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3.4. Southern chamois<br />

Rupicapra pyrenaica<br />

Summary<br />

The Southern chamois is now <strong>in</strong>creas<strong>in</strong>g <strong>in</strong> distribution<br />

and abundance across its range after recover<strong>in</strong>g<br />

from historical lows <strong>in</strong> population numbers<br />

caused by uncontrolled hunt<strong>in</strong>g. Management<br />

<strong>in</strong>terventions have <strong>in</strong>cluded a captive breed<strong>in</strong>g<br />

and <strong>in</strong>troduction programme implemented <strong>in</strong><br />

Italy, translocations <strong>in</strong> France and establish<strong>in</strong>g<br />

hunt<strong>in</strong>g reserves <strong>in</strong> Spa<strong>in</strong>. Whilst the outlook for<br />

the species as a whole rema<strong>in</strong>s positive, cont<strong>in</strong>ued<br />

monitor<strong>in</strong>g of disease outbreaks <strong>in</strong> France and<br />

Spa<strong>in</strong> and targeted conservation management <strong>in</strong><br />

Italy are key to ensur<strong>in</strong>g cont<strong>in</strong>ued success for the<br />

Southern chamois.<br />

Background<br />

General description of the species<br />

The Southern or Pyrenean chamois (Rupicapra<br />

pyrenaica) is a mounta<strong>in</strong> ungulate which occurs<br />

as three subspecies <strong>in</strong> southwest Europe [1] . It is<br />

one of two species <strong>in</strong> the Rupicapra genus which<br />

spread to Europe from Asia <strong>in</strong> the middle Pleistocene,<br />

and it was dur<strong>in</strong>g this period that the<br />

Southern chamois is thought to have diverged<br />

from older ancestors <strong>in</strong> western Europe to occupy<br />

its current distribution through adaptation to<br />

warmer climates [2] .<br />

Distribution <strong>in</strong> Europe<br />

S<strong>in</strong>ce the last glaciation, the Southern chamois<br />

occupied a large part of the Iberian Pen<strong>in</strong>sula [3] .<br />

Dur<strong>in</strong>g the Holocene, with a milder climate,<br />

presence became scarcer, and dur<strong>in</strong>g the last<br />

10,000 years further adaptation to mounta<strong>in</strong>ous<br />

environment, climate warm<strong>in</strong>g and hunt<strong>in</strong>g<br />

pressure reduced its range to today’s extent [4] . In<br />

the Holocene the Apenn<strong>in</strong>e chamois was found<br />

throughout the central southern Apenn<strong>in</strong>es, its<br />

range was then reduced to just the Abruzzo region,<br />

where a population of less than 40 <strong>in</strong>dividuals<br />

survived <strong>in</strong> what is now the Abruzzo, Latium and<br />

Molise National Park [5] .<br />

The species is currently fragmented <strong>in</strong>to<br />

three populations, which occur <strong>in</strong> the follow<strong>in</strong>g<br />

mounta<strong>in</strong>ous regions: the Cantabrian mounta<strong>in</strong>s<br />

of northern Spa<strong>in</strong> (Cantabrian chamois –<br />

subspecies parva); the Pyrenees <strong>in</strong> France, Spa<strong>in</strong><br />

and Andorra (Pyrenean chamois – subspecies<br />

pyrenaica); and three locations <strong>in</strong> the Apenn<strong>in</strong>e<br />

mounta<strong>in</strong> cha<strong>in</strong> <strong>in</strong> Italy (Apenn<strong>in</strong>e chamois –<br />

subspecies ornata) [1] .<br />

Habitat preferences and general densities<br />

Adapted to high altitude, the Southern chamois is<br />

found <strong>in</strong> rocky areas, alp<strong>in</strong>e meadows and forests<br />

accord<strong>in</strong>g to the season. The species has adopted<br />

an altitud<strong>in</strong>al migration strategy <strong>in</strong> response<br />

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