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Dark earth

From Wikipedia, the free encyclopedia
Archaeological term
This article is about the archaeological horizon. For the video game, seeDark Earth. For other uses, seeBlack earth.

Ingeology andarchaeology,dark earth is asubstratum, up to 1 metre (3 ft 3 in) thick, that indicates settlement over long periods of time. The material is high in organic matter, including charcoal, which gives it its characteristic dark colour; it may also contain fragments of pottery, tile, animal bone and other artefacts. It is interpreted as soil enriched with the sooty remains of thatched roofs from houses without chimneys, with other waste materials. In some areas it appears to give the soil added fertility.

Restored blackhouse in a museum onTrotternish,Skye. There is no chimney on this house and the thatch becomes impregnated with soot. When the roof is replaced, the waste thatch can add fertility to the soil, resulting in dark earth.

London's dark earth was originally called 'black earth' by archaeologists. It was renamed 'dark earth' because of confusion with thechernozem (black earth soils inRussia), whose dark colour is traditionally (not universally)[1][2][3][4] thought to come fromhumus, rather thansoot.

Charred material as agricultural improver

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In theHebrides, it was customary to remove the thatch from the"black houses" every spring, and spread it on the fields as fertilizer, improved by the soot which it retained. OnAchill Island, special smoke huts were built in the fields, stone structures with sod roofs. From October to May smoky fires burned inside them, and in spring the sods were spread on the fields.[5] In the Amazon basin, there are very extensive areas of dark soil, known asterra preta, enriched by small particles of soot, and these areas are much more fertile than the natural soil.

Major areas

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Roman Britain

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InEngland, dark earth covers many areas that were built up in the Roman period, especiallyLondinium. In some cases, it may represent open spaces on the edge of urban centres, but can also be found in more rural settings in and around foci of settlement. In the example of London, deposits underlying the ancient city's dark earth are often dated to between the 2nd to 5th century, the middle and later Roman period. Overlying deposits are frequently dated to the 9th century when Saxon London was repopulated and began to expand. The dark earth shows little evidence of any depositional structure or 'horizons', althoughtip lines are sometimes recorded.

Archaeologists have debated what London's dark earth layer may indicate about human use of the city.[6] It has been taken as evidence of refuse disposal or gardeningduring the Roman period on the site of previous buildings. In this case it might be evidence of a decline ofLondinium's population, or of its partial displacement outside the city walls. However, late Roman cemeteries around London do not show a population decline compared with earlier London.

Alternatively, dark earth might have formed onlyafter abandonment at the end of the Roman period. In this interpretation, dark earth would consist of urban deposits of smoke-impregnated thatch, decayed weeds, timber, and earth floors, reworked and homogenized by worm action,[7] or by agricultural activities, such as ploughing, that mixed building materials from the abandoned Roman cities with material deposited later.

Latest findings in France demonstrated that dark earth may originate from a change from stone to organic building materials; timber and straw will decay and build dark earth. The presence of dark earth does not necessarily imply diminished human activity.[6]

Sweden

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InSweden, dark earth covering 40 hectares (100 acres) has been found inUppåkra, inScania, southern Sweden, where a city-like settlement existed from about the year 1 until 1000 CE when the settlement shifted to modern dayLund. Dark earth over 7 hectares (17 acres) has been found in the Viking city ofBjörkö (today called Birka), in central Sweden, close to modernStockholm. Dark earth has also been found inKöpingsvik, on the island ofÖland close to the southern Sweden east coast.[citation needed]

West Africa

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Dark earths occur around ruins in theUpper Guinean forests ofGhana,Guinea,Liberia andSierra Leone.[8][9] For a period of at least 700 years, West African farmers have enriched the rain forest soils around their towns with compost derived from kitchen, animal, agricultural, and fire waste to produce a signature dark earth.[10] Dark earth is part of the local nomenclature, economically important, and is used judiciously by local communities.[9] TheLoma andMende peoples currently improve soil in this fashion. They well understand how this connects them to the durable legacy of fertile dark earth that encircles the ruined sites in the region.[8] Locals associate the age of their own towns with the depth of their black soil.[9][10]

Amazonian dark earths

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Main article:Terra preta

Amazonian Dark Earths (ADEs) or terra preta do índio (inPortuguese, means "black soil of theIndian") are a type of very dark, fertile artificial (anthropogenic)soil occurring in theAmazon Basin. ADEs owe their characteristic black color to their weatheredcharcoal content.

See also

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Notes

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  1. ^Lehmann, J.; Kleber, M. (2015-12-03), "The contentious nature of soil organic matter",Nature,528 (7580):60–8,Bibcode:2015Natur.528...60L,doi:10.1038/nature16069,PMID 26595271,S2CID 205246638
  2. ^Eckmeier, Eileen; Gerlach, Renate; Gehrt, Ernst; Schmidt, Michael W.I. (2007),"Pedogenesis of Chernozems in Central Europe — A review"(PDF),Geoderma,139 (3–4):288–299,Bibcode:2007Geode.139..288E,doi:10.1016/j.geoderma.2007.01.009, archived fromthe original(PDF) on 2016-03-08, retrieved2016-02-28
  3. ^Schmidt, M.W.I.; Skjemstad, J.O.; Jäger, C. (2002), "Carbon isotope geochemistry and nanomorphology of soil black carbon: Black chernozemic soils in central Europe originate from ancient biomass burning",Global Biogeochemical Cycles,16 (4): 70–1–70–8,Bibcode:2002GBioC..16.1123S,doi:10.1029/2002GB001939,S2CID 56045817,These data challenge the common paradigm that chernozems are zonal soils with climate, parent material and bioturbation dominating soil formation, and introduce fire as a novel, important factor in the formation of these soils
  4. ^Eckmeier, E. (2007),Detecting prehistoric fire-based farming using biogeochemical markers (Dissertation), University of Zurich, Faculty of Science.,doi:10.5167/uzh-3752,It is now an open question as to whether Neolithic settlers did indeed prefer to grow crops where Chernozems occurred or if Neolithic burning formed the chernozemic soils.
  5. ^The book of masonry stoves. David Lyle. Brick House Publishing Co, Inc. Andover, Massachusetts, 1984.ISBN 0-931790-57-3 (paperback edition) p.23
  6. ^abMacphail, Richard I.; Galinié, Henri; Verhaeghe, Frans (June 2003)."A future for Dark Earth?".Antiquity.77 (296):349–358.doi:10.1017/S0003598X00092334.
  7. ^"Charles Darwin and his brilliant book on Earth worms chapter-3".www.webmesh.co.uk.
  8. ^abFrausin, Victoria; Fraser, James Angus; Morrison, Woulay Narmah; Thomas, K. Lahai; Winnebah, R. A.; Fairhead, James; Leach, Melissa (October 2014)."God Made the Soil, but We Made It Fertile: Gender, Knowledge, and Practice in the Formation and Use of African Dark Earths in Liberia and Sierra Leone"(PDF).Human Ecology.42 (5):695–710.doi:10.1007/s10745-014-9686-0.ISSN 0300-7839.S2CID 254541143.
  9. ^abcSolomon, Dawit; Lehmann, Johannes; Fraser, James A; Leach, Melissa; Amanor, Kojo; Frausin, Victoria; Kristiansen, Søren; Millimouno, Dominique; Fairhead, James (2016)."Indigenous African soil enrichment as climate-smart sustainable agriculture alternative"(PDF).Front Ecol Environ.14 (2):71–76.Bibcode:2016FrEE...14...71S.doi:10.1002/fee.1226.S2CID 13946639.
  10. ^ab"How Africans Are Saving Their Own Soil".National Geographic. Archived fromthe original on 2016-06-20.

External links

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World Reference Base for Soil Resources (1998–)
USDA soil
taxonomy
Other systems
Non-systematic soil types
Soil on bodies other than Earth
National
Other
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