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    Rights statement: This is the author’s version of a work that was accepted for publication in Anthroprocene. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Anthroprocene, 35, 2021 DOI: 10.1016/j.ancene.2021.100302

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Early historical forest clearance caused major degradation of water quality at Lake Væng, Denmark

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Early historical forest clearance caused major degradation of water quality at Lake Væng, Denmark. / Bennike, O.; Odgaard, B.V.; Moorhouse, H. et al.
In: Anthropocene, Vol. 35, 100302, 30.09.2021.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Bennike, O, Odgaard, BV, Moorhouse, H, McGowan, S, Siggaard-Andersen, M-L, Turner, B, Schomacker, A, Jessen, S, Kazmierczak, J, Olsen, J, Rasmussen, P, Kidmose, J, Nisbeth, CS, Thorling, L & Weckström, K 2021, 'Early historical forest clearance caused major degradation of water quality at Lake Væng, Denmark', Anthropocene, vol. 35, 100302. https://doi.org/10.1016/j.ancene.2021.100302

APA

Bennike, O., Odgaard, B. V., Moorhouse, H., McGowan, S., Siggaard-Andersen, M.-L., Turner, B., Schomacker, A., Jessen, S., Kazmierczak, J., Olsen, J., Rasmussen, P., Kidmose, J., Nisbeth, C. S., Thorling, L., & Weckström, K. (2021). Early historical forest clearance caused major degradation of water quality at Lake Væng, Denmark. Anthropocene, 35, Article 100302. https://doi.org/10.1016/j.ancene.2021.100302

Vancouver

Bennike O, Odgaard BV, Moorhouse H, McGowan S, Siggaard-Andersen ML, Turner B et al. Early historical forest clearance caused major degradation of water quality at Lake Væng, Denmark. Anthropocene. 2021 Sept 30;35:100302. Epub 2021 Jul 16. doi: 10.1016/j.ancene.2021.100302

Author

Bibtex

@article{e620ba30171c44dcb4f4cc683d4abe73,
title = "Early historical forest clearance caused major degradation of water quality at Lake V{\ae}ng, Denmark",
abstract = "Although humans have impacted their environment over millennia, details of these impacts, especially on aquatic systems, is still surprisingly scarce despite potential disturbance by early land use. This study examined a high-resolution radiocarbon-dated Holocene record from the Danish Lake V{\ae}ng, using geochemical and biological proxies, and related the observed impacts to other lake records with catchment disturbance. The results indicate a lengthy and varying history of aquatic eutrophication linked to human activity. Modest impacts on the lake coincided with the first signs of landscape disturbance during the Neolithic (c. 4500 cal. yrs BP). Observed impacts intensified in the Late Bronze and Pre-Roman Iron Age. Viking Age/Medieval deforestation and erosional inputs to the lake associated with new ploughing technology (1200 cal. yrs BP), however, led to a major reorganisation of the aquatic ecosystem. Filamentous bloom-forming cyanobacteria, common today in heavily culturally impacted lakes, reached a historical maxima. The lake ecosystem subsequently recovered somewhat but remains eutrophic to date. The erosion record from Lake V{\ae}ng shows a striking similarity with other Danish lake records, especially the notable increase in Medieval Period catchment inputs, which are observed in other European lacustrine records. Numerous European lowland lakes may have shifted into a degraded ecological state millennia ago, but degradation intensified during the onset of the Medieval Period. Hence, assuming pre-industrial conditions as relatively pristine reference baselines for more recent cultural eutrophication could be flawed in landscapes intensively used by humans for millennia. ",
keywords = "Catchment-lake processes, Holocene, Inorganic phosphorus, Macrofossils, Pigments, Soil erosion, algal bloom, aquatic ecosystem, Bronze Age, catchment, cyanobacterium, deforestation, disturbance, environmental degradation, eutrophication, forest clearance, historical record, human activity, Iron Age, lake ecosystem, land use change, Medieval, Neolithic, radiocarbon dating, water quality, Denmark, Lake Vaeng, Midtjylland, Cyanobacteria",
author = "O. Bennike and B.V. Odgaard and H. Moorhouse and S. McGowan and M.-L. Siggaard-Andersen and B. Turner and A. Schomacker and S. Jessen and J. Kazmierczak and J. Olsen and P. Rasmussen and J. Kidmose and C.S. Nisbeth and L. Thorling and K. Weckstr{\"o}m",
note = "This is the author{\textquoteright}s version of a work that was accepted for publication in Anthroprocene. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Anthroprocene, 35, 2021 DOI: 10.1016/j.ancene.2021.100302",
year = "2021",
month = sep,
day = "30",
doi = "10.1016/j.ancene.2021.100302",
language = "English",
volume = "35",
journal = "Anthropocene",
issn = "2213-3054",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Early historical forest clearance caused major degradation of water quality at Lake Væng, Denmark

AU - Bennike, O.

AU - Odgaard, B.V.

AU - Moorhouse, H.

AU - McGowan, S.

AU - Siggaard-Andersen, M.-L.

AU - Turner, B.

AU - Schomacker, A.

AU - Jessen, S.

AU - Kazmierczak, J.

AU - Olsen, J.

AU - Rasmussen, P.

AU - Kidmose, J.

AU - Nisbeth, C.S.

AU - Thorling, L.

AU - Weckström, K.

N1 - This is the author’s version of a work that was accepted for publication in Anthroprocene. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Anthroprocene, 35, 2021 DOI: 10.1016/j.ancene.2021.100302

PY - 2021/9/30

Y1 - 2021/9/30

N2 - Although humans have impacted their environment over millennia, details of these impacts, especially on aquatic systems, is still surprisingly scarce despite potential disturbance by early land use. This study examined a high-resolution radiocarbon-dated Holocene record from the Danish Lake Væng, using geochemical and biological proxies, and related the observed impacts to other lake records with catchment disturbance. The results indicate a lengthy and varying history of aquatic eutrophication linked to human activity. Modest impacts on the lake coincided with the first signs of landscape disturbance during the Neolithic (c. 4500 cal. yrs BP). Observed impacts intensified in the Late Bronze and Pre-Roman Iron Age. Viking Age/Medieval deforestation and erosional inputs to the lake associated with new ploughing technology (1200 cal. yrs BP), however, led to a major reorganisation of the aquatic ecosystem. Filamentous bloom-forming cyanobacteria, common today in heavily culturally impacted lakes, reached a historical maxima. The lake ecosystem subsequently recovered somewhat but remains eutrophic to date. The erosion record from Lake Væng shows a striking similarity with other Danish lake records, especially the notable increase in Medieval Period catchment inputs, which are observed in other European lacustrine records. Numerous European lowland lakes may have shifted into a degraded ecological state millennia ago, but degradation intensified during the onset of the Medieval Period. Hence, assuming pre-industrial conditions as relatively pristine reference baselines for more recent cultural eutrophication could be flawed in landscapes intensively used by humans for millennia.

AB - Although humans have impacted their environment over millennia, details of these impacts, especially on aquatic systems, is still surprisingly scarce despite potential disturbance by early land use. This study examined a high-resolution radiocarbon-dated Holocene record from the Danish Lake Væng, using geochemical and biological proxies, and related the observed impacts to other lake records with catchment disturbance. The results indicate a lengthy and varying history of aquatic eutrophication linked to human activity. Modest impacts on the lake coincided with the first signs of landscape disturbance during the Neolithic (c. 4500 cal. yrs BP). Observed impacts intensified in the Late Bronze and Pre-Roman Iron Age. Viking Age/Medieval deforestation and erosional inputs to the lake associated with new ploughing technology (1200 cal. yrs BP), however, led to a major reorganisation of the aquatic ecosystem. Filamentous bloom-forming cyanobacteria, common today in heavily culturally impacted lakes, reached a historical maxima. The lake ecosystem subsequently recovered somewhat but remains eutrophic to date. The erosion record from Lake Væng shows a striking similarity with other Danish lake records, especially the notable increase in Medieval Period catchment inputs, which are observed in other European lacustrine records. Numerous European lowland lakes may have shifted into a degraded ecological state millennia ago, but degradation intensified during the onset of the Medieval Period. Hence, assuming pre-industrial conditions as relatively pristine reference baselines for more recent cultural eutrophication could be flawed in landscapes intensively used by humans for millennia.

KW - Catchment-lake processes

KW - Holocene

KW - Inorganic phosphorus

KW - Macrofossils

KW - Pigments

KW - Soil erosion

KW - algal bloom

KW - aquatic ecosystem

KW - Bronze Age

KW - catchment

KW - cyanobacterium

KW - deforestation

KW - disturbance

KW - environmental degradation

KW - eutrophication

KW - forest clearance

KW - historical record

KW - human activity

KW - Iron Age

KW - lake ecosystem

KW - land use change

KW - Medieval

KW - Neolithic

KW - radiocarbon dating

KW - water quality

KW - Denmark

KW - Lake Vaeng

KW - Midtjylland

KW - Cyanobacteria

U2 - 10.1016/j.ancene.2021.100302

DO - 10.1016/j.ancene.2021.100302

M3 - Journal article

VL - 35

JO - Anthropocene

JF - Anthropocene

SN - 2213-3054

M1 - 100302

ER -