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Neanderthal
Temporal range: MiddleLate Pleistocene 0.43/0.25–0.04 Ma
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Homo sapiens neanderthalensis.jpg
Late Neanderthal skull
(La Chapelle-aux-Saints 1)
Neanderthalensis.jpg
An approximate reconstruction of a Neanderthal skeleton. The central rib cage, including the sternum, and parts of the pelvis are from modern humans.
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Primates
Suborder: Haplorhini
Infraorder: Simiiformes
Family: Hominidae
Subfamily: Homininae
Tribe: Hominini
Genus: Homo
Species:
H. neanderthalensis
Binomial name
Homo neanderthalensis
King, 1864
Range of NeanderthalsAColoured.png
Known Neanderthal range in Europe (blue), Southwest Asia (orange), Uzbekistan (green), and the Altai mountains (violet).
Synonyms
Homo stupidus (Haeckel 1866)
Homo mousteriensis (Klaatsch 1909)
Palaeoanthropus neanderthalensis


Neanderthals, Homo neanderthalensis or Homo sapiens neanderthalensis) are an extinct species or subspecies of archaic humans in the genus Homo, who lived within Eurasia from circa 400,000 until 40,000 years ago.

Currently the earliest fossils of Neanderthals in Europe are dated between 450,000 and 430,000 years ago, and thereafter Neanderthals expanded into Southwest and Central Asia. They are known from numerous fossils, as well as stone tool assemblages. Almost all assemblages younger than 160,000 years are of the so-called Mousterian techno-complex, which is characterised by tools made out of stone flakes. The type specimen is Neanderthal 1, found in Neander Valley in the German Rhineland, in 1856.

Compared to modern humans, Neanderthals were stockier, with shorter legs and bigger bodies. In conformance with Bergmann's rule, as well as Allen's rule, this was likely was an adaptation to preserve heat in cold climates. Male and female Neanderthals had cranial capacities averaging 1,600 cm3 (98 cu in) and 1,300 cm3 (79 cu in), respectively, within the range of the values for anatomically modern humans. Average males stood around 164 to 168 cm (65 to 66 in) and females 152 to 156 cm (60 to 61 in) tall.

There has been growing evidence for admixture between Neanderthals and anatomically modern humans, reflected in the genomes of all modern non-African populations but not in the genomes of most sub-Saharan Africans. This suggests that interbreeding between Neanderthals and anatomically modern humans took place after the recent "out of Africa" migration, around 70,000 years ago. Recent admixture analyses have added to the complexity, finding that Eastern Neanderthals derived up to 2% of their ancestry from anatomically modern humans who left Africa some 100,000 years ago.

Name and classification

Neanderthals are named after one of the first sites where their fossils were discovered in the mid-19th century in the Neander Valley, just east of Düsseldorf, at the time in the Rhine Province of the Kingdom of Prussia (now in Northrhine-Westphalia, Germany). The valley itself was named for Joachim Neander, Neander being the graecicized form of the surname Neumann ("new man"). The German spelling of Thal "Valley" was current in the 19th century (contemporary German Tal).

Neanderthal 1 was known as the "Neanderthal cranium" or "Neanderthal skull" in anthropological literature, and the individual reconstructed on the basis of the skull was occasionally called "the Neanderthal man". The binomial name Homo neanderthalensis—extending the name "Neanderthal man" from the individual type specimen to the entire group—was first proposed by the Anglo-Irish geologist William King in a paper read to the British Association in 1863, although in the following year he stated that the specimen was not human and rejected the name. King's name had priority over the proposal put forward in 1866 by Ernst Haeckel, Homo stupidus. Popular English usage of "Neanderthal" as shorthand for "Neanderthal man", as in "the Neanderthals" or "a Neanderthal", emerged in the popular literature of the 1920s.

Since the historical spelling -th- in German represents the phoneme /t/ or /tʰ/, not the fricative /θ/, standard British pronunciation of "Neanderthal" is with /t/ (IPA: /niːˈændərtɑːl/). Because of the usual sound represented by digraph ⟨th⟩ in English, "Neanderthal" is also pronounced with the voiceless fricative /θ/, at least in "layman's American English" (as /niːˈændərθɔːl/).

The spelling Neandertal is occasionally seen in English, even in scientific publications. Since "Neanderthal", or "Neandertal", is a common name, there is no authoritative prescription on its spelling, unlike the spelling of the binominal name H. neanderthalensis, which is predicated by King 1864. The common name in German is always invariably Neandertaler (lit. "of the valley of Neander"), not Neandertal, but the spelling of the name of the Neander Valley itself (Neandertal vs. Neanderthal) has been affected by the species name, the names of the Neanderthal Museum and of Neanderthal station persisting with pre-1900 orthography.

Ever since the discovery of the Neanderthal fossils, expert opinion has been divided as to whether Neanderthals should be considered a separate species (Homo neanderthalensis) or a subspecies (Homo sapiens neanderthalensis) relative to modern humans. Pääbo (2014) described such "taxonomic wars" as unresolveable in principle, "since there is no definition of species perfectly describing the case." The question depends on the definition of Homo sapiens as a chronospecies, which has also been in flux throughout the 20th century. Authorities preferring classification of Neanderthals as subspecies have introduced the subspecies name Homo sapiens sapiens for the anatomically modern Cro-Magnon population which lived in Europe at the same time as Neanderthals, while authorities preferring classification as separate species use Homo sapiens as equivalent to "anatomically modern humans".

During the early 20th century, a prevailing view of Neanderthals as "simian", influenced by Arthur Keith and Marcellin Boule, tended to exaggerate the anatomical differences between Neanderthals and Cro Magnon. Beginning in the 1930s, revised reconstructions of Neanderthals increasingly emphasized the similarity rather than differences from modern humans. From the 1940s throughout the 1970s, it was increasingly common to use the subspecies classification of Homo sapiens neanderthalensis vs. Homo sapiens sapiens. The hypothesis of "multiregional origin" of modern man was formulated in the 1980s on such grounds, arguing for the presence of an unbroken succession of fossil sites in both Europe and Asia. Hybridization between Neanderthals and Cro Magnon had been suggested on skeletal and craniological grounds since the early 20th century, and found increasing support in the later 20th century, until Neanderthal admixture was found to be present in modern populations genetics in the 2010s.

Evolution

Stage 1: Early pre-Neanderthal, possibly Homo erectus, (Tautavel Man, 450 ka)
 
Stage 2: Archaic Neanderthal (Miguelón, 430 ka)
 
Stage 3: Intermediate Neanderthal (Saccopastore I, 130 ka)
 
Stage 4: Classic European Neanderthal (La Chapelle-aux-Saints 1, 50 ka)
 
The evolution of Neanderthals according to the accretion model.

Both Neanderthals and anatomically modern humans were initially thought to have evolved from Homo erectus between 300,000 and 200,000 years ago. H. erectus had emerged around 1.8 million years ago, and had long been present, in various subspecies throughout Eurasia.

The divergence time between the Neanderthal and archaic Homo sapiens lineages is estimated to be between 800,000 and 400,000 years ago. The more recent time depth has been suggested by Endicott et al. (2010) and Rieux et al. (2014).

The time of divergence between archaic Homo sapiens and ancestors of Neanderthals and Denisovans caused by a population bottleneck of the latter was dated at 744,000 years ago, combined with repeated early admixture events and Denisovans diverging from Neanderthals 300 generations after their split from Homo sapiens, was calculated by Rogers et al. (2017).

Homo heidelbergensis, dated 600,000 to 300,000 years ago, has long been thought to be a likely candidate for the last common ancestor of the Neanderthal and modern human lineages. However, genetic evidence from the Sima de los Huesos fossils published in 2016 seems to suggest that H. heidelbergensis in its entirety should be included in the Neanderthal lineage, as "pre-Neanderthal" or "early Neanderthal", while the divergence time between the Neanderthal and modern lineages has been pushed back to before the emergence of H. heidelbergensis, to about 600,000 to 800,000 years ago, the approximate age of Homo antecessor.

The taxonomic distinctions between H. heidelbergensis and Neanderthals is mostly due to a fossil gap in Europe between 300,000 and 243,000 years ago (MIS 8). "Neanderthals", by conventions, are fossils which date to after this gap. The quality of the fossil record greatly increases from 130,000 years ago onwards. Specimens younger than this date make up the bulk of known Neanderthal skeletons and were the first whose anatomy was comprehensively studied. In morphological studies, the term "classic Neanderthal" may be used in a narrower sense for Neanderthals younger than 71,000 years old (MIS 4 and 3).

Microbiome

Neanderthals lived along-side humans until their extinction between 40,000-30,000 years ago, and share a common ancestor which could tell us more about how our microbiome evolved. Using dental calculus, calcified bone that traps microorganism, researchers have been able to look into how ancient human microbiomes may have existed. Based on a 16s shotgun sequence of dental calculus found in neanderthal specimens, researchers have found a large portion of neanderthal oral microbiome contains Actinobacteria, Firmicutes, Bacteroidetes, Proteobacteria, much like modern humans; however, neanderthals also had, Euryarchaeota, fungi and some oral pathogens that modern humans lack.

Diet of neanderthals depend on the environment they live in. Neanderthal remains recovered from Spy Cave, Belgium and examined them using dental calculus which indicated neanderthals in this area had meat based diet, including woolly rhinoceros and wild sheep. This is compared to neanderthal remains found in Spain. In El Sidrón Cave, Spain, they examined remains indicating a large amount of plant material such as nuts and moss, as well as mushrooms. Researchers determined that the difference in diets contributed to the neanderthal microbiota, and meat based diet caused the most variation. According to fecal biomarkers, neanderthals were able to convert cholesterol to coprostanol at a high rate, much like modern humans, because of the bacteria present in their gut.

Habitat and range