A square-rod piston sampler for lake sediments

Wright, H. E.

doi:10.1306/74d71807-2b21-11d7-8648000102c1865d

Cited by 401 publications

(197 citation statements)

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“…In each case, two overlapping cores were collected, ca. 0·5 m apart, using a 7·5 cm diameter Wright-modified square-rod piston corer (Wright, 1967) able to collect 1 m length core segments. Coring depths were adjusted to ensure that junctions between segments in the second core collected fell close to the middle of segments in the first.…”

Section: Sites and Samplingmentioning

confidence: 99%

Spatio-temporal patterns in Lateglacial and Holocene vegetation and climate of Finnmark, northernmost Europe

Huntley

Long

Allen

2013

Quaternary Science Reviews

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. (2013) 'Spatio-temporal patterns in late-glacial and Holocene vegetation and climate of Finnmark, northernmost Europe.', Quaternary science reviews., 70 . pp. 158-175. Further information on publisher's website:http://dx.doi.org/10. 1016/j.quascirev.2013.03.006 Publisher's copyright statement: NOTICE: this is the author's version of a work that was accepted for publication in Quaternary Science Reviews. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be re ected in this document. Changes may have been made to this work since it was submitted for publication. A de nitive version was subsequently published in Quaternary Science Reviews, 70, 2013Reviews, 70, , 10.1016Reviews, 70, /j.quascirev.2013 Additional information: Use policyThe full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-pro t purposes provided that:• a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders.Please consult the full DRO policy for further details. Further work on precisely-dated marine sediment cores will be necessary to understand the factors leading to the periodic and longer-term variations in strength of the North Cape Current.

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Section: Sites and Samplingmentioning

confidence: 99%

Spatio-temporal patterns in Lateglacial and Holocene vegetation and climate of Finnmark, northernmost Europe

Huntley

Long

Allen

2013

Quaternary Science Reviews

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“…were collected from the centres of the lakes using a 174 5 cm-diameter Livingston corer (Wright, 1967) operated from a rubber boat. Lithostratigraphies 175 were recorded in the field with respect to depth from surface water level at the coring location.…”

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confidence: 99%

Distal tephrochronology in volcanic regions: Challenges and insights from Kamchatkan lake sediments

Plunkett

Coulter

Пономарева

et al. 2015

Global and Planetary Change

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“…This corer appeared to recover a complete and undisturbed sample of the sediments, commonly including an algal mat at the sediment surface. The Livingstone (Wright 1967) cores at sites CM2 and HB also appear to be undisturbed. However, comparisons between diatom stratigraphic markers in cores K1 and C7A, collected at the same site, suggests that about 8 cm of sediment were missing from the top of core K1.…”

Section: Cores and Sedimentsmentioning

confidence: 95%

Chronology of Sediment Deposition in Upper Klamath Lake, Oregon

Colman

Bradbury

McGeehin

et al. 2004

Journal of Paleolimnology

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A combination of tephrochronology and 14 C, 210 Pb, and 137 Cs measurements provides a robust chronology for sedimentation in Upper Klamath Lake during the last 45 000 years. Mixing of surficial sediments and possible mobility of the radio-isotopes limit the usefulness of the 137 Cs and 210 Pb data, but 210 Pb profiles provide reasonable average sediment accumulation rates for the last 100-150 years. Radiocarbon ages near the top of the core are somewhat erratic and are too old, probably as a result of detrital organic carbon, which may have become a more common component in recent times as surrounding marshes were drained. Below the tops of the cores, radiocarbon ages in the center of the basin appear to be about 400 years too old, while those on the margin appear to be accurate, based on comparisons with tephra layers of known age.Taken together, the data can be combined into reasonable age models for each site. Sediments have accumulated at site K1, near the center of the basin, about 2 times faster than at site CM2, on the margin of the lake. The rates are about 0.10 and 0.05 cm/yr, respectively. The chronological data also indicate that accumulation rates were slower during the early to middle Holocene than during the late Holocene, consistent with increasing wetness in the late Holocene.

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A square-rod piston sampler for lake sediments

Cited by 401 publications

References 0 publications

Spatio-temporal patterns in Lateglacial and Holocene vegetation and climate of Finnmark, northernmost Europe

Spatio-temporal patterns in Lateglacial and Holocene vegetation and climate of Finnmark, northernmost Europe

Distal tephrochronology in volcanic regions: Challenges and insights from Kamchatkan lake sediments

Chronology of Sediment Deposition in Upper Klamath Lake, Oregon

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