Dinosaurs lived in greenhouse climate with hot summers

Niels de Winter doing research on fossil shells. Credit: Niels de Winter

Paleoclimatologist Niels de Winter and colleagues developed an innovative way to use the clumped isotope method to reconstruct climate in the geological past on the seasonal scale. They show that dinosaurs had to deal with hotter summers than previously thought. The results suggest that in the mid latitudes, seasonal temperatures will likely rise along with climate warming, while seasonal difference is maintained. This results in very high summer temperatures.

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Palaeoclimatologists study climate of the geological past. Using an innovative technique, new research by an international research team led by Niels de Winter (VUB-AMGC & Utrecht University) shows for the first time that dinosaurs had to deal with greater seasonal differences than previously thought.

De Winter states that "we used to think that when the climate warmed like it did in the Cretaceous period, the time of the dinosaurs, the difference between the seasons would decrease, much like the present-day tropics experience less temperature difference between summer and winter. However, our reconstructions now show that the average temperature did indeed rise, but that the temperature difference between summer and winter remained rather constant. This leads to hotter summers and warmer winters."

To better characterize the climate during this period of high CO2 concentration, the researchers used very well-preserved fossils of mollusks that lived in southern Sweden during the Cretaceous period, about 78 million years ago. Those shells grew in the warm, shallow seas that covered much of Europe at the time. They recorded monthly variations in their environment and climate, like the rings in a tree. For their research, de Winter and the team used the "clumped isotope" method for the first time, in combination with a method developed by Niels de Winter.

Clumped isotopes in combination with the VUB-UU method&#;a revolution in geology

Isotopes are atoms of the same element with different masses. Since the s, the ratio of oxygen isotopes in carbonate has been used to measure water temperature in the geological past. However, this required researchers to estimate the chemistry of the seawater, as the isotope ratio of the seawater affects the isotope ratio of the shell, which results in higher uncertainty. About ten years ago, the "clumped isotope" method was developed, which does not depend on the chemistry of the seawater and allows accurate reconstructions. But the clumped isotope method has a disadvantage: it requires so much carbonate that temperature reconstructions at a more detailed level, such as seasonal fluctuations based on shells, were not possible.

De Winter has now developed an innovative method in which measurements of much smaller quantities of carbonate are cleverly combined for temperature reconstructions. The clumped isotope method thus requires much less material and can therefore be used for research on fossil shells, which, like tree rings, hold a great deal of information about their living conditions. The method also allows carbonate from successive summers (and winters) to be aggregated for better reconstruction of seasonal temperatures. For example, Winter found that water temperatures in Sweden during the Cretaceous "greenhouse period" fluctuated between 15°C and 27°C, over 10°C warmer than today.

The team also worked with scientists from the University of Bristol (UK) who develop climate models to compare the results with climate simulations of the Cretaceous period. Whereas previous climate reconstructions of the Cretaceous often came out colder than these models, the new results agree very well with the Bristol models. This shows that variations in seasons and water chemistry are very important in climate reconstructions.

"It is very difficult to determine climate changes from so long ago on the seasonal scale, but the seasonal scale is essential to get climate reconstructions right. If there is hardly any difference between the seasons, reconstructions of average annual temperature come out differently from situations when difference between the seasons is large. It was thought that during the age of the dinosaurs difference between the seasons was small. We have now established that there were greater seasonal differences. With the same temperature average over a year, you end up with a much higher temperature in the summer."

De Winter explains that their "results therefore suggest that in the mid latitudes, seasonal temperatures will likely rise along with climate warming, while seasonal difference is maintained. This results in very high summer temperatures. The results bring new insight into the dynamics of a warm climate on a very fine scale, which can be used to improve both climate reconstructions and climate predictions. Moreover, they show that a warmer climate can also have extreme seasons."

The development has far-reaching implications for the way climate reconstructions are done. It allows researchers to determine both the effect of seawater chemistry and that of differences between summer and winter, thus verifying the accuracy of decades of temperature reconstructions. For his groundbreaking research, De Winter has been nominated for both the annual EOS Pipette Prize and New Scientist Science Talent .

More information: Niels J. de Winter et al, Absolute seasonal temperature estimates from clumped isotopes in bivalve shells suggest warm and variable greenhouse climate, Communications Earth & Environment (). DOI: 10./s-021--9

Journal information: Communications Earth & Environment

Provided by Vrije Universiteit Brussel

Citation: Dinosaurs lived in greenhouse climate with hot summers (, June 10) retrieved 24 June from https://phys.org/news/-06-dinosaurs-greenhouse-climate-hot-summers.html

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Editor's note (11/22/): Over the years, we have heard from readers who tell us that they have seen this article being cited by people who deny the reality or seriousness of human-caused global warming. To make it harder for anyone to mischaracterize this article, we are adding this note:

• The fact that Earth has been hotter in the past than it is today doesn't prove that recent global warming is natural.
  • Forest fires can have both natural and human causes. So can climate change. It is partly through figuring out what caused the periods like the ones described in this article that we came to understand that carbon dioxide sets the thermostat of Earth's climate.
• The fact that Earth has been hotter in the past than it is today doesn't prove that current warming is harmless, either to people or other life on Earth.
  • Some previous hot periods led to global mass extinctions.
  • The hot house periods described in this article occurred millions and millions of years before humans existed. They have no bearing on whether modern human civilization can cope with the level of warming we are likely to face if we do not stop adding greenhouse gases to the atmosphere.

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This article was first published in August , and it has been updated to include new research published since then. This article is one of a three-part series on past temperatures. One is about how warm the Earth has been &#;lately.&#; The other is about the coldest Earth's ever been.

Our 4.54-billion-year-old planet probably experienced its hottest temperatures in its earliest days, when it was still colliding with other rocky debris (planetesimals) careening around the solar system. The heat of these collisions would have kept Earth molten, with top-of-the-atmosphere temperatures upward of 3,600° Fahrenheit.

Even after those first scorching millennia, however, the planet has often been much warmer than it is now. One of the warmest times was during the geologic period known as the Neoproterozoic, between 600 and 800 million years ago. Conditions were also frequently sweltering between 500 million and 250 million years ago. And within the last 100 million years, two major heat spikes occurred: the Cretaceous Hot Greenhouse (about 92 million years ago), and the Paleocene-Eocene Thermal Maximum (about 56 million years ago).

Cartoon by Emily Greenhalgh, NOAA Climate.gov.

History of hot

Temperature records from thermometers and weather stations exist only for a tiny portion of our planet's 4.54-billion-year-long life. By studying indirect clues&#;the chemical and structural signatures of rocks, fossils, and crystals, ocean sediments, fossilized reefs, tree rings, and ice cores&#;however, scientists can infer past temperatures.

None of these techniques help with the very early Earth. During the time known as the Hadean (yes, because it was like Hades), Earth&#;s collisions with other large planetesimals in our young solar system&#;including a Mars-sized one whose impact with Earth likely created the Moon&#;would have melted and vaporized most rock at the surface. Because no rocks on Earth have survived from so long ago, scientists have estimated early Earth conditions based on observations of the Moon and on astronomical models. Following the collision that spawned the Moon, the planet was estimated to have been around 2,300 Kelvin (3,680°F).

What the collision that spawned Earth's Moon may have looked like. Collisions between Earth and rocky debris in the early solar system would have kept the surface molten and surface temperatures blistering. Image courtesy NASA. 

Even after collisions stopped, and the planet had tens of millions of years to cool, surface temperatures were likely more than 400° Fahrenheit. Zircon crystals from Australia, only about 150 million years younger than the Earth itself, hint that our planet may have cooled faster than scientists previously thought. Still, in its infancy, Earth would have experienced temperatures far higher than we humans could possibly survive.

But suppose we exclude the violent and scorching years when Earth first formed. When else has Earth&#;s surface sweltered?

Thawing the freezer

Between 600 and 800 million years ago&#;a period of time geologists call the Neoproterozoic&#;evidence suggests the Earth underwent an ice age so cold that ice sheets not only capped the polar latitudes, but may have extended all the way to sea level near the equator. Reflecting ever more sunlight back into space as they expanded, the ice sheets cooled the climate and reinforced their own growth. Obviously, the Earth didn&#;t remain stuck in the freezer, so how did the planet thaw? 

A geologic history of Earth since its formation 4.6 billion years ago, divided by eon and period, and showing fossils typical of a given period. Fossils reveal not only ancient plants and animals, but also ancient climates. Artwork © Ray Troll, . Used with permission.

Even while ice sheets covered more and more of Earth&#;s surface, tectonic plates continued to drift and collide, so volcanic activity also continued. Volcanoes emit the greenhouse gas carbon dioxide. In our current, mostly ice-free world, the natural weathering of silicate rock by rainfall consumes carbon dioxide over geologic time scales. During the frigid conditions of the Neoproterozoic, rainfall became rare. With volcanoes churning out carbon dioxide and little or no rainfall to weather rocks and consume the greenhouse gas, temperatures climbed.

What evidence do scientists have that all this actually happened some 700 million years ago? Some of the best evidence is "cap carbonates" lying directly over Neoproterozoic-age glacial deposits. Cap carbonates&#;layers of calcium-rich rock such as limestone&#;only form in warm water.

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Rock formation in Namibia that shows a type of rock that only forms in warm water (cap dolostone) lying directly over a type of jumbled sedimentary rock, dated to 635 million years ago, that is commonly found at the margin of glaciers (diamictite). Image from teaching slides available at SnowballEarth.org.

The fact that these thick, calcium-rich rock layers sat directly on top of rock deposits left behind by retreating glaciers indicate that temperatures rose significantly near the end of the Neoproterozoic, perhaps reaching a global average higher than 90° Fahrenheit. (Today's global average is lower than 60°F.)

The tropical Arctic

A Smithsonian Institution project has tried to reconstruct temperatures for the Phanerozoic Eon, or roughly the last half a billion years. Preliminary results released in showed warm temperatures dominating most of that time, with global temperatures repeatedly rising above 80°F and even 90°F&#;much too warm for ice sheets or perennial sea ice. About 250 million years ago, around the equator of the supercontinent Pangea, it was even too hot for peat swamps!

Preliminary results from a Smithsonian Institution project led by Scott Wing and Brian Huber, showing Earth's average surface temperature over the past 500 million years.  For most of the time, global temperatures appear to have been too warm (red portions of line) for persistent polar ice caps. The most recent 50 million years are an exception. Image adapted from Smithsonian National Museum of Natural History.

Geologists and paleontologists have found that, in the last 100 million years, global temperatures have peaked twice. One spike was the Cretaceous Hot Greenhouse roughly 92 million years ago, about 25 million years before Earth&#;s last dinosaurs went extinct. Widespread volcanic activity may have boosted atmospheric carbon dioxide. Temperatures were so high that champsosaurs (crocodile-like reptiles) lived as far north as the Canadian Arctic, and warm-temperature forests thrived near the South Pole.

Another hothouse period was the Paleocene-Eocene Thermal Maximum (PETM) about 55-56 million years ago. Though not quite as hot as the Cretaceous hothouse, the PETM brought rapidly rising temperatures. During much of the Paleocene and early Eocene, the poles were free of ice caps, and palm trees and crocodiles lived above the Arctic Circle.

Around the time of the Paleocene-Eocene Thermal Maximum, much of the continental United States had a sub-tropical environment. This fossil palm is from Fossil Butte National Monument, Wyoming. Image courtesy U.S. National Park Service.

During the PETM, the global mean temperature appears to have risen by as much as 5-8°C (9-14°F) to an average temperature as high as 73°F. (Again, today&#;s global average is shy of 60°F.) At roughly the same time, paleoclimate data like fossilized phytoplankton and ocean sediments record a massive release of carbon dioxide into the atmosphere, at least doubling or possibly even quadrupling the background concentrations.

Global surface temperatures were generally high throughout the Paleocene and Eocene, with a particularly warm spike at the boundary between the two geological epochs around 56 million years ago. Temperatures in the distant past are inferred from proxies, in this case, oxygen isotope ratios from fossil foraminifera, single-celled marine organisms. "Q" stands for Quaternary. Graphic produced using data from Zachos and Hansen, with help from Dr. Carrie Morrill, Director of the World Data Service for Paleoclimatology.

It is still uncertain where all the carbon dioxide came from and what the exact sequence of events was. Scientists have considered the drying up of large inland seas, volcanic activity, thawing permafrost, release of methane from warming ocean sediments, huge wildfires, and even&#;briefly&#;a comet.

Like nothing we&#;ve ever seen

Earth&#;s hottest periods&#;the Hadean, the late Neoproterozoic, the Cretaceous Hot Greenhouse, the PETM&#;occurred before humans existed. Those ancient climates would have been like nothing our species has ever seen.

Modern human civilization, with its permanent agriculture and settlements, has developed over just the past 10,000 years or so. The period has generally been one of low temperatures and relative global (if not regional) climate stability. Compared to most of Earth&#;s history, today is unusually cold; we now live in what geologists call an interglacial&#;a period between glaciations of an ice age. But as greenhouse-gas emissions warm Earth&#;s climate, it's possible our planet has seen its last glaciation for a long time.

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