¿La edad de hielo tuvo efecto en el desarrollo cerebral?

ORIGINAL: NewScientist.com
by Bob Holmes
29 July 2009

Estudios sugieren que cambios (disminución) de la temperatura ambiental tuvieron efecto positivo en el desarrollo cerebral. ¿El cambio climático actual qué podría causar?

Did an ice age boost human brain size?

IT IS one of the biggest mysteries in human evolution. Why did we humans evolve such big brains, making us the unrivalled rulers of the world?

Some 2.5 million years ago, our ancestors' brains expanded from a mere 600 cubic centimetres to about a litre. Two new studies suggest it is no fluke that this brain boom coincided with the onset of an ice age. Cooler heads, it seems, allowed ancient human brains to let off steam and grow.

Cooler heads, it seems, allowed ancient human brains to let off steam and grow

For all its advantages, the modern human brain is a huge energy glutton, accounting for nearly half of our resting metabolic rate. About a decade ago, biologists David Schwartzman and George Middendorf of Howard University in Washington DC hypothesised that our modern brain could not have evolved until the Quaternary ice age started, about 2.5 million years ago. They reckoned such a large brain would have generated heat faster than it could dissipate it in the warmer climate of earlier times, but they lacked evidence to back their hypothesis.

Letting off some steam (Image: Doug Allan/Getty)

Letting off some steam (Image: Doug Allan/Getty)

Now hints of that evidence are beginning to emerge. Climate researcher Axel Kleidon of the Max Planck Institute for Biogeochemistry in Jena, Germany, modelled present-day temperature, humidity and wind conditions around the world using an Earth-systems computer model. He used these factors to predict the maximum rate at which a modern human brain can lose heat in different regions. He found that, even today, the ability to dissipate heat should restrict the activity of people in many tropical regions (Climatic Change, vol 95, p 405).

If keeping cool is a problem now, Kleidon says, it would have been even more challenging - perhaps too challenging - 2 or 3 million years ago when temperatures were a few degrees warmer than today and air-conditioning units were harder to come by.

A new study by Schwartzman and Middendorf suggests that a small drop in global temperatures may have made a big difference. The pair used basic equations of heat loss to estimate how fast the small-brained Homo habilis would have been able to cool off. Assuming overheating limited the size of H. habilis's brain, they then calculated what drop in air temperature would have been needed for Homo erectus to be able to support its bigger brain (see diagram). They found that a drop in air temperature of just 1.5 °C would have done the trick (Climatic Change, vol 95, p 439).

Given the timescales involved, it may be near-impossible to match definitively the onset of an ice age with speciation, but a 1.5 °C drop is consistent with the cooling climate of the time, says Middendorf.

"In principle, I'm receptive to the hypothesis," says Dean Falk, a palaeoanthropologist at Florida State University in Tallahassee, "but I need the data." She says that if measurements showed that people living in tropical countries today have smaller brains relative to their body size than people in temperate climates, this would go against expectation and lend support to Kleidon's model.

Being able to cool bigger brains can only be part of the story, however. It would have lifted the brakes on expansion, says psychologist David Geary at the University of Missouri in Columbia, but there has to be something driving the increase.

Over the years, researchers have come up with three broad reasons why bigger brains might have been advantageous:

  • to give their owners the ability to cope with changing climates by exploiting technologies such as shelter, fire and clothing;
  • to deal with the cognitive demands of hunting and gathering; or
  • to help people outsmart their neighbours.

To help narrow this down, Geary collected data from 175 fossil hominin skulls, from 1.9 million to 10,000 years old. Then he looked to see whether brain size was best correlated with climatic variability - a crude measure of biodiversity which could indicate the complexity of hunting and gathering - or the human population size at the time, which could reflect the complexity of social interactions.

The brain chill factor

Geary's analysis found that population size was the best predictor of brain size, suggesting that our ancestors' need to outcompete their neighbours in order to survive may have been the strongest driver of brain growth (Human Nature, vol 20, p 67).

The case is far from closed - Geary's study does not demonstrate cause and effect, for one thing - but the picture beginning to emerge suggests that an ice age set the stage for a socially driven brain boom. And from that time on, it was the brainiacs who stole the show.

Greenhouse brains

If global cooling allowed humans to evolve their big brains, will today's global warming take them away again? "I'd hate to think that a difference of 1.5 °C might mean the end of humans because our brains cook," says George Middendorf of Howard University in Washington DC, "but I guess it's a scenario that might play out."

It probably won't, though, thanks to what those big human brains made possible: culture.

"When culture comes in, it layers itself on top of the biological constraints," says Tyler Volk, an Earth-systems expert at New York University. Thanks to culture and technology, we now have ways of buffering ourselves against hot climates, not only with air conditioning, but also with basic tools such as fans, thick-walled buildings and reservoirs to ensure we have plenty of water.

Only one thing could destroy that buffer - a total breakdown of society.


Full Article:

Abstract:
No matter what humans do, their levels of metabolic activity are linked to the climatic conditions of the land surface. On the one hand, the productivity of the terrestrial biosphere provides the source of chemical free energy to drive human metabolic activity. On the other hand, human metabolic activity results in the generation of heat within the body. The release of that heat to the surrounding environment is potentially constrained by the climatic conditions at the land surface. Both of these factors are intimately linked to climate: Climatic constraints act upon
the productivity of the terrestrial biosphere and thereby the source of free energy, and the climatic conditions near the surface constrain the loss of heat from the human body to its surrounding environment. These two constraints are associated with a fundamental trade-off, which should result in a distinct maximum in possible levels of human metabolic activity for certain climatic conditions. For present-day conditions, tropical regions are highly productive and provide a high supply rate of free energy. But the tropics are also generally warm and humid, resulting in a low ability to loose heat, especially during daylight. Contrary, polar regions are much less productive, but allow for much higher levels of heat loss to the environment. This trade-off should therefore result in an optimum latitude (and altitude) at which the climatic
environment allows humans to be metabolically most active and perform maximum levels of physical work. Both of these constraints are affected by the concentration of atmospheric carbon dioxide pCO2, but in contrary ways, so that I further hypothesize that an optimum concentration of pCO2 exists and that the optimum latitude shifts with pCO2. I evaluate these three hypotheses with model simulations of an Earth system model of intermediate complexity which includes expressions for the two constraints on maximum possible levels of human metabolic activity. This model is used to perform model simulations for the present-day and sensitivity experiments to different levels of pCO2. The model simulations support the three hypotheses and quantify the conditions under which these apply. Although the quantification of
these constraints on human metabolic activity is grossly simplified in the approach taken here, the predictions following from this approach are consistent with the geographic locations of where higher civilizations first emerged. Applied to past climatic changes, this perspective can explain why major evolutionary events in human evolutionary history took place at times of global cooling. I conclude that the quantification of these constraints on human metabolic activity is a meaningful and quantitative measure of the “human habitability” of the Earth’s climate. When anthropogenic climate change is viewed from this perspective, an important implication
is that global warming is likely to lead to environmental conditions less suitable for human metabolic activity in their natural environment (and for large mammals in general) due to a lower ability to loose heat.

Comments