Homo sapiens (Hominidae)



Homo sapiens ist eine Primatenart innerhalb der Familie Hominidae, die ab dem Pliozän lebten, das vor rund 5,333 Millionen Jahren begann und bis vor vor 2,588 Millionen Jahren andauerte.

Fundorte

Systematik

Daten zu den einzelnen Funden von Homo sapiens
Sammlung Kommentar zum Fundort Epoche, Alter
Wajak Cave Mammal Fauna From the Wajak (Wadjak) Cave site discovered in 1888 south of Kediri in East Java. The site has since been destroyed by local marble mining industry. Lat/Long Given for the town of Kediri. Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie Lithographie Kommentar z. Taxonomie
The age of the Wajak site is very poorly constrained and given as "post-Pleistocene" and "Mesolithic." "Cave breccia" This was the first attempt to describe the entire mammal fauna of the Wajak Cave. Earlier reports listed on the human remains, and some of the species (e.g. tigers).
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Border cave Border Cave, Ingwavuma District, KwaZulu, South Africa Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Third White Ash
Kommentar z. Stratigraphie
Third White Ash, M.S.A.
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West Turkana - Eliye Springs western shore of Lake Turkana Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
ETE Locality 136, Eliye Springs,
Kommentar z. Stratigraphie Lithographie
ETE dating method: time_unit, ETE age comment: . ETE rock type adj: ., ETE lithology comments: also sand
Sammlung Epoche, Alter Kommentar zur Sammlung
Kalemba Rock-Shelter -
zwischen 0 und 2.59 Millionen Jahren
ETE Locality 673, Kalemba Rock-Shelter,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: >35000 BC on bone apatite; 1835 +- 70 AD on beans from pot radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: granite rock-shelter; layers of soil and stone (granite); deep colluvial deposits near site
U.a. am Fundort ausgegraben: Otolemur crassicaudatus
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Mugharet el 'Aliya in cliffs of Cape Ashakar; in Gres de Rabat; High Cave; Tangier -
zwischen 0 und 2.59 Millionen Jahren
ETE Locality 675, Mugharet el 'Aliya,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: max age based on comparisons with dated sites; 2 C14 dates 625 and 2340 bp on charcoal radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: medium grained sand with pebbles and finer materials; yellow and grey in color
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Kom Ombo GS 3 Gabal Silsila 3; in Nile Valley -
zwischen 0.01 und 2.59 Millionen Jahren
Gabal Silsila ETE Locality 707, Kom Ombo GS 3,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: 6615000-10500 BC; age based on dates for the Gabal Silsila Formation radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: Nile silts and sands
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Kom Ombo Oasis in Nile Valley -
zwischen 0.01 und 2.59 Millionen Jahren
Gabal Silsila ETE Locality 710, Kom Ombo Oasis,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: 6615000-10500 BC; age based on dates for the Gabal Silsila Formation radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: Nile silts and sands
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Makwe Rock Shelter in Katete District, in Little Makwe Kopje; includes domestic animals Holocene
zwischen 0 und 0.01 Millionen Jahren
ETE Locality 713, Makwe Rock Shelter,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: on charcoal; dates range from 750 AD +-80 to 3480 BC +- 140 radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: rocky kopje of qurtzofeldspathic rock
U.a. am Fundort ausgegraben: Galago senegalensis
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Black Earth Cave Cape Province -
zwischen 0.01 und 2.59 Millionen Jahren
ETE Locality 739, Black Earth Cave,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: stratigraphy places site between Powerhouse Cave and Witkrans MSA; MSA deposits radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: red and black streaked clay; black earth; various limestones
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Die Kelders pair of caves on SW coast of South Africa -
zwischen 0 und 2.59 Millionen Jahren
ETE Locality 771, Die Kelders
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: max age at least 40000 years, 40000 year based on fauna, artifacts and sediments, C14 on charcoal radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: limestone cave with quartzite deposits; between Table Mountain Sandstone and Bredasdorp Formation
U.a. am Fundort ausgegraben: Papio ursinus
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Middle Awash - Bodo mbr. Lat/long assigned from Bodo D'Ar. Middle Pleistocene
zwischen 0.01 und 0.78 Millionen Jahren
Wehaietu ETE Locality 998, Middle Awash - Bodo mbr.,
Kommentar z. Stratigraphie Lithographie
ETE dating method: composite, ETE age comment: Fauna is comp to Olduvai above the Lemuta mbr. Min age = 8955 y BP (C14 date from Gewani) radiometric intage_min ETE rock type adj: ., ETE lithology comments: "sands, conglomerates, silts, clays, and tuffs"
U.a. am Fundort ausgegraben: Papio hamadryas
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"KomOmbo-GSIII,Lev3" N of Plain -
zwischen 0.01 und 2.59 Millionen Jahren
Gebel Silsila-YCS ETE Locality 1344, "Gebel Silsila III, Level 3", "Gabal Silsila III, Level 3", "KomOmbo-GSIII,Lev3",
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: From Sebekian Assemblage radiometric intage_max, radiometric intage_min ETE rock type adj: calcitic, ETE lithology comments: sand&silt mixed
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GS Area 2A+2B E of Silsila Station -
zwischen 0 und 2.59 Millionen Jahren
ETE Locality 1378, Gebel Silsila 2A+2B, Gabal Silsila 2A+2B, GS Area 2A+2B,
Kommentar z. Stratigraphie Lithographie
ETE dating method: time_unit, ETE age comment: No radiocarbon determinations radiometric intage_min ETE rock type adj: 0, ETE lithology comments: 0
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Doornfontein 1 in the Postmasburg District of the Northern Cape Holocene
zwischen 0 und 0.01 Millionen Jahren
ETE Locality 715, Doornfontein 1,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: 391120 +- 40; 130 +-80; dates on charcoal radiometric intage_max, radiometric intage_min ETE rock type adj: fine red, ETE lithology comments: ash; fine red sand; rubble; artificial bedrock
U.a. am Fundort ausgegraben: Papio ursinus
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Klasies River Mouth Main Site on Southern coast of CapeProvince; continuous caves 1,1A,1B,1C and 2; 3 km East of Klasies River Mouth -
zwischen 0.01 und 2.59 Millionen Jahren
ETE Locality 735, Klasies River Mouth Main Site,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: MSA deposits; C14 on charcoal radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: brown to greyish brown silty sand
U.a. am Fundort ausgegraben: Papio ursinus
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Klasies River Mouth Cave 1D 97200 m from main Klasies site; on Southern Coast of Cape Province; 3km East of Klasies River Mouth Holocene
zwischen 0 und 0.01 Millionen Jahren
ETE Locality 738, Klasies River Mouth Cave 1D,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: LSA deposits; 2285 +- 105; 4755 +- 95; dates on charcoal radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: brown to greyish brown silty sands
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Scott's Cave on farm Scothurst in the Gamtoos Valley, 10 km North of Patensie Holocene
zwischen 0 und 0.01 Millionen Jahren
ETE Locality 749, Scott's Cave,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: 411190 +- 100; 360 +- 80; dates on charcoal radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: cut into Enon conglomerate
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Tienfontein 4A latitude and longitude determined by map Holocene
zwischen 0 und 0.01 Millionen Jahren
ETE Locality 763, Tienfontein 4A,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: 21150 +- 45 on charcoal radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: 0
Sammlung Kommentar zum Fundort Epoche, Alter Kommentar zur Sammlung
Tienfontein 7 latitude and longitude determined by map Holocene
zwischen 0 und 0.01 Millionen Jahren
ETE Locality 764, Tienfontein 7,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: 1970 +- 4 on charcoal radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: 0
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Boomplas Cave in Cango River Valley -
zwischen 0 und 2.59 Millionen Jahren
ETE Locality 767, Boomplas Cave,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: 2416 C14 dates on charcoal radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: 0
U.a. am Fundort ausgegraben: Papio ursinus
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Byeneskranskop Cave 70160 km East of Cape Town in the Southern Cape province of South Africa -
zwischen 0 und 2.59 Millionen Jahren
ETE Locality 770, Byeneskranskop Cave,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: dates on charcoal radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: 0
U.a. am Fundort ausgegraben: Papio ursinus
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Laetoli - Loc. 2 Ngaloba southern part of Locality 2, lat/long obtained from grid overlain on map -
zwischen 0.01 und 2.59 Millionen Jahren
Vogel River Series ETE Locality 637, Laetoli - Loc. 2 Ngaloba,
Kommentar z. Stratigraphie Lithographie
ETE dating method: composite, ETE age comment: based on stratigraphical position, 120,000 +- 30,000 yrs ETE rock type adj: 0, ETE lithology comments: and sandstone
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Swartkrans - Member 5 Lat/long based on Churcher (1956) map & coordinates of Sterkfontein -
zwischen 0.01 und 2.59 Millionen Jahren
Swartkrans ETE Locality 647, Swartkrans - Member 5,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: dates from Antidorcas bondi bones radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: lightly calcified deposit that partially fills an erosional space surr. a massive stalagmite mass on NW side of cave
U.a. am Fundort ausgegraben: Papio ursinus
Sammlung Epoche, Alter Kommentar zur Sammlung
Sea Harvest Site -
zwischen 0.01 und 2.59 Millionen Jahren
ETE Locality 748, Sea Harvest Site,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: dates also based on stratigraphic and sedimentological obs.; C14 on ostrich eggshell radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: 0
U.a. am Fundort ausgegraben: Papio ursinus
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Equus Cave on Gaap Escarpment at Norlim near Taung in the Northern Cape Province of South Africa -
zwischen 0.01 und 2.59 Millionen Jahren
ETE Locality 775, Equus Cave,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: dates on charcoal radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: limestone formed by evaporation of spring waters;sandy loams with tufa grit
U.a. am Fundort ausgegraben: Papio ursinus
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Heuningneskrans Shelter near Ohringstad in the Eastern Transvaal -
zwischen 0 und 2.59 Millionen Jahren
ETE Locality 776, Heuningneskrans Shelter,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: at least 23000 on charcoal radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: dolomite rock shelter
U.a. am Fundort ausgegraben: Papio ursinus
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Ishango - N.F.P. Shore of L. Rutanzige Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
ETE Locality 887, Niveau fossilifere principal, Ishango - N.F.P.,
Kommentar z. Stratigraphie Lithographie
"The first stage, characterised by the Ishangian levels, is illustrative for a Late Pleistocene hunter-fisher-gatherer Community adapted to relatively dry and open savanna living conditions. For the moment it is impossible to give a more precise estimate of the age of the Ishango culture, but it is not inconceivable that the N.F.PR. assemblage relates to one of somewhat drier phases that occurred within the second half of the Late Pleistocene, i.e. from ca. 21000 to 17500 BP or from 14500 to 12500 BP." ETE dating method: absolute, ETE age comment: "Max age = 21,000 +/- 500 (date in NFP at Is11). Min age = 6890 +/- 75 (charcoal from the Katwe ash)." radiometric intage_max, radiometric intage_min. Niveau fossilifere principal. ETE rock type adj: 0, ETE lithology comments: "dense concentration of bones and artifacts, possibly a debris wash"
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Ishango - Z. Post-Em. Shore of L. Rutanzige Holocene
zwischen 0 und 0.01 Millionen Jahren
ETE Locality 889, Zone post-emersion, Ishango - Z. Post-Em.,
Kommentar z. Stratigraphie Lithographie
"This occupation stage might postdate the early Holocene period" ETE dating method: absolute, ETE age comment: "Max age = 21,000 +/- 500 (NFP at Is11). Min age = 6890 +/- 75 (charcoal in Katwe Ash at Kabale)." radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: "brown horizon, lithology otherwise undescribed"
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Matupi Cave - Unit Matupi II "Mt. Hoyo, 40 km SW of Irumu." -
zwischen 0 und 2.59 Millionen Jahren
ETE Locality 895, Matupi Cave - Unit Matupi II,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: "max=21350 +/- 3500y BP,TL date from 120 cm bel surf;min=2910 +/- 75y BP,C14 date from 30 cm bel surf" radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: buff-brown soil and brown loam
U.a. am Fundort ausgegraben: Papio anubis
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Ishango - Katwe Ash "Includes Is4, Is1." Holocene
zwischen 0 und 0.01 Millionen Jahren
ETE Locality 907, Ishango - Katwe Ash,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: Bulk of Katwe ash was extruded at 6890 +/- 75 y BP (C14 date from near top of the ash). radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: "ash, soft or indurated"
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Ishango - LTC Shore of L. Rutanzige -
zwischen 0 und 2.59 Millionen Jahren
ETE Locality 908, Ishango - LTC,
Kommentar z. Stratigraphie Lithographie
ETE dating method: time_unit, ETE age comment: Latest Pleistocene age based on fauna and stratigraphic position radiometric intage_min ETE rock type adj: 0, ETE lithology comments: fine gravels and sands
Sammlung Epoche, Alter Kommentar zur Sammlung
Katanda 2 - Semliki Beds -
zwischen 0 und 5.33 Millionen Jahren
ETE Locality 921, Kt, Katanda 2 - Semliki Beds,
Kommentar z. Stratigraphie Lithographie
ETE dating method: composite, ETE age comment: "estimated to be E.-M. Pleis, L. Plioc at base,main age = 6890 +/- 75 ( radiocarbon date from Katwe ash)." radiometric intage_min ETE rock type adj: 0, ETE lithology comments: "coarse and gravelly sands, clayey sands, concretions, clay, iron oxide stains"
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Kyanyumu - Katwe Ash NW of Ishango Holocene
zwischen 0 und 0.01 Millionen Jahren
ETE Locality 934, Kyanyumu - Katwe Ash,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: Bulk of Katwe ash was extruded at 6890 +/- 75 y BP (C14 date from near top of the ash). radiometric intage_max, radiometric intage_min ETE rock type adj: 0, ETE lithology comments: "ash, soft or indurated"
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Middle Awash (Bodo/UBSU) On the east side of the Awash River in NW Haaghe province. Middle Pleistocene
zwischen 0.01 und 0.78 Millionen Jahren
Wehaietu ETE Locality 955, Middle Awash - Bodo, UBSU, Upper Bodo Sand Unit,
Kommentar z. Stratigraphie Lithographie
ETE dating method: composite, ETE age comment: Max age = fauna correlates with Olduvai above Lemuta mbr. and Olorgesailie. Min age = 8955 y BP (C14 date from Gewani) radiometric intage_min ETE rock type adj: 0, ETE lithology comments: Layer A:conglomerate, coarse sand. Layer B:medium sand with pebble lenses at top. Layer C: medium-fine sand, silt, clay.
U.a. am Fundort ausgegraben: Theropithecus oswaldi
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Vero Vero, on the Atlantic Coast, Florida. Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Kommentar z. Stratigraphie Lithographie
Stratum 3 of Vero excavation produced most materials (= "muck bed"); Stratum 2 less productive but supposedly not significantly older plants are mostly from layer No. 3 and vertebrates are mostly from layer No. 2 according to Hrdlicka 1917 "The former [human skeleton] lay in dark and somewhat indurated sands, layer No. 2 of Sellards, the latter for the most part at the base of layer No. 3, the muck deposit of the stream bed... layer No. 2 is seen to be overlain by a stratum of similar, but somewhat lighter, sandy deposits covered by a layer of marl [ranging] from about 5 to 9 inches in thickness, and when freshly exposed is of the consistency of fresh mortar, but on exposure hardens to fairly solid rock... The second skeleton lay... in some loose white sand and vegetable matter at the base of the muck layer" (Hrdlicka 1917)
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Shenxian Cave, Huifeng Mountain, Lishui County China, Jiangsu Province, Lishui County, Jingnei, Huifeng Mountain, from Lishui City about 21 km in southeastern direction; Shenxian (Fairies') Cave is located on the Northwest slope of Shenxian Mountain. -
zwischen 0 und 2.59 Millionen Jahren
Kommentar z. Stratigraphie Lithographie
upper part Radiocarbon date of 11200 +/- 1000 or 9250 +/- 1000 BC has been yielded. Red-brown sandy clay, not lithified, no layering, occasionally some calcareous breccia, some quartzicic pebbles and fragments of drop stone. The fossils and fragments of coal are scattered around in this layer (1,5-2,5 m in thickness). At the bottom of this layer there is a hardground of drop stone, about 10 cm thick. At some places there is 20 cm of clay between these two layers. In the drop stone have been found fossils, too.
Sammlung Epoche, Alter
Xiashan Cave, upper part, Luoding Holocene
zwischen 0 und 0.01 Millionen Jahren
Lithographie
grayish dark uppermost cave-deposits
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Djebel Irhoud, Ennouchi collection, 1960s Co-ordinates based on the mountain of Djebel Irhoud. Middle Pleistocene
zwischen 0.13 und 0.78 Millionen Jahren
Jebel Irhoud
Kommentar z. Stratigraphie
Late Middle Pleistocene, Mousterian.
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Maasvlakte, Fauna III down-stream from Rotterdam towards the Hook of Holland Holocene
zwischen 0 und 0.01 Millionen Jahren
Meuse Levels, Beer canal
Sammlung Epoche, Alter Kommentar zur Sammlung
Die Kelders 1 -
zwischen 0.01 und 2.59 Millionen Jahren
ETE Locality 513, Die Kelders 1,
Kommentar z. Stratigraphie Lithographie
ETE dating method: absolute, ETE age comment: 0 radiometric intage_min ETE rock type adj: 0, ETE lithology comments: 0
U.a. am Fundort ausgegraben: Papio ursinus
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Liang Bua Holocene deposits "cave formed in Miocene limestone... Flores... 14 km north of Ruteng and 25 km from the north coast, overlooking the Wae Racang river valley... 30 m wide and 25 m high at the entrance, and up to 40 m deep" Holocene
zwischen 0 und 0.01 Millionen Jahren
Lithographie Kommentar z. Taxonomie
none given, but sediments in Sector VII are silt, clay, and rockfall Pleistocene fauna from unspecified locations throughout the cave includes "fish, frog, snake, tortoise, varanids, birds, rodents and bats... Komodo dragon and another, even larger varanid, as well an endemic, dwarfed species of Stegodon"
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Upper Herto Member near Bouri at least three localities within about a kilometer east and south of Herto Village and about 5 km east of the coordinate, which is shown on a map Middle Pleistocene
zwischen 0.13 und 0.78 Millionen Jahren
Bouri
Kommentar z. Stratigraphie Lithographie Kommentar z. Taxonomie
"bentonite tuff... usually located within 1 m below the the Upper/Lower Herto contact... yields an 40Ar/39Ar age of 260 +/- 16 [1 s.d.] thousand years; "two pumice clasts" from member dated at 163 +/- 3 and 162 +/- 3 kyr, respectively" (anorthoclase), and a third at "226 +/- 2 kyr" (sanidine); "Two obsidian clasts from the same sands" dated at 160 +/- 2 kyr; all of the pumice and obsidian dates are maximum estimates; the overlying WAVT tuff is correlated geochemically with a tuff below the Konso Silver Tuff, which is dated at 154 +/- 7 kyr (sanidine) member consists of "fluvial and lake-margin deposits of coarse beach and yellow sandstone... Abundant archaeological and faunal remains are embedded in a sand unit at the base of the Upper Herto Member... [it is] a [fluviatile] volcaniclastic sandstone and gravel deposit that yielded all of the Herto hominid fossils and all of the Upper Herto Member archaeological assemblages... variable in thickness, yellow-brown to grey, and cross-bedded, bearing abundant rolled pumices up to 15 cm in diameter." may be a subset of Bouri (collection 22166)
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Hofmeyr "a dry channel bed of the Vlekpoort River... near the town of Hofmeyr" Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Kommentar z. Stratigraphie Lithographie Kommentar z. Taxonomie
dated with "a combination of optically stimulated luminescence and uranium-series dating" of matrix found in the skull at 36.2 +/- 3.3 ka "indurated carbonate-sand" "No other bones or archaeological artifacts were reportedly found in the vicinity"
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Nuapua 2, Chuquisaca, Bolivia Between Carandaiti and Capiranda Holocene
zwischen 0 und 0.01 Millionen Jahren
Nuapua
Lithographie
1.5-1.0 m of reworked gray tuff
Sammlung Kommentar zum Fundort Epoche, Alter
Guitarrero Cave-Complex 3 in Callejon de Huaylas, bounded by two mountains, on valley floor Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie
C14
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Guitarrero Cave-Complex 4 in Callejon de Huayles, between two mountains, on valley floor Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie
C14
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Fowlkes Cave (Holocene) "approximately 10 km north of Kent... near the edge of the southern termination of the Apache Mountains," which would place it near Kent Draw (basis of coordinate) from "a rectangle 10 by 20 ft... in the lower chamber" Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie Lithographie
"less than 1 ft deep at the western extremity but more than 16 inches deep at the eastern end" "black surficial silt"
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Associated Material and Supply Company Sandpit "Sec. 23, T26S, R1W" Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Kommentar z. Stratigraphie Lithographie
from "about thirty feet below the surface" pit is in a sand with a "coarse fraction" of "'mud balls' [and] water rolled cobbles" but fossils are apparently from a "clay and silt level"
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Oatville Sandpit "Sec. 11, T28S, R1W" Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Lithographie Kommentar z. Taxonomie
no details given "A bird bone exhibiting butchering marks, but not mineralized like the Pleistocene fauna, was also found"
Sammlung Epoche, Alter
Gobero Sites G1-G3 Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie Lithographie
age is "Phase 2-Early Holocene Occupation (7700-6200 B.C.E.)" based on numerous 14C AMS dates on enamel and bone calcrete is composed of "calcite-cemented aeolian sand" (lithified based on this statement and figures of specimens)
Sammlung Epoche, Alter
Gobero Mid-Holocene Middens 1-4 Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie Lithographie
age is "Phase 3-Mid-Holocene Occupation (5200-2500 B.C.E.)" based on numerous 14C AMS dates on enamel and bone calcrete is composed of "calcite-cemented aeolian sand" (lithified based on this statement and figures of specimens)
Sammlung Epoche, Alter Kommentar zur Sammlung
Eland's Bay Cave Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Elands Bay Cave
Sammlung Kommentar zum Fundort Epoche, Alter Kommentar zur Sammlung
Huanglong Cave "About 50 m in front of the site is the Dashui River, a branch of the Hangjiang River. The entrance... is about 7.8 m above the current river level. Huanglong Cave extends more than 400 m... five regions were mapped, and four... were excavated... All of the human fossils and most of the animal fossils were excavated from Region 1. A few animal fossils were found in Region 2... Region 1 [is] about 50 m2" Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Huanglongdong
Kommentar z. Stratigraphie Lithographie Museum
local section has five layers, and "All the seven hominin teeth, all the stone artifacts and most of the animal fossils are derived from Layer 3" U-series dates from two rhinoceros teeth and stalagmites range from 79.4 +/- 6.3 ka to 103.7 +/- 1.6 ka but there is also an ESR date on a rhino tooth of 34.78 to 44.18 ka "Red silt clay layer... Two thin flowstone layers developed with a break. Below the flowstone layers there are isolated stalagmites which have no direct connection with the flowstone layer" IVPP
U.a. am Fundort ausgegraben: Macaca mulatta
Sammlung Kommentar zum Fundort Epoche, Alter Kommentar zur Sammlung
Isleta Caves "8 miles west of Isleta, Bernalillo County, New Mexico, N1/2sec. 31, T. 8 N., R. 1 E., N.M.P.M" in a "cave chamber measuring some 20 meters in its greatest dimension north to south... Isleta 2, about a quarter mile south of Isleta 1 is a flask-shaped chamber, averaging 25 feet in diameter" Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Isleta 1; Isleta 2
Kommentar z. Stratigraphie Lithographie Museum
faunal composition suggests "that deposition started only a short time before general extinction of Pleistocene mammals" caves are "the result of gases entrapped in a lava or of drainage of liquid lava" LACM
Sammlung Epoche, Alter
Punung Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Kommentar z. Stratigraphie
60-125 ka
U.a. am Fundort ausgegraben: Symphalangus syndactylus
Sammlung Kommentar zum Fundort Epoche, Alter Kommentar zur Sammlung
Buhl Burial "approximately 2.5 km north of the town of Buhl" and shown map as about 1.5 km SSW of Clear Lake (basis of coordinate) Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
10TF1019 Burial Locale
Kommentar z. Stratigraphie Lithographie
the radiocarbon date is considered a minimum based on dating of the immediately underlying gravel deposits the "matrix around and above the skeleton was windblown sand" and the including unit consists of "nonbedded, poorly to moderately sorted, medium to very fine sand, supporting randomly distributed, angular to rounded, granule-pebble-cobble-boulder clasts," with an "eolian portion" of "sand and silt," that was deposited adjacent to a "gravel bar"
Sammlung Kommentar zum Fundort Epoche, Alter Kommentar zur Sammlung
Anzick "near Wilsal" (basis of coordinate) Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Wilsal
Kommentar z. Stratigraphie Kommentar z. Taxonomie
"late Pleistocene" (no 14C dates provided) "The bone foreshafts are made from large mammal bone diaphyses" that were not identified
Sammlung Epoche, Alter
Nelson Bay Cave, Holocene Holocene
zwischen 0 und 0.01 Millionen Jahren
U.a. am Fundort ausgegraben: Papio ursinus
Sammlung Epoche, Alter
Lang Trang Cave Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Lithographie
cave breccia
U.a. am Fundort ausgegraben: Pongo pygmaeus
Sammlung Epoche, Alter
Moomomi Dunes, Holocene Holocene
zwischen 0 und 0.01 Millionen Jahren
Sammlung Epoche, Alter Kommentar zur Sammlung
Elandsfontein -
zwischen 0 und 2.59 Millionen Jahren
ETE Locality 529, Elandsfontein,
Kommentar z. Stratigraphie Lithographie
ETE dating method: time_unit, ETE age comment: 0 radiometric intage_min ETE rock type adj: 0, ETE lithology comments: 0
U.a. am Fundort ausgegraben: Theropithecus oswaldi
Sammlung Epoche, Alter
Blombos Cave Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Kommentar z. Stratigraphie
100 ka - 70 ka
Sammlung Epoche, Alter Kommentar zur Sammlung
Hoedjiespunt 1 Middle Pleistocene
zwischen 0.13 und 0.78 Millionen Jahren
HDP1
Sammlung Epoche, Alter
El Harhoura 2 Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie
Neolithic, ca 7000-6000 ybp
Sammlung Epoche, Alter
Man Bac Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie
approximately 25 km from the coast
Sammlung Epoche, Alter
Durham Cave #2 -
zwischen 0.01 und 2.59 Millionen Jahren
Sammlung Kommentar zum Fundort Epoche, Alter Kommentar zur Sammlung
Ely Cave cave consists of "a few hundred feet of narrow and rather damp chambers" Holocene
zwischen 0 und 0.01 Millionen Jahren
Gilley?
Sammlung Epoche, Alter
Diepkloof Rock Shelter -
zwischen 0.01 und 2.59 Millionen Jahren
U.a. am Fundort ausgegraben: Papio ursinus
Sammlung Kommentar zum Fundort Epoche, Alter
Melbourne No. 2 Bed "on property owned by" Singleton "at Melbourne" (basis of coordinate) Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Kommentar z. Stratigraphie Lithographie Museum Kommentar z. Taxonomie
"probably early-Pleistocene" according to Allen, but Wisconsinan according to later workers "stream deposits... [comprise] an upper, somewhat barren layer (No. 3 bed) lying uncomforably upon an older deposit rather in rich in fossil bones (the 'bone bed', No. 2). Below these is a layer of coquina (No. 1 bed) believed to be of Pleistocene age." MCZ a long English-language list is given by Allen, who also mentions that "elephant and mastodon still persisted" in the No. 3 bed
Sammlung Epoche, Alter Kommentar zur Sammlung
Devil's Den Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
UF LV002
Museum
FLMNH
Sammlung Kommentar zum Fundort Epoche, Alter
Potter Creek Cave Section 23, T. 34 N., R. 4 W., O'Brien 7.5' Quadrange. North of Potter Creek Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Kommentar z. Stratigraphie Museum
radiocarbon dates from R. S. Feranec (2009) UCMP
Sammlung Epoche, Alter
Morse Creek Number 1 Holocene
zwischen 0 und 0.01 Millionen Jahren
Sammlung Kommentar zum Fundort Epoche, Alter
Cotuit Port Barnstable Holocene
zwischen 0 und 0.01 Millionen Jahren
Sammlung Epoche, Alter
Coningham Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Sammlung Epoche, Alter
Clare Bay Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Sammlung Kommentar zum Fundort Epoche, Alter
Cueva del Muerto A previously unreported fossil site; a cave with a vertical entrance and a depth of 4 m, containing three chambers excavated in January 2013. The smallest chamber, with an area of 2.72 m2, yielded giant tortoise material at a depth of 37 cm. Late Pleistocene
zwischen 0 und 0.13 Millionen Jahren
Sammlung Kommentar zum Fundort Epoche, Alter
Cueva de las Caritas A previously unreported fossil site; a large cave with a vertical entrance with easy access, a depth of 3 m and an area of 104 m2, and which contains two pre-Columbian petroglyphs of human faces. Late Pleistocene
zwischen 0 und 0.13 Millionen Jahren
Sammlung Kommentar zum Fundort Epoche, Alter
Saqqaq Site Disco Bay, West Greenland Holocene
zwischen 0 und 0.01 Millionen Jahren
Sammlung Epoche, Alter
Oosterschelde, Pleistocene Calabrian
zwischen 0.78 und 2.59 Millionen Jahren
Sammlung Kommentar zum Fundort Epoche, Alter
AIT10, Ureia site, Aitutaki The Ureia site is a stratified sequence of calcareous sands just above sea level. It is about 100m inland from the modern beach and is backed by a hill composed of volcanic bedrock and associated eroded soils. In 1987, M. S. Allen, S. E. Schubel, and I excavated 11 m2 of sediment at Ureia to a depth of up to 2 m. Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie
Charcoal-based radiocarbon chronology of Ureia ranges from 200 ± 50 yr B.P. (layer III) to 1040 ± 80 yr B.P. (layer VII). Attempts to date the very small amounts of charcoal from strata below layer VII have not been successful.
Sammlung Kommentar zum Fundort Epoche, Alter Kommentar zur Sammlung
Railhunter Rockshelter, Layer IIB, Tinian Carolinas area, Tinian. Small shelter formed in an isolated block of limestone. Includes test pits 4-6 combined. Holocene
zwischen 0 und 0.01 Millionen Jahren
Site 131
Sammlung Kommentar zum Fundort Epoche, Alter Kommentar zur Sammlung
Railhunter Rockshelter, Layer IIC, Tinian Carolinas area, Tinian. Small shelter formed in an isolated block of limestone. Includes test pits 4-6 combined. Holocene
zwischen 0 und 0.01 Millionen Jahren
Site 131
Sammlung Kommentar zum Fundort Epoche, Alter
Pisonia rockshelter, layer III, Aguiguan A deeply stratified human habitation site formed beneath an undercut limestone wall along a trail to the rugged north coast. The site lies about 250 m inland from the north-central coast, in the vicinity of Butler’s site number 7. Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie
Layers II-IV are pottery-rich, prehistoric cultural deposits spanning more than a millennium
Sammlung Kommentar zum Fundort Epoche, Alter
Pisonia rockshelter, layer IV, Aguiguan A deeply stratified human habitation site formed beneath an undercut limestone wall along a trail to the rugged north coast. The site lies about 250 m inland from the north-central coast, in the vicinity of Butler’s site number 7. Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie
Layers II-IV are pottery-rich, prehistoric cultural deposits spanning more than a millennium
Sammlung Kommentar zum Fundort Epoche, Alter
Pisonia rockshelter, layer IV-V, Aguiguan A deeply stratified human habitation site formed beneath an undercut limestone wall along a trail to the rugged north coast. The site lies about 250 m inland from the north-central coast, in the vicinity of Butler’s site number 7. Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie
A loose area of the excavation wall that had to be salvaged in such a way that Layers IV and V could not be distinguished. Layers II-IV are pottery-rich, prehistoric cultural deposits spanning more than a millennium. Layer V may be partly pre-human in age, based on a sharp decline in pottery content, lack of charcoal, and scarcity of burned bones.
Sammlung Kommentar zum Fundort Epoche, Alter
Pisonia rockshelter, layer V, Aguiguan A deeply stratified human habitation site formed beneath an undercut limestone wall along a trail to the rugged north coast. The site lies about 250 m inland from the north-central coast, in the vicinity of Butler’s site number 7. Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie
Layer V may be partly pre-human in age, based on a sharp decline in pottery content, lack of charcoal, and scarcity of burned bones.
Sammlung Epoche, Alter
Site 1, Utrok Island Holocene
zwischen 0 und 0.01 Millionen Jahren
Sammlung Kommentar zum Fundort Epoche, Alter Kommentar zur Sammlung
Jebel Irhoud Co-ordinates based on the mountain of Djebel Irhoud. Middle Pleistocene
zwischen 0.13 und 0.78 Millionen Jahren
Jebel Irhoud
Sammlung Epoche, Alter
Malakunanja II -
zwischen 0.01 und 2.59 Millionen Jahren
Sammlung Kommentar zum Fundort Epoche, Alter
Apidima Cave C The Apidima complex of six maritime caves is located in Mesa Mani (Lakonia), on a steep coast of the western Mani peninsula, which is the southernmost continental point of the Balkan peninsula, very near to the active Hellenic subduction zone. Middle Pleistocene
zwischen 0.01 und 0.78 Millionen Jahren
Kommentar z. Stratigraphie Kommentar z. Taxonomie
The Apidima caves are karstic formations within the MIddle Triassic-Late Eocene limestone (Plattenhalk) of depth 500m, from 4m to 23m above sea level. Dated using ESR on travertine calcite and fossils - two samples with dates of 250-450,000BP and 200-300,000BP. "As the Apidima fauna is stratigraphically mixed, careful interpretation is required" rodents, birds (mostly beaks), leporids and turtles are also mentioned.
Sammlung Epoche, Alter
Cho-chen Holocene
zwischen 0 und 0.01 Millionen Jahren
Sammlung Epoche, Alter
Cho-chen -
zwischen 0 und 2.59 Millionen Jahren
Sammlung Kommentar zum Fundort Epoche, Alter Kommentar zur Sammlung
El Pit cenote El Pit cenote is part of the private diving and snorkel park Dos Ojos, which is located 15 km north of Tulum in the Mexican federal state of Quintana Roo. El Pit cenote forms part of the Dos Ojos subsystem and the latter is part of the Sac Actun system of underwater caves Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Dos Ojos; 15 km north of Tulum
Sammlung Epoche, Alter
Paisley Caves Late Pleistocene
zwischen 0.01 und 0.13 Millionen Jahren
Sammlung Epoche, Alter
Roebuck Site Holocene
zwischen 0 und 0.01 Millionen Jahren
Sammlung Epoche, Alter
Gruta das Fadas -
zwischen 0.01 und 2.59 Millionen Jahren
Sammlung Epoche, Alter
Río Luján 1 Holocene
zwischen 0 und 0.01 Millionen Jahren
Kommentar z. Stratigraphie
Carbon dating of the D. avus specimen suggests an age of 724 ± 52 14C year BP, in good agreement with the estimated age of human burials at 600 cal years BP (Prevosti et al. 2015)

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