

Where landmass used to be:
http://www.scotese.com/earth.htm
temperature and CO2 over the long term:
http://i46.tinypic.com/2582sg6.jpg

Bill Illis
April 22, 2014 5:19 am

This is a much better illustration of Antarctica circa about 45 million years ago.
http://cdn.phys.org/newman/gfx/news/hires/2014/1-iconicaustra.jpg
But I don’t think Antarctica was quite at the south pole then, even though all the reconstructions have it not quite in its current position but close. It had to be more like 2000 kms to the northwest, going by the location of the mid-oceanic ridge between Antarctica and Australia/Tasmania. Its just something that I think cannot be ignored. It is factual evidence.
The other issue is what were the ocean currents doing then? There was no Antarctic circumpolar current. Just the large ocean gyres which would have brought warm water from the tropics to Antarctica.
The ocean currents and continental positions about 45 million years ago.
http://img35.imageshack.us/img35/8862/antoceancurrents35m.jpg
This is an in-depth description/chart of temperature and geography over the last 45 million years.
http://s22.postimg.org/804qp4xo1/Temp_Geography_45_Mys.png
Was Antarctica warmer then? Yes, trees grew there and some marsupials lived in Antarctica at the time (Australia and South American cousins). But it still had six months of darkness. Reasonably warm summers (above 0.0C certainly) but it was extremely cold in the six months of dark winter at the pole.
When Australia and South America separated from it just enough so that the ocean was about 400 metres deep (it could take tens of millions of years for this to occur after an initial separation), the Antarctic Circumpolar Current started up, exactly at 33.6 million years ago. Within 75,000 years, Antarctica became nearly completely glaciated over and all the plants and animals were gone.

April 22, 2014 5:27 am

FYI, Eocene paleogeography map source :
http://jan.ucc.nau.edu/rcb7/50moll.jpg
Paleogeography for other time slices :
http://jan.ucc.nau.edu/rcb7/mollglobe.html
Also, FYI, Dr. Blakey is now commercializing these maps. See :
http://cpgeosystems.com/index.html
If you like them, you can buy the latest updated maps here & support Dr. Blakey (now Professor Emeritus from Northern Arizona University)

April 22, 2014 5:54 am

Doesn’t that mean that we would be far wiser to learn to adapt to climate change, rather than try to “control” it? We are not as almighty, as we would seem to think!

Walt S
April 22, 2014 6:11 am

Middle Eocene was one hell of a time in a variety of places around the globe. In Texas, for example, a gorge was cut into the near offshore sediments that measured 65 miles long, in places up to 12 miles wide and easily cut 3,000 feet deep. One hell of an erosional feature, cut in a very short amount of geological time. It must have taken some very special conditions to do that. The fun part is that the entire gorge then almost as quickly filled up with sediments– so that the Upper Eocene sediments are flat above it. It’s called the Yoakum Channel if you wish to Google. During this same time period in other places in the Gulf of Mexico depositional basin, sands that would normally be deposited near the shoreline were remarkably transported hundreds of miles offshore — some forming the reservoirs now exploited in the ultra deep portions of the Gulf of Mexico.
Wicked conditions must have existed during a portion of the Eocene. But I don’t believe those (strange) conditions existed at the beginning nor at the end of the Eocene in areas along the Gulf Coast.

Tom BR
April 22, 2014 6:13 am

“We managed to combine data from a variety of geochemical techniques on past environmental conditions with climate model simulations to learn something new about how the Earth’s climate system works under conditions different from its current state,” Affek said. “This combined result provides a fuller picture than either approach could on its own.”
TRANSLATION: We cooked up some data-like numbers by compiling a bunch of unrelated stuff, then threw them into known-to-be-skewed climate models and hit the “go” button, generating some simulated-output that has no relationship whatsoever to climate dynamics as now understood. The combined result provides us with something to talk about in our faculty lounge — isolated from the real world so well — in a way our underlings won’t understand, yet also offer fodder for a subsequent grant application, which will allow us to economically survive for another year or two.

ferdberple
April 22, 2014 6:32 am

a period with high concentrations of atmospheric CO2 and consequently a greenhouse climate.
=================
question 1. does making the glass thicker make a greenhouse warmer?
question 2. does CO2 lead or lag temperature?
question 3. how can the IPCC claim of low natural variability be correct? wasn’t this large variability due to natural causes?

Chris4692
April 22, 2014 6:46 am

Bill Illis says:
April 22, 2014 at 5:19 am

But I don’t think Antarctica was quite at the south pole then, even though all the reconstructions have it not quite in its current position but close. It had to be more like 2000 kms to the northwest,

Am having trouble envisioning what direction Northwest of the south pole could be.

April 22, 2014 6:57 am

wws says:
April 22, 2014 at 4:04 am
I couldn’t help but notice their map has a little England and ireland off the coast of proto-europe; even though it’s now agreed that the English Channel wasn’t carved out until the end of the last ice age, about 12K years ago.
=================================================
Sheesh !!!
It’s Climate “Science.”
You want accuracy?

JimS
April 22, 2014 7:05 am

Extract:
“This provides strong evidence that global warming is especially pronounced close to the Earth’s poles. Warming in these regions has significant consequences for climate well beyond the high latitudes due to ocean circulation and melting of polar ice that leads to sea level rise.”
Comment: OK, so given that the sea ice has steadily increased for the last 40 years around Antarctica, what is all the fuss about global warming?

Jeff Alberts
April 22, 2014 7:17 am

I have a problem with proclamations about the past that “this happened” or “that happened”. They simply don’t know, and have no way of knowing. They can make an educated guess, but that guess could be, and probably is, orders of magnitude off. They don’t know the configuration of the continents 50mya. Sure they might have been where they think they were, but it’s still speculation, not a fact.
It’s that uncertainty thing again.

David Ball
April 22, 2014 7:35 am

This might help define the era climatologically;
http://arctic.synergiesprairies.ca/arctic/index.php/arctic/article/view/1738

Michael
April 22, 2014 7:40 am

Could all this be silly speculation stemming from a bad hypothesis (Wegener’s)? Perhaps. See here for an alternative view: http://www.threeimpacts-twoevents.com/wp-content/uploads/2013/05/Geologic-Sensemaking-Simultaneous-Impacts-10May2013.pdf

Phil.
April 22, 2014 7:57 am

wws says:
April 22, 2014 at 4:04 am
I couldn’t help but notice their map has a little England and ireland off the coast of proto-europe; even though it’s now agreed that the English Channel wasn’t carved out until the end of the last ice age, about 12K years ago.

That isn’t their map it doesn’t occur anywhere in the paper!

george e. smith
April 22, 2014 8:27 am

So what do these “scientists” ; as a result of this research “result”, wish for the Congress of the united States to take up as an action item, for the current or next President of the United States to sign ??
Most functioning rational businesses, would want to know what they can do to improve their bottom line for their next 90 day predictions to Wall Street. Otherwise their stock is going to get a sell recommendation.
Seems to me to be functionally dishonest to waste resources on an issue, that we can do nothing about; namely where Florida and California were 40-50 million years ago (maybe).
I see the principal author, is on his way to his permanent position as a post doc fellow, at a taxpayer funded institutional establishment. Add one more to the list of PhDs, unable to find work in their field of expertise.

Jimbo
April 22, 2014 8:45 am

Led by scientists at Yale, the study focused on Antarctica during the Eocene epoch, 40-50 million years ago, a period with high concentrations of atmospheric CO2 and consequently a greenhouse climate.

The ordovician had “high concentrations of atmospheric CO2 and consequently” an ice age.

Jim
April 22, 2014 8:46 am

I think you are forgetting the amazing part, this paper and the work represents current supreme court thought. It doesn’t have to be accurate or true, or veritable or reproducible. Just following the program set out. This is also what will be taught in the future. I pity the poor students. Talk about what they will face.

Robert Wykoff
April 22, 2014 8:46 am

Chris4692 says:
“Am having trouble envisioning what direction Northwest of the south pole could be.”
Snicker, was thinking the same thing, though I think he meant relative to if you were looking at the “south pole” on a rectangular wall map.

Phil.
April 22, 2014 8:51 am

george e. smith says:
April 22, 2014 at 8:27 am
I see the principal author, is on his way to his permanent position as a post doc fellow, at a taxpayer funded institutional establishment. Add one more to the list of PhDs, unable to find work in their field of expertise.

George,I thought Caltech was privately funded?

Robert W Turner
April 22, 2014 9:03 am

Before going out and conducting paleotemperature research using this new method it would be nice to see how this new technique compares to the proxy temperature reconstruction from O18 isotopes that we’ve been basing reconstructions on for a while now.

April 22, 2014 9:44 am

With a 95% probability, there is a 75% chance that they had a warrior-king named Conan on this warmer continent, but I’ll need further funding to continue my research.

george e. smith
April 22, 2014 12:35 pm

“””””……Phil. says:
April 22, 2014 at 8:51 am
george e. smith says:
April 22, 2014 at 8:27 am
I see the principal author, is on his way to his permanent position as a post doc fellow, at a taxpayer funded institutional establishment. Add one more to the list of PhDs, unable to find work in their field of expertise.
George,I thought Caltech was privately funded?……”””””
Phil, they probably are; just like MIT is privately funded (I think).
The probability, that neither of those institutions is doing ANY Federal Government / Military research programs, is likely rather small. A sizeable part of my tech library, consists of that set of text books, known as “The Radiation Laboratory Series”, published by McGraw Hill from MIT Government research.
In fact, I just pulled out Volume 18; by “Valley and Wallman” on “Vacuum Tube Amplifiers” to pass over to my son who is doing an electronics course, at a local “community College”. He will actually learn more Electronics fundamental principles he can use, from that book, than from what he has brought home as text book materials, from his instructor.
And I’m quite sure that workers at any “publish or perish” institution, will gladly glean grant money from ANY source, public or private, to keep from having to get a job. Including this new post Doc student wunderkind of Caltech.
I’m quite happy as a taxpayer, to help fund potentially useful research; and no I don’t want to be sitting in a position of judgement, as to what such projects should be. I have enough faith in academia, to let them run their own show.
But I know a boondoggle when I see one, and criticism of poor judgement, is still ok with me.
I can conceive of no business like corporation, ever wanting to hire anyone, whose specific expertise is the earth, 50 million years ago.
Now “Marine Biology” as a course being pursued by a deserving middle age student, at my alma mater, I’m quite happy to help with funding. But he intends to work with living sea creatures; not 50 million years dead ones.

Louis
April 22, 2014 1:18 pm

“polar regions of the southern Pacific Ocean registered 21st-century Florida heat”

Didn’t Hansen tell us that a climate-change event like that would be irreversible? Why didn’t Earth’s climate spiral out of control and turn into Venus back then?

Ort
April 22, 2014 2:19 pm

Very interesting study. Thank you.

milodonharlani
April 22, 2014 2:26 pm

The poles have had ice when CO2 was much higher & lacked it when CO2 was lower. Other factors are far more important.
As for the Eocene, Antarctica was still connected to South America then & only separated from Australia by shallow water. Antarctic glaciation is associated with the formation of deep channels between both South America & Australia around the Eocene/Oligocene transition.

chemman
April 22, 2014 3:30 pm

Jimbo says:
April 22, 2014 at 8:45 am
_____________________________________________________________________________
Trying to confuse them with the facts when their models say otherwise. What is the world coming too.

bushbunny
April 22, 2014 7:24 pm

phil, Australia is moving northwards by a small amount of cms a year, in a 100,000 million years we will be right in the middle of the ring of fire and Japan will be closer to the North Pole. You are correct, no living organism has survived 100,000 million years unless we planet hop.

Phil.
April 23, 2014 5:27 am

george e. smith says:
April 22, 2014 at 12:35 pm
But I know a boondoggle when I see one, and criticism of poor judgement, is still ok with me.
I can conceive of no business like corporation, ever wanting to hire anyone, whose specific expertise is the earth, 50 million years ago.

What about an oil and gas company? Like say, Statoil, who funded this particular study.

Pamela Gray
April 23, 2014 8:06 am

Shocking that oceanic/atmospheric teleconnections can keep a higher lattitude country warmer than it would otherwise be. And all done without the aid of human influence (that little tidbit about CO2 was added for the funds – the conclusion. SHOCKING I say! Right Northern Europe?
I swear the next orgasm these climate science people have is when they find out that rivers don’t flow uphill.

Pamela Gray
April 23, 2014 8:09 am

Oops. Didn’t finish the sentence – the conclusion “tags oceanic circulation patterns at the time to be the likely reason for warmer Antarctic temperatures.”

phlogiston
April 23, 2014 11:49 am

These papers always start with the answer – CAGW – then look for a question that makes the answer seem plausible and respectable. A futile exercise.

phlogiston
April 23, 2014 3:18 pm

If CO2 global warming is amplified at the poles then why is only the North pole warming while the South pole cools and its sea ice increases? It looks more like a bipolar seesaw (NH warms by stealing ocean heat from the SH which cools).

bushbunny
April 23, 2014 8:14 pm

Hi phlogiston, good query. Simple it is coming into winter here in the Southern hemisphere. And that Antarctica is a land mass unlike the North Pole. Can you remember at primary school we were asked to name the continents in rote. ” Europe, Americas, Australasia, Asia, and Antarctica. The Arctic is not a continent.” That might be a simplistic answer, but it is true.

Brian H
April 25, 2014 1:36 am

I tried to find where they explained how CO2 caused continental drift, but I couldn’t. Anyone help?