Ocean seawater chemistry linked with periods of global cooling, sharp changes from greenhouse to icehouse climate

From the University of Toronto , something quite unexpected.

Scientists connect seawater chemistry with climate change and evolution

TORONTO, ON – Humans get most of the blame for climate change, with little attention paid to the contribution of other natural forces. Now, scientists from the University of Toronto and the University of California Santa Cruz are shedding light on one potential cause of the cooling trend of the past 45 million years that has everything to do with the chemistry of the world’s oceans.

Caption: This is a satellite view of the Zagros mountain belt in western Iran. The range forms part of the most extensive belt of water-soluble gypsum on Earth, stretching from Oman to Pakistan, and well into Western India. Scientists suggest that the dissolution of ancient salt deposits caused drastic changes in seawater chemistry, which may have triggered long-term global cooling. Credit: US Geological Survey/Center for Earth Resources Observation and Science

“Seawater chemistry is characterized by long phases of stability, which are interrupted by short intervals of rapid change,” says Professor Ulrich Wortmann in the Department of Earth Sciences at the University of Toronto, lead author of a study to be published in Science this week. “We’ve established a new framework that helps us better interpret evolutionary trends and climate change over long periods of time. The study focuses on the past 130 million years, but similar interactions have likely occurred through the past 500 million years.”

Wortmann and co-author Adina Paytan of the Institute of Marine Sciences at the University of California Santa Cruz point to the collision between India and Eurasia approximately 50 million years ago as one example of an interval of rapid change. This collision enhanced dissolution of the most extensive belt of water-soluble gypsum on Earth, stretching from Oman to Pakistan, and well into Western India – remnants of which are well exposed in the Zagros mountains.

Caption: This is the Zagros mountain belt in western Iran as seen from the space shuttle Atlantis. The range forms part of the most extensive belt of water-soluble gypsum on Earth, stretching from Oman to Pakistan, and well into Western India. Scientists suggest that the dissolution of ancient salt deposits caused drastic changes in seawater chemistry, which may have triggered long-term global cooling. Credit: Photo courtesy of NASA

The authors suggest that the dissolution or creation of such massive gyspum deposits will change the sulfate content of the ocean, and that this will affect the amount of sulfate aerosols in the atmosphere and thus climate. “We propose that times of high sulfate concentrations in ocean water correlate with global cooling, just as times of low concentration correspond with greenhouse periods,” says Paytan.

“When India and Eurasia collided, it caused dissolution of ancient salt deposits which resulted in drastic changes in seawater chemistry,” Paytan continues. “This may have led to the demise of the Eocene epoch – the warmest period of the modern-day Cenozoic era – and the transition from a greenhouse to icehouse climate, culminating in the beginning of the rapid expansion of the Antarctic ice sheet.”

The researchers combined data of past seawater sulfur composition, assembled by Paytan in 2004, with Wortmann’s recent discovery of the strong link between marine sulfate concentrations and carbon and phosphorus cycling. They were able to explain the seawater sulfate isotope record as a result of massive changes to the accumulation and weathering of gyspum – the mineral form of hydrated calcium sulfate.

“While it has been known for a long time that gyspum deposits can be formed and destroyed rapidly, the effect of these processes on seawater chemistry has been overlooked,” says Wortmann. “The idea represents a paradigm shift in our understanding of how ocean chemistry changes over time and how these changes are linked to climate.”

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The findings are reported in the paper “Rapid Variability of Seawater Chemistry over the Past 130 Million Years.” The research is supported by a Discovery Grant to Wortmann from the Natural Sciences and Engineering Research Council of Canada, and a National Science Foundation CAREER award to Paytan. Data used in the research was collected through the Integrated Ocean Drilling Program (IODP) and facilitated by the United States Implementing Organization (USIO) and the Canadian Consortium for Ocean Drilling (CCOD).

About the IODP & the CCOD

The Integrated Ocean DrillingProgram (IODP) is an international research program dedicated to advancing scientific understanding of the Earth through drilling, coring, and monitoring the subseafloor. The JOIDES Resolution is a scientific research vessel managed by the U.S. Implementing Organization of IODP (USIO). Texas A&M University, Lamont-Doherty Earth Observatory of Columbia University and the Consortium for Ocean Leadership together comprise the USIO. IODP is supported by two lead agencies: the U.S. National Science Foundation (NSF) and Japan’s Ministry of Education, Culture, Sports, Science, and Technology. Additional program support comes from the European Consortium for Ocean Research Drilling (ECORD), the Australia-New Zealand IODP Consortium (ANZIC), India’s Ministry of Earth Sciences, the People’s Republic of China (Ministry of Science and Technology), and the Korea Institute of Geoscience and Mineral Resources. For more information, visit www.iodp.org.

The Canadian Consortium for Ocean Drilling (CCOD) is a consortium composed of Canadian universities formed to facilitate, support and encourage Canada’s participation in IODP.

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Science 20 July 2012:

Vol. 337 no. 6092 pp. 334-336

DOI: 10.1126/science.1220656

Rapid Variability of Seawater Chemistry Over the Past 130 Million Years

Ulrich G. Wortmann ,Adina Paytan

Abstract

Fluid inclusion data suggest that the composition of major elements in seawater changes slowly over geological time scales. This view contrasts with high-resolution isotope data that imply more rapid fluctuations of seawater chemistry. We used a non–steady-state box model of the global sulfur cycle to show that the global δ34S record can be explained by variable marine sulfate concentrations triggered by basin-scale evaporite precipitation and dissolution. The record is characterized by long phases of stasis, punctuated by short intervals of rapid change. Sulfate concentrations affect several important biological processes, including carbonate mineralogy, microbially mediated organic matter remineralization, sedimentary phosphorous regeneration, nitrogen fixation, and sulfate aerosol formation. These changes are likely to affect ocean productivity, the global carbon cycle, and climate.

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Babsy
July 21, 2012 11:33 am

No! No! No! This cannot possibly be so!!!! It’s all about CO2 and the Coal Trains of Death!! Oh, THE HU-MANN-ITY

NickB.
July 21, 2012 11:42 am

Am I reading this right? Could this help explain that nagging temperature rise preceding CO2 rise by ~800 year problem that the “CO2 is the world’s thermostat” crowd seem to have such trouble explaining?

David L. Hagen
July 21, 2012 12:16 pm

Could solar/cosmic rays changing clouds affect precipitation which increases/decreases sulfate runoff?

Jeremy
July 21, 2012 12:23 pm

Interesting. It is well understood in Earth Sciences that geological epochs appear to be linked to climatic changes. Most geologists suspect that plate tectonics and the movement of the continents play are a very large role in climate, whether these are down to changes in Ocean circulation and/or other factors is still not fully understood. The nice thing is that if you look back 100’s of millions of years it is pretty clear that CO2 is not even a minor factor. Changes in atmospheric CO2 are most likely an indicator or flag that something else has changed in the overall system. It is impossible for any rational person who has an understanding of geology to attribute any meaningful role to CO2 as an actual driver.

Sean
July 21, 2012 12:29 pm

An interesting post. But is it the sulfate or the calcium. Perhaps higher calcium sulfate concentrations permits much more of the earths gaseous CO2 to be dissolved into the ocean as calcium bi-carbonate (in the cold regions) or precipitated out as limestone in the warm regions.

Editor
July 21, 2012 12:38 pm

NickB. says:
July 21, 2012 at 11:42 am

Am I reading this right? Could this help explain that nagging temperature rise preceding CO2 rise by ~800 year problem that the “CO2 is the world’s thermostat” crowd seem to have such trouble explaining?

I don’t see how, while the abstract talks about recent events, it means recent in a geologist’s sense. 800 years is merely an instant, if that.
“When India and Eurasia collided, it caused dissolution of ancient salt deposits which resulted in drastic changes in seawater chemistry,” Paytan continues. “This may have led to the demise of the Eocene epoch – the warmest period of the modern-day Cenozoic era – and the transition from a greenhouse to icehouse climate, culminating in the beginning of the rapid expansion of the Antarctic ice sheet.”
The Eocene is 37 – 56 million years ago. There’s a lot of 800 year instants in that period.

July 21, 2012 1:03 pm

The correlation between the Indian plate collision with Asia & the subsequent downward trend in global temps has long been known by geologists but this is the first time I have heard this sulfate hypothesis proposed. Previously, the correlation was generally attributed to changes in upper atmosphere circulation, driven by the lifting of the mountains, both in Asia and in North America (Rocky Mtns uplift at roughly the same time).
I can see the potential validity in this hypothesis, although I wouldn’t say that it rules out the old hypothesis either. In reality, it could be a combination of both effects.
For non-geoscientists out there, the images of the Zagros foldbelt attached with the post , show compressional anticlines, which where formed by the collision of the Indian plate with Asia. The significance of this, which isn’t explicitly stated in the article, is that these folds are cored by evaporite minerals, such as gypsum, anhydrite & halite. The collision process forms the folds & lifts these evaporite rocks to the surface, where prior to that,they would have been buried deep in the subsurface. Evaporite minerals are easily dissolved in water, so once at the surface, they can be rapidly dissolved / eroded & carried into the ocean by rainwater / streams / rivers, thus potentially dramatically changing ocean chemistry in a short period of time, such as the article suggests. The Zagros belt is extremely extensive , so this isn’t an unreasonable hypothesis.
I hope this explanation helps tie the images to what the author’s are thing to propose for non-geoscientists.
This article further strengthens the ties of geologic & climatologic processes together. Geoscientists are well aware of these ties & understand the huge variability of climate of geologic time, all driven by non-anthropogenic processes, thus why you will find the vast majority of geoscientists (myself included) falling into the skeptic camp when it comes to the subject of CAGW.

Alex
July 21, 2012 1:03 pm

Hmmmm. But what about the periodicity of various cycles, such as the 1500-year periodicity seen over the past 6,000 years? Is this overlain on top?

July 21, 2012 1:18 pm

“cooling trend of the past 45 million years” ????
Too curious? Or, towards new thinking with the jellyfish?
Given the limited attention paid to the anthropogenic component in the process between ocean and atmosphere, the magazine Nature surprised at least me, when it recently presented a study titled: “Jellyfish help mix the world’s oceans. Marine creatures could stir up seas as much as do winds and tides.” [*]
• ” Small sea creatures such as jellyfish may contribute to ocean mixing by pulling water along as they swim, according to a new study. The collective movement of animals could generate stirring of the same order as winds and tides, the authors suggest.”
• “Some scientists are skeptical that the process plays an essential role in the mixing of the oceans. However, should further evidence confirm this, it should be based on modeling effects that include the sea water mixing to simulate the past and future climate.”
• “If swimming animals do affect ocean mixing substantially, climate modellers will face “a forbidding challenge”, says physical oceanographer Carl Wunsch…”
It seems not too difficult to imagine that world shipping has a much more pronounced effect, and during war time the anthropogenic impact on the marine environment would literally explode.
More at: http://www.seaclimate.com/a/a3.html
(*)Kwok, Roberta (2009); “Jellyfish help mix the world’s oceans”, Nature, online 29 July doi:10.1038/news.2009.745; http://www.nature.com/news/2009/090729/full/news.2009.745.htm

Mariana Britez
July 21, 2012 1:22 pm

Maybe this type of article gives some possibility for the career of “climate scientist” may have some future. I am sure once they give up on the CO2 story, there actually may be some chance for these guys to study NATURAL CLIMATE LOL

John F. Hultquist
July 21, 2012 1:27 pm

Seems to be one of those things that hides in plain sight. Geologists should enjoy this – another example of “catastrophism” and the implications for review of old and development of new science.
Very interesting, though it seems not to tighten the wobbly wheels on the catastrophic global warming wagon. “. . . short intervals of rapid change.” in a geologic sense isn’t necessarily short in a human’s timeframe and ‘short’ is the essence of CAGW.

Editor
July 21, 2012 1:29 pm

Alex says:
July 21, 2012 at 1:03 pm
> Hmmmm. But what about the periodicity of various cycles, such as the 1500-year periodicity seen over the past 6,000 years? Is this overlain on top?
The Eocene ended about 37,000,000 years ago. Even 6,000 years ago, the Eocene had been over for about 37,000,000 years. While 6,000 years is longer than 800 years, it’s still just a moment ago to geologists that work outside the Holocene.

otsar
July 21, 2012 1:46 pm

.Is this new? I studied the geochemical consequences of India colliding with Asia in the 70’s, in a geochemistry class. In what I have read of this paper they fail to mention that the Himalayan orogeny (Mountain building) disrupted atmospheric circulation in a significant way. The Himalayas produced and continues to produce a great deal of orographic precipitation. The Himalayas are still growing as the Indian continent pushes further into the Eurasians continent.
They also failed to mention that a large amount of limestone became exposed to weathering and dissolution. It is well known that when limestone is dissolved in water CO2 is removed from the atmosphere.
The Himalayas continue to remove a lot of water and CO2 from the atmosphere, and also modify atmospheric circulation. It appears that their grant was for the study of sulfates therefore it is the most significant parameter “One potential cause.” They also seem to be making an oblique case for the importance sulfate aerosols.
I wonder if in their framework, if it is the kind of framework I am thinking of, they included atmospheric circulation changes due to mountain building and destruction. It would have been educational if they had mentioned some of the other parameters in their framework
When I read through abstracts and news releases like this, I get the feeling that some of the Earth Sciences have become disconnected from others and have agendas.

July 21, 2012 1:48 pm

You know what I don’t like about WUWT? It’s too sciency. It’s the weekend! How about some pandas, or a puppy video? I mean, you’ve already won. No scientist who isn’t paid to believe in AGW believes in AGW.
I’m an engineer. I have to think in terms of science all week long. When it’s the weekend, show us some puppies, Anthony! Or a cat and a rabbit hugging. Something like that. No more forcing me to muddle through a chart or a graph. Save that for M-F.
Thanks in advance. 😉

Caz in BOS
July 21, 2012 2:10 pm

How did the authors exclude other possible factors, co-incidently happening at the same time, especially the position of South America relative to Antarctica and North America?

Dr Burns
July 21, 2012 2:20 pm

“We propose that times of high sulfate concentrations in ocean water correlate with global cooling” Gypsum solubility increase to 40 deg C. It is also effected by carbonate (marine invertebrates), chloride and pressure. I wonder if these factors have all been considered ?

Robert of Ottawa
July 21, 2012 2:21 pm

Salinity sanity … only in Canada eh? 🙂 Sorry, must brag. But we do appear to have a somewhat saner government than most Western Nations. In a purported letter from 2002, publicized by his political enemies – including the socialist CBC – he supposedly states:
We’re gearing up for the biggest struggle our party has faced since you entrusted me with the leadership. I’m talking about the “battle of Kyoto” — our campaign to block the job-killing, economy-destroying Kyoto Accord.
It would take more than one letter to explain what’s wrong with Kyoto, but here are a few facts about this so-called “Accord”:
◦It’s based on tentative and contradictory scientific evidence about climate trends.
◦ It focuses on carbon dioxide, which is essential to life, rather than upon pollutants.
◦ Canada is the only country in the world required to make significant cuts in emissions. Third World countries are exempt, the Europeans get credit for shutting down inefficient Soviet-era industries, and no country in the Western hemisphere except Canada is signing.
◦ Implementing Kyoto will cripple the oil and gas industry, which is essential to the economies of Newfoundland, Nova Scotia, Saskatchewan, Alberta and British Columbia.
◦As the effects trickle through other industries, workers and consumers everywhere in Canada will lose. THERE ARE NO CANADIAN WINNERS UNDER THE KYOTO ACCORD.
◦The only winners will be countries such as Russia, India, and China, from which Canada will have to buy “emissions credits.” Kyoto is essentially a socialist scheme to suck money out of wealth-producing nations.
◦On top of all this, Kyoto will not even reduce greenhouse gases. By encouraging transfer of industrial production to Third World countries where emissions standards are more relaxed, it will almost certainly increase emissions on a global scale

I don’t remember seeing this letter at the time (I was a member), but it’s great if true.

Robert of Ottawa
July 21, 2012 2:24 pm

HE being Prime Minster Stephen Harper, of course.

pat
July 21, 2012 2:28 pm

I am not so sure. But it bears following up. Glad to see some original thinking in climate science for a change.

rogerknights
July 21, 2012 3:02 pm

This must have affected oceanic PH a lot. Which way? And what effect did it have on marine life, corals, etc.?

Gary Hladik
July 21, 2012 3:13 pm

Wait. So the science isn’t settled???

jayhd
July 21, 2012 3:30 pm

Jeff L says: July 21, 2012 at 1:03 pm
Thanks Jeff. As a non-scientist I appreciate your explanation.
Jay Davis

Louis Hooffstetter
July 21, 2012 3:40 pm

This is an interesting idea that bears further investigation. However, I remain highly skeptical of statements like “We used a… model… to show that the… record can be explained,,,.”.
Models are easily tweaked to hindcast historical data, (which gives them the appearance of validity), but if they can’t accurately predict future trends, they’re garbage. The ‘acid test’ for any model is how well it predicts or matches reality.

NickB.
July 21, 2012 3:46 pm

Thanks Ric.
Cheers,
NickB.

Bill Illis
July 21, 2012 3:50 pm

The big white spot at the bottom of this actual picture is Antarctica. The big brown spot above and to the right is Australia.
http://media.web.britannica.com/eb-media/80/4280-004-C7086222.jpg
At 33.7 million years ago, Antarctica looked more like Australia’s surface in the southern hemisphere’s summer when this picture was taken. .
By 33.5 million years ago, it was already as white as the current picture.
If you calculate the change in the Earth’s overall Albedo caused by this change, which took less than 100,000, it is enough to drop the Earth’s temperature by 2.0C (which is exactly what happened). The Antarctic Circumpolar Current was initiated at this time which isolated Antarctica in an extreme polar climate which lead to a complete glaciation of the continent.
If you want to go back through the Eocene, one will find that similar kinds of changes in Albedo lead to slow cooling (and then warming) and then cooling and then warming again.

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