Neanderthals in Gibraltar
The Neanderthals in Gibraltar were among the first to be discovered by modern scientists and have been among the most well studied of their species according to a number of extinction studies which emphasize regional differences, usually claiming the Iberian Peninsula partially acted as a “refuge” for the shrinking Neanderthal populations and the Gibraltar population of Neanderthals as having been one of many dwindling populations of archaic human populations, existing just until around 42,000 years ago. Many other Neanderthal populations went extinct around the same time.
The skull of a Neanderthal woman, discovered in a quarry in 1848, was only the second Neanderthal skull ever found and the first adult Neanderthal skull to be discovered, eight years before the discovery of the skull for which the species was named in Neandertal, Germany; had it been recognised as a separate species, it might have been called Calpican rather than Neanderthal Man. The skull of a Neanderthal child was discovered nearby in 1926. The Neanderthals are known to have occupied ten sites on the Gibraltar peninsula at the southern tip of Iberia, which may have had one of the densest areas of Neanderthal settlement of anywhere in Europe, although not necessarily the last place of possible habitation.
The caves in the Rock of Gibraltar that the Neanderthals inhabited have been excavated and have revealed a wealth of information about their lifestyle and the prehistoric landscape of the area. The peninsula stood on the edge of a fertile coastal plain, now submerged, that supported a wide variety of animals and plants which the Neanderthals exploited to provide a highly varied diet. Unlike northern Europe, which underwent massive swings in its climate and was largely uninhabitable for long periods, the far south of Iberia enjoyed a stable and mild climate for over 125,000 years. It became a refuge from the ice ages for animals, plants and Neanderthals. Around 42,000 years ago, the climate underwent cycles of abrupt change which would have greatly disrupted the Gibraltar Neanderthals' food supply and may have stressed their population beyond recovery, leading to their aggregated extinction in areas of Europe with similar climates.
Fossil discoveries
The Gibraltar Neanderthals first came to light in 1848 during excavations in the course of the construction of a fortification called Forbes' Barrier at the northern end of the Rock of Gibraltar. The skull of a Neanderthal was discovered in Forbes' Quarry by Lieutenant Edmund Flint, though its exact provenance is unknown, and was the subject of a presentation to the Gibraltar Scientific Society by Lieutenant Flint in March 1848. It was not realised at the time that the skull, now known as Gibraltar 1, was of a separate species and it was not until 1862 that it was studied by palaeontologists George Busk and Hugh Falconer during a visit to Gibraltar. They gave a report on it to the British Association for the Advancement of Science in 1864 and proposed that the species be called Homo calpicus after Mons Calpe, the ancient name for Gibraltar. It was only later realised that the skull was a specimen of Homo neanderthalensis, which had been named for the Neanderthal 1 skull found in Germany in 1856. Busk described it as "characteristic of a race extending from the Rhine to the Pillars of Hercules", highlighting its importance as confirmation that the Neanderthal 1 specimen was genuinely a member of a distinct species and not simply a deformed Homo sapiens.The skull was the first Neanderthal adult cranium to be discovered and, although small, is nearly complete; it is thought to have belonged to a woman due to its gracile features. In 1926, a second Neanderthal skull was found by Dorothy Garrod at a rock shelter named Devil's Tower, very close to Forbes' Quarry. This fossil, known as Gibraltar 2, is much less complete than the Gibraltar 1 skull and has been identified as that of a four-year-old child. Further excavations at the two sites are infeasible. Quarrying at Forbes' Quarry has meant that it has been virtually denuded of Pleistocene sediments while Devil's Tower is directly under the North Front of the Rock of Gibraltar and is one of the most dangerous places on the entire peninsula due to frequent rockfalls.
Occupation sites
The limestone massif of the Rock of Gibraltar is riddled with caves – its ancient name, Calpe, means "hollow" – and it was here that archaeologists focused their efforts to find sites of Neanderthal occupation. Ten such sites have been discovered so far, of which the most important are five caves on the eastern side of the Rock: Ibex Cave, high up on the east side, which was only discovered in 1975 due to being buried under the wind-blown sands of the Great Gibraltar Sand Dune, and four sea caves near sea level on the south-eastern flank: Boathoist Cave, Vanguard Cave, Gorham's Cave and Bennett's Cave.Large-scale excavations in 1947–54 by John d'Arcy Waechter showed that Gorham's Cave had been occupied for over 100,000 years during the Middle Palaeolithic, Upper Palaeolithic and Holocene epochs. Further excavations have been carried out in Gorham's, Vanguard and Ibex Caves since 1994 as part of the Gibraltar Museum's Gibraltar Caves Project. The excavations have revealed possibly the best evidence of a Neanderthal landscape found anywhere, buried under many metres of sand, fallen stalactites, bat guano and other debris that has fortuitously preserved an abundance of palaeontological evidence on the cave floors. The finds have enabled palaeontologists to reconstruct the lifestyles of the occupants and their environment in considerable detail.
The finds in Gorham's Cave include charcoal, bones, stone tools and burnt seeds dating from the Middle to Upper Palaeolithic periods, while Vanguard Cave contains Pleistocene and Middle Palaeolithic deposits. When Ibex Cave was discovered in 1975, fifty artifacts from the Middle Pleistocene period were found on the surface along with vertebrate remains and shells. Neanderthal tools were found in an excavation carried out there in 1994 by the Gibraltar Caves Project, though occupation of the cave seems to have been sporadic. Most of the stone tools appear to have been deposited during a single period of occupation, perhaps as short as a single day.
In July 2012, archaeologists discovered an engraving in Gorham's Cave, buried under 39,000-year-old sediments, which has been called "the oldest known example of abstract art". Consisting of a series of intersecting lines, the engraving is located about inside the cave on a ledge that is thought to have been used by Neanderthals as a sleeping place. Its meaning is not known but researchers have described it as providing the first evidence that Neanderthals had the cognitive ability to produce abstract art. The engraving was clearly made deliberately, rather than being an accidental by-product of another process such as cutting meat or fur, and would have taken a significant amount of effort to carve into the dolomite rock of the cave.
Gibraltar in prehistory
Pleistocene Gibraltar was physically very different from today. During the ice ages, the much greater volume of water locked up in the polar ice caps and continental glaciers meant that sea levels were far lower than in the present day. In the late Pleistocene period, when Neanderthals inhabited Gibraltar, the sea level was as much as lower than today. The drop in sea levels exposed a coastal plain which considerably increased the size of the Gibraltar peninsula. The Bay of Gibraltar, to the west, was considerably smaller than it is today and was probably an estuary, while the eastern coast of the peninsula would have extended out around to east of the modern shoreline. Another small estuary to the north-east of Gibraltar would have marked the northern boundary of the peninsula's extended shoreline. Whereas modern Gibraltar is only in size, the Pleistocene coastal plain would have added about another.The entire coastal plain is now submerged in the Bay of Gibraltar, Strait of Gibraltar and Alboran Sea due to the rise in sea levels over the last 12,000 years, but its environment can be reconstructed in detail from the evidence of pollen, seeds and animal bones found in the caves of Gibraltar. It would have predominantly been a sandy grassland with patchy trees and shrubs, supporting a wide variety of flora and fauna. The wildlife included important game species – red deer, wild cattle, rabbits and wild boars – and predators including spotted hyenas, leopards, lynxes, wolves, brown bears, wildcats and possibly lions. Gibraltar was, then as now, a key waypoint on the avian migration route between Europe and Africa and a very wide variety of birds were present. Bones from the caves indicate the widespread presence of scavengers such as various species of vulture and waterbirds that would have lived in the estuarine areas of the plain. The general appearance of the habitat was similar to that of the present-day Doñana National Park, north-west of Gibraltar.
The region enjoyed a much more stable and temperate climate than almost anywhere else in Iberia. The range of the climate of prehistoric Gibraltar can be deduced from proxies such as the remains of animals that are very sensitive to heat and humidity, such as Hermann's tortoise, which depends on a mean annual temperature of for its eggs to hatch and a rainfall of no more than annually. Whereas northern Europe underwent massive climatic swings between temperate and extreme glacial conditions, which made large areas of the continent uninhabitable for extended periods, Gibraltar's prehistoric climate appears to have been largely unaffected by such changes. The iconic ice age mammals of northern Europe – woolly rhinos, mammoths, bison, reindeer, muskox and cave bears – never made it as far south as Gibraltar, which enjoyed a temperate and stable year-round climate due to its southerly latitude, distance from the coastal mountains and position on the Mediterranean shore. As a result, it became a kind of "Africa in Europe" where animals, plants and Neanderthals were able to shelter from the worst effects of the ice ages.