Coastal lagoons and beach ridges as complementary sedimentary archives for the reconstruction of Holocene relative sea-level changes

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Coastal lagoons and beach ridges as complementary sedimentary archives for the reconstruction of Holocene relative sea-level changes. / Sander, Lasse; Hede, Mikkel Ulfeldt; Fruergaard, Mikkel; Nielsen, Lars; Clemmensen, Lars B; Kroon, Aart; Johannessen, Peter N; Nielsen, Lars H.; Pejrup, Morten.

In: Terra Nova, Vol. 28, No. 1, 02.2016, p. 43-49.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Sander, L, Hede, MU, Fruergaard, M, Nielsen, L, Clemmensen, LB, Kroon, A, Johannessen, PN, Nielsen, LH & Pejrup, M 2016, 'Coastal lagoons and beach ridges as complementary sedimentary archives for the reconstruction of Holocene relative sea-level changes', Terra Nova, vol. 28, no. 1, pp. 43-49. https://doi.org/10.1111/ter.12187

APA

Sander, L., Hede, M. U., Fruergaard, M., Nielsen, L., Clemmensen, L. B., Kroon, A., ... Pejrup, M. (2016). Coastal lagoons and beach ridges as complementary sedimentary archives for the reconstruction of Holocene relative sea-level changes. Terra Nova, 28(1), 43-49. https://doi.org/10.1111/ter.12187

Vancouver

Sander L, Hede MU, Fruergaard M, Nielsen L, Clemmensen LB, Kroon A et al. Coastal lagoons and beach ridges as complementary sedimentary archives for the reconstruction of Holocene relative sea-level changes. Terra Nova. 2016 Feb;28(1):43-49. https://doi.org/10.1111/ter.12187

Author

Sander, Lasse ; Hede, Mikkel Ulfeldt ; Fruergaard, Mikkel ; Nielsen, Lars ; Clemmensen, Lars B ; Kroon, Aart ; Johannessen, Peter N ; Nielsen, Lars H. ; Pejrup, Morten. / Coastal lagoons and beach ridges as complementary sedimentary archives for the reconstruction of Holocene relative sea-level changes. In: Terra Nova. 2016 ; Vol. 28, No. 1. pp. 43-49.

Bibtex

@article{686c4ded6f1f4a91b43e07571b4b64f3,
title = "Coastal lagoons and beach ridges as complementary sedimentary archives for the reconstruction of Holocene relative sea-level changes",
abstract = "Coastal lagoons and beach ridges are genetically independent, though non-continuous, sedimentary archives. We here combine the results from two recently published studies in order to produce an 8000-year-long record of Holocene relative sea-level changes on the island of Sams{\o}, southern Kattegat, Denmark. The reconstruction of the initial mid-Holocene sea-level rise is based on the sedimentary infill from topography-confined coastal lagoons (Sander et al., Boreas, 2015b). Sea-level index points over the mid- to late Holocene period of sea-level stability and fall are retrieved from the internal structures of a wide beach-ridge system (Hede et al., The Holocene, 2015). Data from sediment coring, georadar and absolute dating are thus combined in an inter-disciplinary approach that is highly reproducible in micro-tidal environments characterised by high sediment supply. We show here that the commonly proximate occurrence of coastal lagoons and beach ridges allows us to produce seamless time series of relative sea-level changes from field sites in SW Scandinavia and in similar coastal environments.",
author = "Lasse Sander and Hede, {Mikkel Ulfeldt} and Mikkel Fruergaard and Lars Nielsen and Clemmensen, {Lars B} and Aart Kroon and Johannessen, {Peter N} and Nielsen, {Lars H.} and Morten Pejrup",
year = "2016",
month = "2",
doi = "10.1111/ter.12187",
language = "English",
volume = "28",
pages = "43--49",
journal = "Terra Nova",
issn = "0954-4879",
publisher = "Wiley-Blackwell",
number = "1",

}

RIS

TY - JOUR

T1 - Coastal lagoons and beach ridges as complementary sedimentary archives for the reconstruction of Holocene relative sea-level changes

AU - Sander, Lasse

AU - Hede, Mikkel Ulfeldt

AU - Fruergaard, Mikkel

AU - Nielsen, Lars

AU - Clemmensen, Lars B

AU - Kroon, Aart

AU - Johannessen, Peter N

AU - Nielsen, Lars H.

AU - Pejrup, Morten

PY - 2016/2

Y1 - 2016/2

N2 - Coastal lagoons and beach ridges are genetically independent, though non-continuous, sedimentary archives. We here combine the results from two recently published studies in order to produce an 8000-year-long record of Holocene relative sea-level changes on the island of Samsø, southern Kattegat, Denmark. The reconstruction of the initial mid-Holocene sea-level rise is based on the sedimentary infill from topography-confined coastal lagoons (Sander et al., Boreas, 2015b). Sea-level index points over the mid- to late Holocene period of sea-level stability and fall are retrieved from the internal structures of a wide beach-ridge system (Hede et al., The Holocene, 2015). Data from sediment coring, georadar and absolute dating are thus combined in an inter-disciplinary approach that is highly reproducible in micro-tidal environments characterised by high sediment supply. We show here that the commonly proximate occurrence of coastal lagoons and beach ridges allows us to produce seamless time series of relative sea-level changes from field sites in SW Scandinavia and in similar coastal environments.

AB - Coastal lagoons and beach ridges are genetically independent, though non-continuous, sedimentary archives. We here combine the results from two recently published studies in order to produce an 8000-year-long record of Holocene relative sea-level changes on the island of Samsø, southern Kattegat, Denmark. The reconstruction of the initial mid-Holocene sea-level rise is based on the sedimentary infill from topography-confined coastal lagoons (Sander et al., Boreas, 2015b). Sea-level index points over the mid- to late Holocene period of sea-level stability and fall are retrieved from the internal structures of a wide beach-ridge system (Hede et al., The Holocene, 2015). Data from sediment coring, georadar and absolute dating are thus combined in an inter-disciplinary approach that is highly reproducible in micro-tidal environments characterised by high sediment supply. We show here that the commonly proximate occurrence of coastal lagoons and beach ridges allows us to produce seamless time series of relative sea-level changes from field sites in SW Scandinavia and in similar coastal environments.

U2 - 10.1111/ter.12187

DO - 10.1111/ter.12187

M3 - Journal article

VL - 28

SP - 43

EP - 49

JO - Terra Nova

JF - Terra Nova

SN - 0954-4879

IS - 1

ER -

ID: 167476105