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Friday, November 16, 2012

Megafauna Extinction Debate Gets Heated


What is the oldest debate in Australian science? Probably, the argument over what caused extinction of our Pleistocene megafauna – the diprotodons, giant kangaroos, marsupial tapirs, über-echidnas and other big and bizarre creatures that used to live here.

In 1877 the great English anatomist Sir Richard Owen suggested that these big animals had been driven extinct by “the hostile agency of man”. That is, hunting did it, in a process we now call overkill. Other people responded that climate change must have been the cause, and it was on.

A string of recent studies from a wide range of disciplines – geochronology, palaeoecology, palaeontology, and ecological modelling – have supported Owen’s opinion. But the argument continues. Why?

The main reason is that many Australian archaeologists reject overkill. They have looked for direct evidence that people killed megafauna, and they haven’t found it. No great piles of bones around ancient campsites; no diprotodon skeletons with spears stuck in their ribs; no arsenal of specialised weapons for bringing down large prey. Very few archaeological sites even have remains of people and megafauna in close association.

Some archaeologists conclude that megafauna-hunting just did not happen, or if it happened it was rare and insignificant. Often this conclusion is stated with a ringing confidence that dismisses all non-archaeological evidence for overkill.

But they have not asked a crucial question: if people did hunt megafauna to extinction, how much evidence of killing should we now be able to get from archaeological sites? A new paper by archaeologists Todd Surovell and Brigid Grund suggests the answer to that question is “very little or none”.

Surovell and Grund point out, first, that the period when archaeological evidence of killing of megafauna could have been formed is a small fraction of the total archaeological record of Australia. People arrived here between about 50,000 and 40,000 years ago. This is also the interval during which animals like diprotodon disappeared. A comparison of archaeological and fossil dates suggests humans and megafauna overlapped for only about 4,000 years continent-wide, and modelling suggests that if hunting caused extinction it would have been all over in less than 1,000 years in any place.

This means that no more than 8%, perhaps as little as 2%, of the Australian archaeological record covers the period of human-megafauna interaction. The “smoking gun” evidence of overkill should therefore be rare. Surovell and Grund show that the problem of finding such evidence is even worse than that, for two reasons.

First, when people first arrived their populations were necessarily small. Living sites therefore occurred at low density. As population size grew exponentially, site density increased. So, the very earliest sites must be far rarer than later ones.

But if overkill happened, populations of megafauna would have been going down as humans went up: as the density of sites was rising the proportion of them that could have contained evidence of megafauna kills was falling. Thus, sites with potential to preserve that evidence are actually a tiny proportion, perhaps much less than .01%, of the total archaeological record.

Second, material in archaeological sites degrades with time due to breakdown, weathering and scavenging of bone and removal by erosion. Old sites are eventually buried under sediments. The probability of discovering archaeological sites from the earliest occupation of Australia is intrinsically much lower than for later times, and most of the contents of those sites will have disappeared.

In fact, the very oldest archaeological sites in Australia typically contain only a few stone tools. They can tell us very little about interaction of the first Australians with any animals or plants, let alone reveal a picture of megafauna-killing.

Our fundamental task as scientists is to test hypotheses using evidence. To test the overkill hypothesis, we need a kind of evidence that would differ according to whether the hypothesis is true or false. Obviously, if overkill did not happen, evidence of megafauna-killing should be rare in the archaeological record. But, Surovell and Grund’s analysis makes it clear that if overkill happened, we should still expect evidence of killing to be rare. Therefore, failure to find such evidence does not amount to a test of the overkill hypothesis.

This does not mean that archaeological evidence of killing (or absence of such evidence) is useless in testing the overkill hypothesis. Surovell and Grund show it can be useful, by comparing the archaeological records of Australia, North America and New Zealand. All three places lost their megafaunas when people arrived, but this happened a very long time ago in Australia, and very recently (700 years ago) in New Zealand. North America is intermediate, with human arrival and extinction from 14,000 to 13,000 years ago.

Applying the same logic to all three cases, we predict that if overkill caused megafaunal extinction in each place the archaeological evidence of killing should be abundant in New Zealand, rare in North America, and vanishingly rare in Australia. That is exactly what we find.

There is so much evidence showing New Zealand’s moa were heavily hunted that nobody doubts overkill was the main cause of their extinction. In North America, there are undoubted kill sites for mammoths, mastodons and a few other species, but this evidence is far thinner than in New Zealand. Australian archaeology is yet to reveal any convincing evidence for megafauna-killing.

So, far from disproving overkill, the archaeological evidence from Australia is actually consistent with the overkill hypothesis.

Source: The Conversation, Christopher Johnson

Friday, September 30, 2011

Anthropology 101: Environmental Changes and Technology During the Woodland and Archaic Period


What were the major environmental changes that took place in North America from the Paleo-Indian through the Woodland period?

During the Pleistocene glacial (20,000-16,000BC) most of the world’s water was locked in ice. The climate was windier and dryer even nearest to the ice sheets. Hunter-gatherers saw the first flora and fauna communities with the climatic shift.

As glaciers started to retreat in 16,000 BC, the temperatures started to rise and water levels changed. Consequently, there was a shift in ocean currents, wind patterns, and rainfall. Forests and plant resources started to expand and rivers formed terraces due to the changing sea level. Migrations took place north of southern forest types and the post - glacial temperatures peaked about 3000 BC when weather was warmer and drier than today.

What were the major technological developments during the archaic and the major technological developments during woodland periods?

During the Archaic period advances were made in polished stonework which gave way to new tools and assemblages including celts, axes, spear thrower weights, ornaments such as beads, effigies, pendants and plummets. The stone tools also allowed for a new technology called the atlatl, a spear thrower. Consequently, during the Archaic we see the emergence of fired clay -the first pottery- which was used as storage containers.

During the Woodland Period we see the emergence of ceramics and the bow and arrow, distinguished by smaller projectile points. One of the more important technological advances during the Woodland phase was the manufacture of pottery vessels which allowed direct-heat cooking and food storage, replacing the older practice of hot rock cooking. Mound building was also a major advancement during the Woodland Period because it represented a “switch from the scattered individual burials of earlier periods to a system of formal, periodic and planned periodic burials in mounds”.

Friday, March 4, 2011

Can Humans Survive In An Even Warmer World?



During the Pleistocene ice sheets close to 2 miles thick covered the earth, the ground temperature was much cooler, and sea temperatures were 3 to 4 degrees cooler than they are today.

Change of a single degree in ocean temperature can cause irreversible changes or cessation in the movement of ocean currents. Florida and the Bahamas are a perfect example used to demonstrate the drop in sea level during the Pleistocene.



As you can see by the picture, sea levels dropped close to 300 feet in Florida, exposing larger land mass, aiding large animals in their transition from South America to North America via the Great American Biotic Interchange (Florida Museum).

Pleistocene land mammals were probably the single most important food source for Upper Paleolithic humans. On the contrary, depending on who you talk to today, people are sustaining a healthy lifestyle by living off the land or eating a diet rich in meatless protein, such as legumes.

Grasslands and cooler environments are indeed favorable for large land mammals, as the case was with megafauna during the Pleistocene, but today we don’t depend on them for survival.

Although it’s easy to have faith in humankind that we will find a way in a warmer world, I can’t help but question the actual facts presented by NASA’s Goddard Institute for Space Studies. Read this excerpt from the article, Global Surface Temperature Change, by J. Hansen, R. Ruedy, M. Sato, and K. Lo, and see how your outlook for humans in a warmer world changes.

The 12-month running mean global temperature in the GISS analysis has reached a new record in 2010. The new record temperature in 2010 is particularly meaningful because it occurs when the recent minimum of solar irradiance (defined as the amount of radiant energy emitted by the Sun over all wavelengths that fall each second on 11 sq ft (1 sq m) outside the earth's atmosphere) is having its maximum cooling effect. At the time of this writing (July 2010) the tropical Pacific Ocean is changing from El Nino to La Nina conditions in the tropical Pacific Ocean. It is likely that global temperature for calendar year 2010 will reach a record level for the period of instrumental data, but that is not certain if La Nina conditions deepen rapidly (Hansen et al 2010).

Each decade that passes, global warming continues without any fear of slowing down. Temperature anomalies furnished by NASA and NOAA, effectively illustrate the never declining warming trend of the earth that is occurring on decadal time scales.

In essence, let’s consider our situation here in Florida. When temperatures rise to over 90°, what kind of clothing do you see people wearing? What if the temperature rose to 120°? 150°? and how about 200°? Is there any question in your mind whether you could cope in such conditions?

Unless there’s a way to shield our bodies from the sun, whether that’s by protective clothing or underground living spaces, I fail to see how we’d ever be prepared for such an event. We won’t experience these changes in our lifetime, but generations of humans, plants, and animal species after us might.

This is my opinion. So what's yours? Please leave comments below.

Resources

Global Surface Temperature Change
Florida Image

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