Pleistocene Park

Pleistocene Park (Russian: Плейстоценовый парк) is a nature reserve south of Chersky in the Sakha Republic in northeastern Siberia, where an attempt is being made to recreate the northern steppe grassland ecosystem that flourished in the area during the last ice age.[1]

Contents

Goals

The effort is being led by Russian researcher Sergey Zimov,[2] with hopes to back the hypothesis that hunting, and not climate change, destroyed the wildlife.

The aim of Pleistocene Park is to recreate the ancient taiga/tundra grasslands that were widespread in the region during the last ice age. The key concept is that animals, more than temperature, maintained that ecosystem. This argument is the justification for rewilding Pleistocene Park's landscape with megafauna that was previously abundant in the area, as evidenced by the fossil record.

Progress and plans

In 1988, Yakutian horses were introduced as a first step in recreating the ancient landscape as horses were abundant back then. Over the years, as the horses multiplied, it was discovered that in areas where the horses grazed, mosses and weeds were replaced by grasses which rapidly began to spread as the range of the horses was enlarged.[2] In company of the horses are other forms of Pleistocene survivors which still reside in the local wilderness such as reindeer, snow sheep, elk and moose. However in order for full restoration of the ancient ecosystem to take place biodiversity must be increased and populations must rise to larger numbers than they are today. The next phase was the introduction of Wood bison or Wisent into the park as the fossil record shows that the extinct but closely related Steppe Wisent was present in large numbers, quite possibly well into the Holocene era. In September 2010 the musk-ox from Wrangel island were reintroduced.[3] Seven months later, red deers and wisents arrived in park ...[4] Other ungulates such as the yak or bactrian camel are hardy animals well adapted to the temperature fluctuations and have also been considered for introduction.

It has been proposed that the introduction of a variety of large herbivores will recreate their ancient ecological niches in Siberia and regenerate the Pleistocene terrain with its different ecological habitats such as taiga, tundra, steppe and alpine terrain.

The main object is however to recreate the extensive grasslands that covered the Beringia region in the late Pleistocene. This form of grassland (which is also known as Mammoth-tundra) was inhabited by a diverse set of large and medium herbivores. Back in the Pleistocene the area was populated by many species of grazers which assembled in large herds similar in size to those in Africa today. Species that roamed the great grasslands included the Woolly mammoth, Steppe wisent, Reindeer, Lena horse, Saiga antelope, Muskox.

At the edges of these large stretches of grassland there could be found more shrub-like terrain and dry conifer forests (similar to the taiga). In this terrain there was to be found the browsers of the Pleistocene. This group of megafauna included Woolly rhinoceros, Moose, Elk, Yukon wild ass, Bactrian camel. The more mountainous terrain was occupied by several species of mountain going animals like the Snow sheep.

Back in the Pleistocene there was also a great variety of carnivores as well. On the plains there were prides of beringian cave lion. These large cats were the apex predators of the region, but also shared their habitat with other predators such as grey wolf, cave hyena, homotherium, brown bear, wolverine and arctic fox.

On the edges of the grasslands ( in the shrubs and forests) were also brown bears, wolverines, cave bears, Eurasian Lynx, siberian tigers, Amur leopard and red fox.

Other herbivores which were abundant during the Pleistocene in this region but which are now faced with possible extinction in their remaining habitats is the saiga antelope which can form massive herds that keep the vegetation down.

The most controversial aspect of the reintroduction of species to the park are the carnivores. Most of these species are however already present in the region such as grey wolf, wolverines, Eurasian lynx, red fox and Eurasian brown bear. However there have been suggestions for the rewilding of more Pleistocene-like carnivores as there is a need for large carnivores to keep control over growing populations of herbivores. Suggestions include reintroducing the amur leopard which was present in the area up until historical times and which is now facing a bitter struggle for survival in a small habitat on the eastern coast of Russia.

The same has been proposed for the Siberian Tiger, which is one of the largest and most feared land carnivores on earth but which has suffered a fate similar to that of the Amur leopard with which it shares its range. Another carnivore possible for reintroduction is the spotted hyena, which in fact the famous cave hyena was a subspecies of. The former range of the cave hyena extended to nearly all of Eurasia and Africa, but the eradication of grasslands pushed back the spotted hyenas until Africa.

Perhaps the most controversial of all reintroductions is that of the Asiatic lion which is on the verge of extinction, surviving only in a small reservation in the Gir region of west India. Lions were once one of the most widespread of all species inhabiting all of the world's continents except Australia and Antarctica. Evidence of this is widespread with the existence of fossils from the European lion, the cave lion, the Beringian cave lion and the American lion. Evidence of lions surviving Siberian winter temperatures can be found in the famous zoo of Novosibirsk, which has kept African lions since the 1950s in out-door all-year enclosures. This proves that the concept of introducing wild animals to different climates than their native range is possible. Lions lived side by side with people for several millennia and it is only recently that many of them disappeared. The Romans and Greeks for instance reported the existence of lions in the Balkan mountains and northern Greece as recently as 100 AD. These dangerous but beautiful creatures roamed the northern grasslands of Russia with other large species of animals, some of which survive today, and many that sadly do not, such as Moose, reindeer, cave bear, cave hyena, siberian roe deer, woolly rhinoceros, siberian tiger, amur leopard, Homotherium, steppe wisent, irish elk, saiga antelope, muskox, Elasmotherium, yak, woolly mammoth, snow sheep, wolverine, Eurasian lynx and all the other smaller animals which in total comprise the massive richness of Siberian biodiversity.

The ideas are not however entirely restricted to existing megafauna. There are hopes that one day cloning technology will be advanced enough to recreate a woolly mammoth, a species which became extinct at the end of the last ice age. Recent evidence however suggests that they may have survived into the Holocene with isolated populations of dwarfed individuals surviving on remote islands in the arctic circle such as St. Paul's island and Wrangel island, both of which are situated very close to the location of Pleistocene Park. Evidence points out that these populations could have existed as recently as 1700 BC. Another candidate for cloning could be the woolly rhinoceros, or an elasmotherium, as there are many of their frozen carcasses in Siberia. If scientists cannot clone them however, they may use black rhinoceros to fill the ecological niche.

Size and administration

Pleistocene Park is a 160 km2 scientific nature reserve (zakaznik), owned and administered by a non-profit corporation, Pleistocene Park Association, consisting of the ecologists from the Northeast Science Station in Chersky and the Grassland Institute in Yakutsk. The reserve is surrounded by a 600 km2 buffer zone that will be added to the park by the regional government, once the animals have successfully established themselves.

Animals

Animals already present in the park:

Carnivores: Eurasian Lynx, Grey Wolf, Arctic Fox, Eurasian Brown Bear, Wolverine, Red Fox,

Herbivores: Reindeer, Elk, European Bison, Moose, Yakutian horse, Muskox

Animals considered or suggested for reintroduction:

Carnivores: Amur Leopard, Siberian Tiger, Asiatic Lion, Spotted Hyena (?)

Herbivores: Yak, Snow Sheep, Saiga antelope, Bactrian Camel, Siberian Roe Deer, Woolly Mammoth, Rhinoceros.

Similar projects

See also

References

  1. ^ "Pleistocene Park Underway: Home for Reborn Mammoths?", National Geographic, May 17, 2005, http://news.nationalgeographic.com/news/2005/05/0517_050517_pleistocene.html, retrieved 2009-04-20, ""... During the last ice age northeastern Siberia remained a grassy refuge for scores of animals, including bison and woolly mammoths. Then, about 10,000 years ago, this vast ecosystem disappeared as the Ice Age ended. Now, though, the Ice Age landscape is on its way back, with a little help from the Russian scientists who have established "Pleistocene Park." ..." 
  2. ^ a b Anna Meyer (2005), Hunting the double helix: how DNA is solving puzzles of the past, Allen & Unwin, ISBN 1741141079, http://books.google.com/?id=CBxhrHjECoUC, retrieved 2009-04-20, "... lies in the work of a Russian ecologist, Sergei Zimov, who hopes to recreate a 'mammoth steppe' in north-east Siberia, part of a 'Pleistocene Park.' Work on the project has begun, and so far there are horses, moose, reindeer and bison in the park. These animals are removing mosses and shrubs, ..." 
  3. ^ Diary of Nikita Zimov during the trip to Wrangel island in August-September 2010 (In Russian)
  4. ^ Diary of Nikita Zimov during the trip from Nignii Novgorod to Cherskii to bring wapiti in March-April 2011 (In Russian)

External links