Autor: Michał Kazubski

ssaki epoki lodowcowej

ssaki epoki lodowcowej

Wielkie ssaki epoki lodowcowej - ekspozycja PAN Muzeum Ziemi

PAN MUZEUM ZIEMI W WARSZAWIE

WIELKIE SSAKI
EPOKI LODOWCOWEJ

Stań oko w oko z gigantami epoki lodowcowej!

Od 21 października 2026 r.  •  Biały Pałacyk  •  al. Na Skarpie 20/26, Warszawa

Szkielety wielkich ssaków epoki lodowcowej na wystawie

Podróż do świata prehistorycznych olbrzymów

Od 21 października 2026 r. w PAN Muzeum Ziemi w Warszawie można oglądać wystawę „Wielkie ssaki epoki lodowcowej”. Ekspozycja prezentowana w Białym Pałacyku przenosi zwiedzających w świat prehistorycznych olbrzymów, które niegdyś zamieszkiwały tereny dzisiejszej Polski, w tym Warszawy.

Na wystawie zobaczysz autentyczne skamieniałości oraz rekonstrukcje szkieletów wielkich ssaków w naturalnej wielkości. Prezentowane okazy przybliżają bogactwo fauny ciepło- i zimnolubnej, charakterystycznej dla okresów międzylodowcowych i lodowcowych.

Wśród najcenniejszych eksponatów

Słoń leśny

Palaeoloxodon antiquus

Szczątki odkryte przy ul. Leszno w Warszawie.

Nosorożec leśny

Stephanorhinus kirchbergensis

Najlepiej zachowana na świecie czaszka tego gatunku.

Drapieżniki epoki lodowcowej

Unikatowe kości lwa jaskiniowego (Panthera spelaea) i hieny jaskiniowej (Crocuta spelaea).

Makieta wystawy Wielkie ssaki epoki lodowcowej

Odkryj tajemnice klimatu i dawnych ekosystemów

Wystawa to nie tylko spotkanie z imponującymi prehistorycznymi zwierzętami, lecz także opowieść o zmianach klimatu i środowiska naturalnego. Dowiesz się, jak wyglądały tereny dzisiejszej Polski przed tysiącami lat, jak żyły ówczesne ssaki oraz w jaki sposób przystosowywały się do zmieniających się warunków klimatycznych.

Ekspozycja stanowi również uzupełnienie oferty edukacyjnej Muzeum Ewolucji Instytutu Paleobiologii PAN. To dobre miejsce do organizacji zajęć dla grup szkolnych, szczególnie w ramach lekcji biologii i geografii poświęconych m.in. zmianom klimatu, ekologii i ewolucji.

W stronę Muzeum Historii Naturalnej

Otwarcie wystawy jest kolejnym ważnym krokiem w kierunku utworzenia długo wyczekiwanego w Polsce Muzeum Historii Naturalnej.

Zaplanuj swoją wizytę

PAN Muzeum Ziemi w Warszawie
Biały Pałacyk, al. Na Skarpie 20/26

Godziny

Poniedziałek – Piątek: 9:00–16:00
Sobota – Niedziela: 10:00–16:00

Ostatnie wejście na pół godziny przed zamknięciem Muzeum.

Bilety

Bilet normalny: 16 zł
Bilet ulgowy: 12 zł
Bilet rodzinny: 40 zł
Asystent osoby z niepełnosprawnością: 1 zł

Bezpłatny wstęp: w każdy wtorek dla emerytów i rencistów (za okazaniem odpowiedniego dokumentu) oraz dla dzieci do ukończenia 5. roku życia.

Zapraszamy do odkrywania fascynującego świata wielkich ssaków epoki lodowcowej!

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GREAT MAMMALS OF THE ICE AGE

Cave lion

Panthera spelaea

Cave lion and giant deer

The cave lion was a close relative of today’s African lion (Panthera leo). Judging by cave paintings, however, the males appear to have had no mane. Despite its name, the cave lion did not live in caves. It was drawn into them by the prospect of relatively easy prey in the form of hibernating cave bears. Cave lions probably hunted alone or in pairs, taking prey such as steppe bison (Bison priscus), aurochs (Bos primigenius) and deer of the genera Megaloceros and Cervus.

Cave lions were adapted to a cold climate and probably had a thick coat with dense underfur to protect them from the cold. Neanderthals and modern humans hunted them for their skins and for their bones, which were made into tools. Cave lion canine teeth were made into ornaments such as necklaces and pendants.

The cave lion was an animal of open country. It died out at the end of the Pleistocene, probably because climate change caused the mammoth steppe to be replaced by forest and scrub. The youngest known remains of the species are dated to around 13,000 years ago.

Giant deer

Megaloceros giganteus

The giant deer is also known as the ‘Irish elk’, even though its closest living relatives are the fallow deer (genus Dama). It stood up to about 2 metres at the shoulder, and its spectacular antlers could span more than 4 metres and weigh as much as 40–45 kilograms.

Paintings in the French caves of Chauvet and Cougnac, dated to around 36,000 and 25,000–23,000 years ago respectively, depict giant deer with remarkable accuracy, faithfully rendering their outline, antlers and coat markings.

The giant deer ranged across much of Europe and southern Siberia, reaching as far east as the area around Lake Baikal. Particularly large numbers of its remains have been found in Ireland, including impressive examples of its enormous antlers. In the nineteenth and early twentieth centuries, giant deer antlers found their way into private collections, museums and aristocratic houses. The animal also appeared on the historical coat-of-arms of Northern Ireland, granted in 1924.

As an animal of open country, the giant deer saw its range shrink considerably at the start of the Holocene, when dense forest rapidly spread. The youngest known remains of the species are dated to around 7,700–7,600 years ago and come from the Ural region of western Russia.

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GREAT MAMMALS OF THE ICE AGE

Cave bear

Ursus spelaeus

Cave bear

The cave bear lived in Europe alongside the brown bear (Ursus arctos), to which it was closely related, and was of comparable size. Plants made up a greater part of the cave bear’s diet than of the brown bear’s. Cave bears are also thought to have spent more time in caves than brown bears, which used them mainly for hibernation.

Many cave bears died during hibernation, especially individuals that had fared poorly over the summer through inexperience, illness or old age, and so lacked the reserves to survive the winter. Skeletons of adult cave lions found deep inside cave bear dens suggest that lions sometimes ventured inside to prey on hibernating bears. Some of the lions probably also died in the attempt.

The cave bear died out around 24,000 years ago, during one of the coldest phases of the Vistulian glaciation. It is known to have been hunted by humans from time to time, which has led to the hypothesis that bears and humans competed for shelter in caves. Pressure from humans may therefore have been one of the causes of the species’ extinction.

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GREAT MAMMALS OF THE ICE AGE

Woolly mammoth

Mammuthus primigenius

Woolly mammoth

The woolly mammoth was about the size of today’s African elephant (Loxodonta africana). The largest males stood about 3.5 metres at the shoulder and weighed over 8 tonnes. Females were somewhat smaller. The woolly mammoth’s closest living relative is the Asian elephant (Elephas maximus).

In what is now Poland, the mammoth’s natural predators were the large sabre-toothed cats of the genus Homotherium, as well as cave lions and cave hyenas, which hunted mainly young animals.

Modern humans (Homo sapiens) encountered woolly mammoths as they spread out of Africa into Eurasia around 50,000 years ago. Mammoths provided people with meat, hides and bones; the bones were used to make tools and to build simple, round dwellings covered with hides. Mammoth tusks were carved into figurines, pendants and other objects, including the ceremonial boomerang found in Obłazowa Cave in southern Poland.

The ancestors of the Indigenous peoples of North America also hunted mammoths. With the environmental changes of the early Holocene, however, and after the disappearance of the mammoths and other megafauna, bison became one of the most important game animals on the vast plains of North America, although people had been hunting them before then.

The woolly mammoth survived the climatic changes at the end of the Pleistocene, but its populations shrank rapidly and retreated northwards. The last woolly mammoths lived on Wrangel Island in the Arctic Ocean until about 4,000 years ago. By then, writing had already been in use in Mesopotamia and Egypt for more than a thousand years.

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GREAT MAMMALS OF THE ICE AGE

Woolly rhinoceros

Coelodonta antiquitatis

Woolly rhinoceros

The woolly rhinoceros descended from the Tibetan woolly rhinoceros (Coelodonta thibetana) and was a close relative of the living Sumatran rhinoceros (Dicerorhinus sumatrensis). Unlike its relatives, however, it was adapted to far harsher climatic conditions. The woolly rhinoceros also had the largest range of any rhinoceros species, from Scotland and Spain in the west to Korea and China in the east. It fed on the low-growing plants of the mammoth steppe, a type of vegetation that covered vast areas of Eurasia and North America during the colder, glacial phases of the Pleistocene. Adults measured 3 to 3.8 metres in length, stood about 2 metres at the shoulder and could weigh more than 2 tonnes. Woolly rhinos used their horns to sweep away snow and expose plants in winter, and also to fight with one another, a scene captured in cave paintings.

The species probably died out around 14,000 years ago as a result of warmer climate conditions at the end of the Pleistocene, loss of habitat and hunting. Woolly rhinos were hunted by both Neanderthals and modern humans, and their horns and bones were used to make tools and weapons.

At the Natural History Museum of the Institute of Systematics and Evolution of Animals, Polish Academy of Sciences, in Kraków, visitors can see the superbly preserved, naturally mummified remains of a woolly rhinoceros that lived around 30,000 years ago. They were discovered in 1929 in an ozokerite (earthwax) mine in the village of Starunia, near what was then the town of Stanisławów (now known as Ivano-Frankivsk in Ukraine).

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GREAT MAMMALS OF THE ICE AGE

Aurochs

Bos primigenius

Aurochs

The aurochs was the wild ancestor of modern domestic cattle (Bos taurus) and zebu (Bos indicus).

During glacial periods, aurochs retreated to refugia: areas in southern Europe where they could survive the colder climatic conditions. These included the Iberian, Italian and Balkan peninsulas. The species survived the extinctions at the end of the Pleistocene, and in the Holocene still ranged over vast areas, from western Europe and North Africa to East Asia. Its numbers gradually declined because of hunting, the loss and fragmentation of its habitat as farming and herding spread, and interbreeding with domestic cattle. The last known aurochs was a female living in the Jaktorów Forest in central Poland, which died in 1627. Her death is regarded as marking the extinction of the species.

Aurochs were a common subject of rock art and cave paintings. In ancient Egypt, a relief from the 12th century BC in the mortuary temple of Ramesses III at Medinet Habu shows the pharaoh hunting wild bulls identified as aurochs.

In Roman times, aurochs were among the wild animals brought in for venationes – staged hunts in which animals were pursued and killed in the arena. Such spectacles were held in the Colosseum in Rome and elsewhere, and many other species were also used, including lions, leopards, bears, elephants and rhinoceroses.

For centuries, the aurochs has been associated with strength, courage and extraordinary vitality, which explains its popularity in heraldry.

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GREAT MAMMALS OF THE ICE AGE

Straight-tusked elephant

Palaeoloxodon antiquus

Straight-tusked elephant

Elephants of the genus Palaeoloxodon, such as P. recki, P. namadicus and P. antiquus, were among the largest land mammals that ever lived. The European straight-tusked elephant, Palaeoloxodon antiquus, could stand around 4.2 metres at the shoulder and weigh up to 15 tonnes, and some estimates suggest that the species P. namadicus may have been even larger. By comparison, the largest bulls of modern-day African elephants (Loxodonta africana) stand about 3.4 metres at the shoulder and can weigh up to about 7 tonnes.

Intriguingly, dwarf species of elephant evolved on islands in the Mediterranean. Their distinctive skulls, found in caves, may have inspired the legend of the Cyclops: the large opening at the front of the skull, where the trunk was attached, could easily have been mistaken for the socket of a single eye. The species Palaeoloxodon falconeri, from Sicily and Malta, was tiny – adult males stood about 1 metre at the shoulder and weighed around 250 kilograms.

The straight-tusked elephant Palaeoloxodon antiquus lived in Europe, Anatolia and the Middle East. Being a warmth-loving species, it spread northwards during interglacials and retreated to southern Europe during glacials. The last populations survived on the Iberian Peninsula until around 28,000 years ago. Neanderthals and other early humans (genus Homo) hunted straight-tusked elephants and butchered their carcasses for meat.

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GREAT MAMMALS OF THE ICE AGE

Merck’s rhinoceros

Stephanorhinus kirchbergensis

Merck’s rhinoceros

Merck’s rhinoceros – also known as the forest rhinoceros – was similar in size to the woolly rhinoceros and was one of its close relatives. It lived in Europe and in Central and East Asia, in both forests and more open landscapes.

At fossil sites it is often found together with the straight-tusked elephant (Palaeoloxodon antiquus). Like the elephant, it died out during the last glaciation. It survived longest in East Asia, perhaps until as recently as about 14,000 years ago.

The remains of an exceptionally large Merck’s rhinoceros were discovered in 2016 during construction of an expressway in Gorzów Wielkopolski, western Poland. The animal stood more than 1.8 metres at the shoulder, and its diet included hazel, hornbeam, mistletoe and birch.

Neanderthals hunted Merck’s rhinoceroses and used their bones and teeth as tools.

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GREAT MAMMALS OF THE ICE AGE

The Vistulian Glaciation

115,000–11,700 years ago

Vistulian glaciation landscape

During the Vistulian glaciation, the northern part of present-day Poland lay beneath an ice sheet. In the ice-free areas, steppe-tundra developed, dominated by grasses and other herbaceous plants, along with shrubby willows (Salix). This ‘mammoth steppe’, as it is called, provided vast grazing lands not only for the woolly mammoth (Mammuthus primigenius), but also for the woolly rhinoceros (Coelodonta antiquitatis), musk ox (Ovibos moschatus), steppe bison (Bison priscus) and reindeer (Rangifer tarandus). During the Last Glacial Maximum (26,000–20,000 years ago) the climate became especially harsh, and over large areas the steppe-tundra gave way to polar desert.

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GREAT MAMMALS OF THE ICE AGE

The Eemian Interglacial

130,000–115,000 years ago

Eemian interglacial landscape

The Eemian (also known as the Riss–Würm interglacial, among other local names) was one of the warmest interglacials of the last 800,000 years. One indication of what the climate was like at the time is the range of the common hippopotamus (Hippopotamus amphibius) – the same species that lives in Africa today – whose fossils have been found across much of Europe, as far north as Yorkshire in northern England.

Present-day Poland was then covered by forests dominated by deciduous trees such as oak, lime, hornbeam and elm, with shrubs including hazel. Holly and boxwood also grew here. The warm, humid climate supported numerous lakes. Mammal remains from this period are often found in lake sediments, which favoured the preservation of bone. Animals living in Poland during the Eemian included the huge straight-tusked elephant (Palaeoloxodon antiquus) and Merck’s rhinoceros (Stephanorhinus kirchbergensis), as well as species still found here today, such as red deer (Cervus elaphus), roe deer (Capreolus capreolus) and wild boar (Sus scrofa).