Ahrensburg culture

Last updated
Ahrensburg culture
Kultura ahrensburska.jpg
Geographical range Europe
Period Mesolithic Europe
Datesc. 12,900–11,700 BP
Type site Ahrensburg
Preceded by Magdalenian
Followed by Maglemosian culture; Swiderian culture

The Ahrensburg culture or Ahrensburgian (c. 12,900 to 11,700 BP [1] ) was a late Upper Paleolithic nomadic hunter culture (or technocomplex) in north-central Europe during the Younger Dryas, the last spell of cold at the end of the Weichsel glaciation resulting in deforestation and the formation of a tundra with bushy arctic white birch and rowan. The most important prey was the wild reindeer. The earliest definite finds of arrow and bow date to this culture, though these weapons might have been invented earlier. The Ahrensburgian was preceded by the Hamburg and Federmesser cultures and superseded by the Maglemosian and Swiderian cultures. Ahrensburgian finds were made in southern and western Scandinavia, the North German plain and western Poland. The Ahrensburgian area also included vast stretches of land now at the bottom of the North and Baltic Sea, since during the Younger Dryas the coastline took a much more northern course than today.

Contents

The culture is named after a tunnel valley near the village of Ahrensburg, 25 km (16 mi) northeast of Hamburg in the German state of Schleswig-Holstein, where Ahrensburg find layers were excavated in Meiendorf, Stellmoor and Borneck. While these as well as the majority of other find sites date to the Young Dryas, the Ahrensburgian find layer in Alt Duvenstedt has been dated to the very late Allerød, thus possibly representing an early stage of Ahrensburgian which might have corresponded to the Bromme culture in the north. Artefacts with tanged points are found associated with both the Bromme and the Ahrensburg cultures.

Origin

An Ahrensburg arrowhead Ahrensburg point.png
An Ahrensburg arrowhead

The Ahrensburg culture belongs to a Late Paleolithic and early Mesolithic (or Epipaleolithic) cultural complex that started with the glacial recession and the subsequent disintegration of Late Palaeolithic cultures between 15,000 and 10,000 BCE. The extinction of mammoth and other megafauna provided for an incentive to exploit other forms of subsistence that included maritime resources. Northward migrations coincided with the warm Bølling and Allerød events, but much of northern Eurasia remained inhabited during the Younger Dryas. During the holocene climatic optimum, the increased biomass led to a marked intensification in foraging by all groups, the development of inter-group contacts, and ultimately, the initiation of agriculture. [2]

The different technolithic complexes are chronologically associated with the climatic chronozones. The re-colonisation of Northern Germany is connected to the onset of the late Glacial Interstadial between Weichsel and the Dryas I glaciation, at the beginning of the Meiendorf Interstadial around 12,700 BCE. Palynological results demonstrate a close connection between the prominent temperature rise at the beginning of the Interstadial and the expansion of the hunter-gatherers into the northern Lowlands. The existence of a primary “pioneer phase” in the re-colonisation is contradicted by proof of e.g. an early Central European Magdalenian in Poland. Today it is commonly accepted that the Hamburgian, featured by "Shouldered Point" lithics, is a techno-complex closely related to the Creswellian and rooted in the Magdalenian [ citation needed ]. Within the Hamburgian techno-complex, a younger dating is found for the Havelte phase, sometimes interpreted as a northwestern phenomenon, perhaps oriented towards the former coastline. The Hamburgian culture existed during the warm Bølling period, the brief Dryas II glaciation (lasting 300 years) and in the early warmer Allerød period.

However, the distribution of the Hamburgian east of the Oder River has been confirmed and Hamburgian culture can also be distinguished in Lithuania. Finds in Jutland indicates the expansion of early Hamburgian hunters and gatherers reached further north than previously expected. The Hamburgian sites with shouldered point lithics reach as far north as the Pomeranian ice margin. The younger Havelte phase has been proven for the area beyond the Pomeranian ice margin and on the Danish Isles after c. 12,300 BCE.

The "Backed Point" lithics of Federmesser culture are usually dated in the Allerød Interstadial. Early Federmesser finds follows shortly or are contemporary to Havelte. The culture lasted approximately 1200 years from 11,900 to 10,700 BCE., and is located in Northern Germany and Poland to south Lithuania. Fish-hooks were discovered in Allerød layers and emphasize the importance of fishing in the Late Palaeolithic. A certain survival of late Upper Palaeolithic traditions similar to contemporary Azilian (France, Spain) becomes apparent, such as the amber elk from Weitsche that can be considered as a link to the Mesolithic, amber animal sculptures.

Bromme culture sites are found in the entire southern and southeastern Baltic, and are dated to the second half of Allerød and the early cold Dryas III period. The "classical" Brommian complex is typified by simple and fast, but uneconomical, flint processing using unipolar (single-platform) cores. A new development noticed in Lithuania introduced both massive and smaller "tanged Points". In Bromme culture this technology is proposed to be an innovation derived from tanged Havelte groups. As such, derivation of Bromme culture and even migration of its representatives from the territories of Denmark and northern Germany have been proposed, [3] although other sources hold early Bromme not to be very well defined in (late Allerød) Northern Germany, [4] where it groups with Federmesser.

Ahrensburg culture is normally associated with the Younger Dryas glacialization and the Pre-boreal period. The traditional view of the Ahrensburg culture being a direct inheritor of the Bromme culture in the late Dryas period is contradicted by new information that the Ahrensburgian techno-complex probably already started before the Younger Dryas, [4] strengthening proposals to a direct derivation from the Havelte stage of the Hamburg culture. [5] Some recent finds, such as the Hintersee 24 site in southern Landkreis Vorpommern-Greifswald, would contribute to the argument of an early Ahrensburgian in northern Germany. Alternatively, flint artefacts of Bromme tanged-point groups is considered to prelude the techno-complex of the Ahrensburg culture and would point to the provenience of Ahrensburg from Bromme culture. As such, the Grensk culture in Bromme territory at the source of the Dnieper River was proposed to be the direct originator of Ahrensburgian culture. [6] However, the exact typological chronology of this culture is still unclear. Though associated with the Bromme complex, Grensk culture has its roots more defined in the local Mammoth Hunters' culture.

Another possibility derives from the observation that on a regional scale, the Hamburgian culture is succeeded geographically as well as chronologically by the Federmesser culture, or Arch-Backed Piece Complex. The existence of a genuine Federmesser occupation in southern Scandinavia is highly controversial, and there is wide, though not unanimous, agreement that some Federmesser types constitute an integral part of the early Brommean artefact inventory. Still, Federmesser types are also often found in close association with Hamburgian assemblages (e.g. at Slotseng and Sølbjerg) and tentative, dating from northern Germany shows some degree of contemporaneity between the late Hamburgian Havelte sites and the Federmesser ones. Therefore, in southern Scandinavia the Federmesser may represent a brief transitory phase between the Hamburgian and the Brommean. [7] This corresponds with the notion that "tanged point cultures" such as "Brommian" or "Bromme-Lyngby" appear to be based on the Magdalenian, during the Allerød and were closely associated with reindeer hunting. [8]

Stellmoor

Stellmoor was a seasonal settlement inhabited primarily during October, and bones from 650 reindeer have been found there. The hunting tool was bow and arrow. From Stellmoor there are also well-preserved arrow shafts of pine intended for the culture's characteristic skaftunge arrowheads of flint. A number of intact reindeer skeletons, with arrowheads in the chest, has been found, and they were probably sacrifices to higher powers. At the settlements, archaeologists have found circles of stone, which probably were the foundations of hide teepees.

Scandinavia, Hensbacka group

The earliest reliable traces of habitation in the northern territories of Norway and western Sweden date to the transition period from the Younger Dryas to the Preboreal. More favourable living conditions, and past experience gained through seasonal rounds, prompted increased maritime resource exploitation in the northern territories. The Hensbacka group on the west coast of Sweden exemplifies the cultural fragmentation process that took place within the Continental Ahrensburgian. [9] [10] [11] Instead of new immigrations at the beginning of the Mesolithic, the discovery of deposited bones and new dating indicate that there was no (significant) break in settlement continuity. New knowledge provides aspects for a further autochthonous development, with a rapid climatic change stimulating a swift cultural change. [4]

See also

Related Research Articles

<span class="mw-page-title-main">Epipalaeolithic</span> Period in Levantine history

In archaeology, the Epipalaeolithic or Epipaleolithic is a period occurring between the Upper Paleolithic and Neolithic during the Stone Age. Mesolithic also falls between these two periods, and the two are sometimes confused or used as synonyms. More often, they are distinct, referring to approximately the same period of time in different geographic areas. Epipaleolithic always includes this period in the Levant and, often, the rest of the Near East. It sometimes includes parts of Southeast Europe, where Mesolithic is much more commonly used. Mesolithic very rarely includes the Levant or the Near East; in Europe, Epipalaeolithic is used, though not very often, to refer to the early Mesolithic.

<span class="mw-page-title-main">Creswell Crags</span> Gorge with caves in East Midlands, England

Creswell Crags is an enclosed limestone gorge on the border between Derbyshire and Nottinghamshire, England, near the villages of Creswell and Whitwell. The cliffs in the ravine contain several caves that were occupied during the last ice age, between around 43,000 and 10,000 years ago. Its caves contain the northernmost cave art in Europe. The evidence of occupation found in the rich series of sediments that accumulated over many thousands of years is regarded as internationally unique in demonstrating how prehistoric people managed to live at the extreme northernmost limits of their territory during the Late Pleistocene period.

<span class="mw-page-title-main">Magdalenian</span> Prehistoric archaeological culture in Europe

The Magdalenian cultures are later cultures of the Upper Paleolithic and Mesolithic in western Europe. They date from around 17,000 to 12,000 years ago. It is named after the type site of La Madeleine, a rock shelter located in the Vézère valley, commune of Tursac, in France's Dordogne department.

<span class="mw-page-title-main">Azilian</span> Mesolithic industry of the Franco-Cantabrian region

The Azilian is a Mesolithic industry of the Franco-Cantabrian region of northern Spain and Southern France. It dates approximately 10,000–12,500 years ago. Diagnostic artifacts from the culture include projectile points, crude flat bone harpoons and pebbles with abstract decoration. The latter were first found in the River Arize at the type-site for the culture, the Grotte du Mas d'Azil at Le Mas-d'Azil in the French Pyrenees. These are the main type of Azilian art, showing a great reduction in scale and complexity from the Magdalenian Art of the Upper Palaeolithic.

The Allerød oscillation was a warm and moist global interstadial that occurred c.13,900 to 12,900 BP. It was preceded by the Older Dryas and followed by the Younger Dryas cold periods. The Allerød was nearly at the end of the Last Glacial Period. It raised temperatures in the northern Atlantic region to almost present-day levels, before they declined again in the Younger Dryas, which was followed by the present warm Holocene.

<span class="mw-page-title-main">Upper Paleolithic</span> Subdivision of the Paleolithic or Old Stone Age

The Upper Paleolithic is the third and last subdivision of the Paleolithic or Old Stone Age. Very broadly, it dates to between 50,000 and 12,000 years ago, according to some theories coinciding with the appearance of behavioral modernity in early modern humans, until the advent of the Neolithic Revolution and agriculture.

Federmesser group is an archaeological umbrella term including the late Upper Paleolithic to Mesolithic cultures of the Northern European Plain, dating to between 14,000 and 12,800 years ago. It is closely related to the Tjongerian culture, as both have been suggested. It includes the Tjongerian sites at Lochtenrek in the Frisian part of the Netherland, spanning the area of Belgium, the Netherlands, northern France, northern Germany, southern Denmark, and Poland. It is also closely related to the Creswellian culture to the west and the Azilian to the south. The name is derived from the characteristic small backed flint blades, in German termed Federmesser. It is succeeded by the Ahrensburg culture after 12,800 BP.

The Bølling oscillation, also Bølling interstadial, was a cool temperate climatic interstadial between the glacial Oldest Dryas and Older Dryas stadials, between 14,700 and 14,100 BP, near to the end of the last glacial period. It is named after a peat sequence discovered at Bølling lake in central Jutland, Denmark. It is used to describe a period of time in relation to Pollen zone Ib—in regions where the Older Dryas is not detected in climatological evidence, the Bølling–Allerød is considered a single interstadial period.

<span class="mw-page-title-main">Bromme culture</span>

The Bromme culture is a late Upper Paleolithic culture dated to c. 11,600 to 9,800 cal BC, which corresponds to the second half of the Allerød Oscillation.

<span class="mw-page-title-main">Hamburg culture</span> Archaeological culture

The Hamburg culture or Hamburgian was a Late Upper Paleolithic culture of reindeer hunters in northwestern Europe during the last part of the Weichsel Glaciation beginning during the Bölling interstadial. Sites are found close to the ice caps of the time. They extend as far north as the Pomeranian ice margin.

<span class="mw-page-title-main">Late Pleistocene</span> Third division (unofficial) of the Pleistocene Epoch

The late Pleistocene is an unofficial age in the international geologic timescale in chronostratigraphy, also known as upper Pleistocene from a stratigraphic perspective. It is intended to be the fourth division of the Pleistocene Epoch within the ongoing Quaternary Period. It is currently defined as the time between c. 129,000 and c. 11,700 years ago. The late Pleistocene equates to the proposed Tarantian Age of the geologic time scale, preceded by the officially ratified Chibanian and succeeded by the officially ratified Greenlandian. The estimated beginning of the Tarantian is the start of the Eemian interglacial period. It is held to end with the termination of the Younger Dryas, some 11,700 years ago when the Holocene Epoch began.

The Older Dryas was a stadial (cold) period between the Bølling and Allerød interstadials, about 14,000 years Before Present, towards the end of the Pleistocene. Its date is not well defined, with estimates varying by 400 years, but its duration is agreed to have been around 200 years.

The Bølling–Allerød interstadial, also called the Late Glacial Interstadial, was an abrupt warm and moist interstadial period that occurred during the final stages of the Last Glacial Period. This warm period ran from 14,690 to 12,890 years before the present (BP). It began with the end of the cold period known as the Oldest Dryas, and ended abruptly with the onset of the Younger Dryas, a cold period that reduced temperatures back to near-glacial levels within a decade.

<span class="mw-page-title-main">Prehistory of France</span> Paleolithic to Iron Age prehistory of France

Prehistoric France is the period in the human occupation of the geographical area covered by present-day France which extended through prehistory and ended in the Iron Age with the Roman conquest, when the territory enters the domain of written history.

The Late Glacial Interstadial (LGI) c. 14,670 to c. 12,890 BP, also called the Bølling–Allerød interstadial, represents the first pronounced warming since the end of the Last Glacial Maximum (LGM). Human populations, which had previously been forced into refuge areas, gradually begin to repopulate the Northern Hemisphere's Eurasian landmass.

<span class="mw-page-title-main">Prehistoric Sweden</span> Time period in present-day Sweden before recorded history

Human habitation of present-day Sweden began c. 12000 BC. The earliest known people belonged to the Bromme culture of the Late Palaeolithic, spreading from the south at the close of the Last Glacial Period. Neolithic farming culture became established in the southern regions around 4000 BC, but much later further north. About 1700 BC the Nordic Bronze Age began in the southern regions, based on imported metals; this was succeeded about 500 BC by the Iron Age, for which local ore deposits were exploited. Cemeteries are known mainly from 200 BC onward.

<span class="mw-page-title-main">Swiderian culture</span> Mesolithic culture in what is now Poland

The Swiderian culture is an Upper Palaeolithic/Mesolithic cultural complex, centred on the area of modern Poland. The type-site is Świdry Wielkie, in Otwock near the Swider River, a tributary to the Vistula River, in Masovia. The Swiderian is recognized as a distinctive culture that developed on the sand dunes left behind by the retreating glaciers. Rimantienė (1996) considered the relationship between Swiderian and Solutrean "outstanding, though also indirect", in contrast with the Bromme-Ahrensburg complex, for which she introduced the term "Baltic Magdalenian" for generalizing all other North European Late Paleolithic culture groups that have a common origin in Aurignacian.

<span class="mw-page-title-main">Early history of Pomerania</span>

After the glaciers of the Ice Age in the Early Stone Age withdrew from the area, which since about 1000 AD is called Pomerania, in what are now northern Germany and Poland, they left a tundra. First humans appeared, hunting reindeer in the summer. A climate change in 8000 BC allowed hunters and foragers of the Ertebølle-Ellerbek culture to continuously inhabit the area. These people became influenced by farmers of the Linear Pottery culture who settled in southern Pomerania. The hunters of the Ertebølle-Ellerbek culture became farmers of the Funnelbeaker culture in 3000 BC. The Havelland culture dominated in the Uckermark from 2500 to 2000 BC. In 2400 BC, the Corded Ware culture reached Pomerania and introduced the domestic horse. Both Linear Pottery and Corded Ware culture have been associated with Indo-Europeans. Except for Western Pomerania, the Funnelbeaker culture was replaced by the Globular Amphora culture a thousand years later.

The archaeological site Niederbieber is an important representative of the Federmesser culture. Dating to the end of the Pleistocene, the site is one of the most extensively excavated archaeological sites dating to the late Upper Palaeolithic. Finds and features are extraordinarily well preserved as the site was protected by fallout from the Laacher See volcanic eruption approximately 12,900 years ago. Comprehensive archaeological studies have provided a detailed view of activities and settlement dynamics of hunter-gatherer groups at the end of the ice age.

Bad Breisig is an archaeological site in Germany.

References

  1. Ashton, Nick (2017). Early Humans. London: William Collins. p. 313. ISBN   978-0-00-815035-8.
  2. Dolukhanov, P. M. (1997), "The Pleistocene-Holocene transition in northern Eurasia: Environmental changes and human adaptations", Quaternary International, 41–42: 181–191, Bibcode:1997QuInt..41..181D, doi:10.1016/S1040-6182(96)00051-1
  3. Egidijus Šatavičius, The Final Palaeolithic Cultures in Lithuania Archaeologia Lituana vol. 6 (2005)
  4. 1 2 3 Thomas Terberger, From the First Humans to the Mesolithic Hunters in the Northern German Lowlands, Current Results and Trends, in: Across the western Baltic, edited by: Keld Møller Hansen & Kristoffer Buck Pedersen, Sydsjællands Museums Publikationer Vol. 1 (2006), ISBN   87-983097-5-7
  5. Egidijus Šatavičius, Brommian (Lyngby) Finds in Lithuania (2006) Archived 2008-04-16 at the Wayback Machine
  6. Otte M. The northwestern European plain around 18,000 BP. in Soffer O, Gamble C (eds) The world at 18,000 BP London: Unwin Hyman, 1990, Vol 1, pp. 54–68.
  7. Eriksen, B.V. Reconsidering the geochronological framework of Lateglacial hunter-gatherer colonization of southern Scandinavia. In: B.V. Eriksen & B. Bratlund (eds.): Recent studies in the Final Palaeolithic of the European plain. Proceedings of a U.I.S.P.P. Symposium. Stockholm, 14–17. October 1999. Jutland Archaeological Society Publications Vol. 39. Højbjerg, pp. 25–41.
  8. Kozlowski, J.; Bandit, H. (1984). "The Paleohistory of Circumpolar Arctic Colonization". Arctic. 37 (4): 358–372. doi: 10.14430/arctic2220 .
  9. Schmitt, L.; et al. (2009), "Chronological insights, cultural change, and resource exploitation on the west coast of Sweden during the Late Palaeolithic/early Mesolithic transition", Oxford Journal of Archaeology, 28 (1): 1–27, doi:10.1111/j.1468-0092.2008.00317.x
  10. Schmitt, L.; et al. (2006), "'Why they came'; the colonization of the coast of western Sweden and its environmental context at the end of the last glaciation", Oxford Journal of Archaeology, 25 (1): 1–28, doi:10.1111/j.1468-0092.2006.00246.x
  11. Schmitt, L. (1999), "Comparative points and relative thoughts: the relationship between the Ahrensburgian and Hensbacka assemblages", Oxford Journal of Archaeology, 13 (4): 327–337, doi:10.1111/1468-0092.00087