Research Reveals Warmer Than Thought Pliocene Oceans
30.06.2014 06:01 Age: 13 min
The hottest regions of the tropical oceans were one to two degrees Celsius warmer than today during a period of warmth in the Pliocene epoch, three to five million years ago even though CO2 levels were similar, reports a paper published online in Nature Geoscience. This finding opposes previous suggestions that Pliocene tropical ocean temperatures were similar to today even though average global temperatures were three to four degrees higher. Researchers reconstructed the sea surface temperature history of parts of the tropical Indo-Pacific and Atlantic warm pools, using three indicators of past temperature recovered from marine sediments. They found that in the Pliocene, sea surface temperatures in these regions were warmer than today as would be expected in the warmer atmosphere.
Click to enlarge. Scanning electron microscopy (SEM) image of the fossilised shell of planktic foraminifer Globigerinoides ruber. Planktic foraminifera are a highly abundant group of unicellular calcifiers that live in surface or near-surface waters of the open ocean. Courtesy: Richard Abell
Higher concentrations of carbon dioxide (CO2) in the atmosphere cause warming not only at high latitudes but also across tropical regions, according to new research by scientists at the University of Bristol’s Cabot Institute and their collaborators.
The impact of the greenhouse gas CO2 on the Earth’s temperature is well established by climate models and temperature records over the past 100 years, as well as coupled records of carbon dioxide concentration and temperature throughout Earth history. However, past temperature records have suggested that warming is largely confined to mid-to-high latitudes, especially the poles, whereas tropical temperatures appear to be relatively stable: the tropical thermostat model.
The new results, published in Nature Geoscience, contradict those previous studies and indicate that tropical sea surface temperatures were warmer during the early-to-mid Pliocene, an interval spanning about 5 to 3 million years ago. In an accompanying News and Views article in the journal, Mark Pagani,director of the Yale Climate & Energy Institute, writes that “we are now left to explain an even warmer Pliocene world than previously assumed, even though that world was bathed in atmospheric CO2 concentrations very similar to today.”
The Pliocene is of particular interest because CO2 concentrations then were thought to have been about 400 parts per million, the highest level of the past 5 million years but a level that was reached for the first time last summer due to human activity. The higher CO2 levels of the Pliocene have long been associated with a warmer world, but evidence from tropical regions suggested relatively stable temperatures.
Project leader and Director of the Cabot Institute, Professor Richard Pancost said: “These results confirm what climate models have long predicted – that although greenhouse gases cause greater warming at the poles they also cause warming in the tropics. Such findings indicate that few places on Earth will be immune to global warming and that the tropics will likely experience associated climate impacts, such as increased tropical storm intensity.”
The scientists focussed their attention on the South China Sea which is at the fringe of a vast warm body of water, the West Pacific Warm Pool (WPWP). Some of the most useful temperature proxies are insensitive to temperature change in the heart of the WPWP, which is already at the maximum temperature they can record. By focussing on the South China Sea, the researchers were able to use a combination of geochemical records to reconstruct sea surface temperature in the past. Not all of the records agree, however, and the researchers argue that certain tools used for reconstructing past ocean temperatures should be re-evaluated.
The paper’s first author, Charlotte O’Brien added: “It’s challenging to reconstruct the temperatures of the ocean many millions of years ago, and each of the tools we use has its own set of limitations. That is why we have used a combination of approaches in this investigation. We have shown that two different approaches agree – but a third approach agrees only if we make some assumptions about how the magnesium and calcium content of seawater has changed over the past 5 million years. That is an assumption that now needs to be tested.”
The work was funded by the UK’s Natural Environment Research Council and is ongoing.
Dr Gavin Foster at the University of Southampton is particularly interested in coupling the temperature records with improved estimates of Pliocene carbon dioxide levels. He said: “Just as we continue to challenge our temperature reconstructions we must challenge the corresponding carbon dioxide estimates. Together, they will help us truly understand the natural sensitivity of the Earth system and provide a better framework for predicting future climate change.”
The western warm pools of the Atlantic and Pacific oceans are a critical source of heat and moisture for the tropical climate system. Over the past five million years, global mean temperatures have cooled by 3–4 °C. Yet, present reconstructions of sea surface temperatures indicate that temperature in the warm pools has remained stable during this time. This stability has been used to suggest that tropical sea surface temperatures are controlled by a thermostat-like mechanism that maintained consistent temperatures. Here we reconstruct sea surface temperatures in the South China Sea, Caribbean Sea and western equatorial Pacific Ocean for the past five million years, using a combination of the Mg/Ca-, TEX86H and U37k’ surface-temperature proxies. Our data indicate that during the period of Pliocene warmth from about 5 to 2.6 million years ago, the western Pacific and western Atlantic warm pools were about 2 °C warmer than today. We suggest that the apparent lack of warmth seen in the previous reconstructions was an artefact of low seawater Mg/Ca ratios in the Pliocene oceans. Taking this bias into account, our data indicate that tropical sea surface temperatures did change in conjunction with global mean temperatures. We therefore conclude that the temperature of the warm pools of the equatorial oceans during the Pliocene was not limited by a thermostat-like mechanism.
‘High sea surface temperatures in tropical warm pools during the Pliocene’ by Charlotte L. O’Brien, Gavin L. Foster, Miguel A. Martínez-Botí, Richard Abell, James W. B. Rae and Richard D. Pancost in Nature Geoscience
Read the abstract and get the paper here.
News release issued by the university of Bristol here.