Development of plateau dunes controlled by iron pan formation and changes in land use and climate

Breuning‐Madsen, Henrik; Bird, Karen Lise; Balstrøm, Thomas; Elberling, Bo; Kroon, Aart; Lei, Else Benete

doi:10.1016/j.catena.2018.07.011

Cited by 5 publications

(5 citation statements)

References 16 publications

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“…Aeolian sand activities along the North Sea cost seems more distributed in time and are maybe more related to the Atlantic ocean' oscillations (e.g., Szokornik et al, 2008, Goslin et al, 2019. The findings from Ulbjerg supplements the finding by Breuning-Madsen et al (2018) and stress that significant in-land drift sand problems took place in the early 17 th century in Denmark. Furthermore, it suggest that research not only in the Little Ice Age but also in archaeology have to focus on the coldest years and decades during the Holocene, as the recent revised ice-core chronologies (Sigl et al, 2015) show that 8 of the 40 coldest years and 2 of the 12 coldest decades actually took place in the early 17 th century.…”

Section: Discussionmentioning

confidence: 70%

Quartz SAR optically stimulated lumines-cence (OSL) dating of sands from Ulbjerg Klint, Central Jutland, Denmark

Kristiansen¹,

Larsen²,

Srivastava³

et al. 2020

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Please note that the methodological descriptions may contain technical descriptions that are reused from previous reports and can be reused in future reports. We are grateful for help from Nina H. Nielsen, Pernille Trant, Ida-Emilie Nilsson and Thomas Ljungberg during the fieldwork, while background information was kindly provided by Mette Løvschal. The report for the archaeological fieldwork can be found at Viborg Museum, journal number: VSM 10569 Ulbjerg Klint. Financial support Viborg Museum covered Aarhus University' expenses for the fieldwork. Viborg Museum covered costs of the OSL analyses at University of St. Andrews, Scotland. It was funded by Agency for Culture and Palaces (Slotsog Kulturstyrelsen).

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Section: Discussionmentioning

confidence: 70%

Quartz SAR optically stimulated lumines-cence (OSL) dating of sands from Ulbjerg Klint, Central Jutland, Denmark

Kristiansen¹,

Larsen²,

Srivastava³

et al. 2020

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“…Van Asselen et al, 2017), impermeable deposits or resistant layers in the soil profile (e.g. Breuning-Madsen et al, 2018;Van der Meij et al, 2018), landforms and surface topography (e.g. Almquist-Jacobson and Foster, 1995;Mäkilä, 1997;Loisel et al, 2013), and anthropogenic influence (e.g.…”

Section: Introductionmentioning

confidence: 99%

Faded landscape: unravelling peat initiation and lateral expansion at one of northwest Europe's largest bog remnants

et al. 2023

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Abstract. On the mainland of northwest Europe generally only remnants of former peat landscapes subsist. Due to the poor preservation of these landscapes, alternative approaches to reconstruct peat initiation and lateral expansion are needed compared to regions with intact peat cover. Here we aim (1) to find explanatory variables within a digital soil mapping approach that allow us to reconstruct the pattern of peat initiation and lateral expansion within (and potentially beyond) peat remnants, and (2) to reconstruct peat initiation ages and lateral expansion for one of the largest bog remnants of the northwest European mainland, Fochteloërveen. Basal radiocarbon dates were obtained from the peat remnant, which formed the basis for subsequent analyses. We investigated the relationship between peat initiation age and three potential covariates: (1) total thickness of organic deposits, (2) elevation of the Pleistocene mineral surface that underlies the organic deposits, and (3) a constructed variable representing groundwater-fed wetness based on elevation of the mineral surface and current hydraulic head. Significant relationships were found with covariates (1) and (3), which were then used for subsequent modelling. Our results indicate simultaneous peat initiation at several loci in Fochteloërveen during the Early Holocene and continuous lateral expansion until 900 cal BP. Lateral expansion accelerated between 5500–3500 cal BP. Our approach is spatially explicit (i.e. results in a map of peat initiation ages), and it allows for a quantitative evaluation of the prediction using the standard deviation and comparison of predictions with validation points. The applied method based on covariate (1) is only useful where remnant peat survived, whereas covariate (3) may ultimately be applied to reconstruct peat initiation ages and lateral peatland expansion beyond the limits of peat remnants.

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“…Almquist-Jacobson and Foster, 1995;Mäkilä, 1997;Loisel et al, 2013), impermeable deposits or resistant layers in the soil profile (e.g. Breuning-Madsen et al, 2018;Van der Meij et al, 2018), and anthropogenic influence (e.g. Moore, 1975;Moore, 1993).…”

Section: Introductionmentioning

confidence: 99%

Dating basal peat: The geochronology of peat initiation revisited

Quik

Palstra

Beek

et al. 2022

Quaternary Geochronology

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Development of plateau dunes controlled by iron pan formation and changes in land use and climate

Cited by 5 publications

References 16 publications

Quartz SAR optically stimulated lumines-cence (OSL) dating of sands from Ulbjerg Klint, Central Jutland, Denmark

Quartz SAR optically stimulated lumines-cence (OSL) dating of sands from Ulbjerg Klint, Central Jutland, Denmark

Faded landscape: unravelling peat initiation and lateral expansion at one of northwest Europe's largest bog remnants

Dating basal peat: The geochronology of peat initiation revisited

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