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Marine sediment core data from the Lomonosov Ridge off Greenland, Arctic Ocean

Matt O'Regan

Newer versions of this dataset are available

Sedimentological data from six marine sediment cores collected from the Lomonosov Ridge, Arctic Ocean. The sediment cores were collected on two separate icebreaker led expeditions to the Arctic Ocean in 2012 (LOMROG-12) and 2016 (AO16). The data is used to investigate the occurrence of sub-polar planktic foraminifera on the Lomonosov Ridge north of Greenland during interglacials periods of the last 500 thousand years. The data set includes physical property measurements, geochemical measurements, sediment grain size, and relative abundances of foraminifera.

MarineSediment coresArctic OceanLomonosov RidgePleistoceneChronologyLithostratigraphyPlanktonic foraminiferaTurborotalita quinquelobaBiostratigraphy

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Name

oden-ao-2016-sediment-lomonosov

Version

1

Citation

Matt O'Regan (2019) Marine sediment core data from the Lomonosov Ridge off Greenland, Arctic Ocean. Dataset version 1. Bolin Centre Database. https://doi.org/10.17043/oden-ao-2016-sediment-lomonosov-1

References

O'Regan, M., Coxall, H. K., Cronin, T. M., Gyllencreutz, R., Jakobsson, M., Kaboth, S., Löwemark, L., Wiers, S., and West, G. (2019): Stratigraphic Occurrences of Sub-Polar Planktic Foraminifera in Pleistocene Sediments on the Lomonosov Ridge, Arctic Ocean. Frontiers in Earth Science, 7, 71. https://doi.org/10.3389/feart.2019.00071

Data description

The dataset is included in one xlsx file with 12 data sheets.

The core data includes:
1. Relative foraminifera abundance counts in the >125 μm size fraction, and the occurrence of *Turborotalita quinqueloba* in the 63-125 μm. Relative abundance is defined as: Abundant (≥50% of sample), Common (>100 specimens), Few (50-100 specimens), Rare (< 50 specimens), Barren (0 specimens). Intervals where *T. quinqueloba* occurs are marked by an 'X'. 2. Grain size measurements acquired at a 1-2 cm downcore resolution using a Malvern Mastersizer 3000 laser diffraction particle analyser. Data is averaged from 5 replicate measurements at each sample position. Data includes: % volume of sand, silt and clay, as well as the fine, medium and coarse silt volumes. 3. Physical properties measured using a GeoTek Multi-Sensor Core Logger: Bulk Density (g/cc) and Bartington loop sensor Magnetic Susceptibility (SI × 10⁻⁵). 4. ITRAX XRF scanner data at a 2 mm downcore resolution.

Spreadsheet tabs:
LOMROG12_PC07_Foraminifera; AO16_5PC_Foraminifera; LOMORG12-6PC_Grainsize; LOMORG12-7PC_Grainsize; LOMORG12-12PC_Grainsize; MSCL Data; LOMROG12-3PC_ITRAX_XRF; LOMROG12-6PC_ITRAX_XRF; LOMROG12-7PC_ITRAX_XRF; LOMROG12-12PC_ITRAX_XRF; AO16-12PC_ITRAX_XRF; AO16-5PC_ITRAX_XRF

Comments

The six sediment cores are:<br /> LOMROG12-3PC, 1607 m water depth, 87.7247°N, -54.4253°E;<br /> LOMROG12-6PC, 2923 m water depth, 88.2511°N, -46.3972°E;<br /> LOMROG12-7PC, 2953 m water depth, 88.1976°N, -55.6845°E;<br /> LOMROG12-12PC, 1366 m water depth, 88.1085°N, 134.6451°E;<br /> AO16-5PC, 1253 m water depth, 89.0780°N, -130.5470°E;<br /> AO16-12PC, 1269 m water depth, 87.8577°N, 136.9875°E

Project

Material for this study was collected by the Swedish icebreaker Oden on the Danish-Swedish Lomonosov Ridge off Greenland III in 2012 (LOMROG12), and the Canadian-Swedish Arctic Ocean 2016 expedition (AO16).

Publisher

Bolin Centre Database

First name

Matt

Last name or organisation

O'Regan

Email address

matt.oregan@geo.su.se

Address

Department of Geological Sciences, Stockholm University

Postal code

SE-106 91

City

Stockholm

Country

Sweden

GCMD science keyword

Earth science > Oceans > Marine sediments

GCMD location

Ocean > Arctic Ocean

Dataset language

English

DOI

10.17043/oden-ao-2016-sediment-lomonosov-1

Time

2019-04-09T12:52:42+00:00

Versions

  • 1 2022-01-26T13:47:43.752567+00:00
  • 1 2021-12-03T16:09:29.752589+00:00
  • 1 2021-10-29T06:23:12.202887+00:00
  • 1 2019-04-09T12:52:42+00:00