After finally
having done a post on Bubalus murrensis,
it’s time to look at the extinct European wild ass, Equus hydruntinus. This enigmatic taxon once roamed Europe during
the Pleistocene until the a part of the Holocene, and its presence is therefore
interesting for “European rewilding”. This post is going to investigate its
systematic position, time and range, looks and reasons for extinction. And of
course which implications it has for the (re)introduction of megafauna here in
Europe.
But before
that, there is some (paleo-)equine terminology to learn:
caballines:
anything closer to horses than to other living equines (or: domestic horses
opposed to the Przewalski’s horse)
hemiones: E. hemionus plus E. kiang, which form a clade
stenonines:
Equus
stenonis plus similar equine remains from the Plio-Pleistocene.
asinines: anything
closer to the African wild ass E. asinus
than to other living equines.
Skull of E. hydruntinus from Crimea, taken from [4] |
Equus hydruntinus was a small equine with a gracile and
cursorial build. It has been difficult to classify it for a long time. The
remains were only sparse and mostly fragmentary, and it seemed that it showed a
mosaic of characters [1;2]. The elements used for a phylogenetic classification
based on skeletal morphology were mostly limb elements, tooth and – after two
almost complete crania were found [3,4] – also skull proportions. Because of this
morphological mosaic of characters, it has been variously classified as a
donkey relative, a zebra relative, hemione and stenonine [1] since it shares
characters with most Equus clades
with the exception of horses.
The
similarity to stenonine horses was based tooth characteristics [1], while its
leg bones and skull morphology was reminiscent of hemiones and asinines [1]. A
dental similarity with hemiones has also been pointed out, but also that there
seems to be a certain degree of polymorphism within equines [5], making this
feature less useful for evaluating systematic positions.
Nevertheless,
there is a general agreement that morphological characters suggest that Equus hydruntinus was a distinct
species, differing from but also resembling its Equus relatives in a number of features [5]. What is important to
note is that hydruntinus was
sympatric with other of species/subspecies in a number of regions, such as caballines,
asinines, E. h. hemionus and E. h. hemippus [5].
It is out of question that hydruntinus
was a horse due to the lack of morphological similarity. Its coexistence with sp.
hemionus subspecies sheds doubts on
the hypothesis that hydruntinus was a
member of this species because they would interbreed and merge together, even
if they occupy different ecologic niches. You will find no example of two
subspecies of a species inhabiting one and the same biotope. The idea that hydruntinus occupied a different
ecological niche is supported by its small size and different tooth morphology.
Even within the clade of hemionus + kiang, hydruntinus seems to be kind of a patchwork of characters: the
metapodials are as long as in the Kulan, the teeth and protocones are as small
as in the Syrian wild ass.
However,
since osteomorphologic characters alone are not ideal to create a solid
hypothesis on hydruntinus’ identity
due to intraspecific variation and the scarcity of the fossil/subfossil material.
Therefore, genetic studies are needed to help to clarify.
Orlando et
al. 2006 and 2009 did such studies using aDNA of the mitochondria. They found Equus hydruntinus showing no affinity to
the Burchell’s zebra and asses (2006)[3] to be nested within Equus hemionus
(2009)[2]. Together they share a 28-bp deletion in the mitochondrial HVR-1 gene
[2]. They conclude that the hydruntinus
therefore is a subspecies of Equus
hemionus. On the other hand, kulan/onager and kiang are regarded as
separate species because of different coat colour, morphology and karyotype yet
show poor mitochondrial differentiation [2] (the coat colour and karyotype of hydruntinus are not even accessible to
us). Another issue is that also the Grevy zebra is nested within the hemionus group (yet not showing the
28-bp deletion). Therefore Orlando et al. suggest that nuclear loci are needed
to further clarify the relationships of E.
hydruntinus.
Possible depiction of E. hydruntinus from the Chauvet cave (Bottom) |
What we
know from skeletal remains, including relatively recent finds of a nearly
complete skeleton from Iran and two well-preserved crania from Crimea [3], E. hydruntinus was a small equine
(smaller even than hemionus and hemippus) with gracile and cursorial
legs. The body was short and the backline, typically for wild asses, straight
or slightly convex. The muzzle was comparably short in the well-preserved
crania – this has been interpreted as an adaption to cold climate [3], but I
consider that premature because this based on pretty scanty data and equines
have much cranial variation [3]. As an ass, it very likely had long ears, a
short mane and its tail only had a short tassel on its end. But apart from
that, we do not know much about its outer appearance because it is not nearly
as often represented in coloured paintings as aurochs and wild horses are. There
is one coloured painting in Lascaux that may or not may be a wild ass, the
equine next to it is undefinable. Assuming it is E. hydruntinus, it might implicate it was of a dark brown colour. But
this is nothing but a weak hint, the European wild ass might have had any
colour nuance displayed by modern equines with a bay dun colour. There is
another possible depiction of E. hydruntinus
at Chauvet that shows a panel of wild horses plus an equine at the bottom which might be
an ass because of the different, ass-like head shape and possibly long ears. In
this case we might infer that E.
hydruntinus was of a darker colour with a clearly recognizalbe muzzle ring.
Or maybe it was another species of ass. Or maybe not an ass at all. The data is
simply not sufficient.
Obviously E. hydruntinus is morphologically and
genetically distinct enough to distinguish it from other members of the genus
and to reconstruct a geographic and geologic range. The species seemingly had
been existing since the Middle Pleistocene. In Europe, the main body of its geographic range was
Southern Europe, which also was a refuge for this and many other species during
the last glacial maximum [3]. Its northwards range during the Pleistocene was
restricted only by the ice sheaths. It went up was much north as UK or Germany
[3] in the past. Findings in Siberia that have been previously assigned to hydruntinus in fact turned out to be
related to Equus sussenbornensis, a
more basal species from Germany, with which it forms the now extinct group of
the sussemiones. Eastwards, its range reached as far as Iran[3],
where it coexisted with E. h. hemionius
but also Syria [3], where its range overlapped with the Syrian wild ass E. h. hemippus.
The
European wild ass died out comparably recently. It occurred in the subfossil
record until the Iron Ages. For example, there is a solid record of the species
in Neusiedl in the east of Austria (Pucher 1991 [6], Erich Pucher in personal
communication 2012). The hypothesis that Equus
hydruntinus is the mysterious “zebro” of the Iberian peninsular in historic
time has always been controversial. For once, the “zebro” was described as an equine
clear striping, while hemiones – which are most likely the closest relative of hydruntinus – do not show striped patterns,
only a very faint shoulder streak in some cases. The skeleton of the alleged
last zebro from the 17th century turned out to be a donkey [2]. So
there are no remains that suggest it survived beyond the Iron age.
The sites
where it was found suggest it was an animal of dry and open areas, like other
asses. In fact even the location in Austria where it was found, Neusiedl, is
sometimes described as a “small exclave of the Puszta”.
The fact
that Equus hydruntinus was not as prevalent in prehistoric art as other mammals
were might implicate that it was not that spectacular and important to humans and
not all too numerous. The last point is indeed supported by fossil and
subfossil evidence to a certain degree. By the Holocene, its range was apparently
highly fragmented [3] Probably this was originally the result of ecologic
changes at the end of the last glacial [7], but it was probably human hunting
and habitat loss that made it a true extinction process. Although it seems that
it was not one of the most important game species for humans, there is evidence
from several sites that this species was seized by man [7]. Particularly the
fact that the population seemingly began to drop from the Neolithic onwards is
indicative of human influence [7]. Therefore it is likely that the European
wild ass would have recovered from the ecological changes that occurred by the
end of the last glacial if there had not been anthropogenic factors, similar to
the case of giant deer [7] or the woolly mammoth. So it might still inhabit at
least some regions of Europe, particularly the dry and open ones. I cannot
speak for the Near and Middle East.
So my view
on wild asses in Europe is similar to that on water buffalo. I think it is O.K.
to use a closely related and ecologically probably similar species to replace hydruntinus in some regions, be it kulan
or onager (I favour kulan). But European reserves probably would do well
without them as well. Whether it would be an ecologic benefit I cannot say, but
it probably would do no harm either. But a claim that it is a “necessary
keystone species” would be, in my opinion, baseless. Regions that might be
best-suited for wild asses might be the Balkan, Eastern European steppe-like
environments such as the Hungarian Puszta, and probably also the Italian and
Iberian peninsular.
Literature
1. A.
Burke, V. Eisenmann, G.K. Ambler: The
systematic position of Equus hydruntinus, an extinct species of Pleistocene
equid. 2003.
2. L.
Orlando et al.: Revising the recent
evolutionary history of Equids using ancient DNA. 2009.
3. L.
Orlando et al.: Geographic distribution
of an extinct equid (Equus hydruntinus: Mammalia, Equidae) revealed by
morphological and genetical analyses of fossils. 2006.
4. E.N. van Asperen, K. Stefaniak, I. Proskurnyak, B. Ridush: Equids from the Emine-Bair-Khosar Cave (Crimea, Ukraine): co-occurrence of the stenoid Equus hydruntinus and the caballoid E. ferus latipes on skull and postcranial remains. 2012.
5. E.-M.
Geigl, T. Grange: Eurasian wild asses in
time and space: Morphological versus genetical diversity. 2012.
6. E.
Pucher: Erstnachweis des Europäischen
Wildesels (Equus hydruntinus, Regalia, 1907) im Holozän Österreichs. 1991.
7. J.J.
Crees, S.T. Turvey: Holocene extinction
dynamic of Equus hydruntinus, a late-surviving European megafaunal mammal. 2014.