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Persistent Identifier
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doi:10.18710/M3PWDV |
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Publication Date
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2026-05-05 |
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Title
| Replication data for "Siderite concretions in Svalbard Lake sediments capture 7000 years of extreme Arctic cold season climate change" |
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Author
| van der Bilt, WillemUniversity of BergenORCIDhttps://orcid.org/0000-0003-3157-451X
Csiszár, Barnabáshttps://ror.org/03zga2b32ORCIDhttps://orcid.org/0009-0008-7125-6261
Bulinova, Mariehttps://ror.org/00wge5k78ORCIDhttps://orcid.org/0000-0001-8733-975X
Rydland Pedersen, Leif-Erikhttps://ror.org/03zga2b32ORCIDhttps://orcid.org/0000-0003-3906-3079
Rouillard, Alexandrahttps://ror.org/00wge5k78ORCIDhttps://orcid.org/0000-0001-5778-6620
Thorseth, Ingunnhttps://ror.org/03zga2b32ORCIDhttps://orcid.org/0000-0003-3432-6968
Røthe, Torgeir Opelandhttps://ror.org/05phns765ORCIDhttps://orcid.org/0000-0001-7907-8246
Strzelecki, Mateusz Chttps://ror.org/00yae6e25ORCIDhttps://orcid.org/0000-0003-0479-3565
Schomacker, Andershttps://ror.org/00wge5k78ORCIDhttps://orcid.org/0000-0002-8031-9008 |
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Point of Contact
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Use email button above to contact.
van der Bilt, Willem (University of Bergen) |
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Description
| All proxy measurements performed on core STU-P1 for the upcoming publication that was only available as a pre-print at the time of submission: https://doi.org/10.22541/essoar.176617193.36041880/v1
The Arctic warms faster than anywhere else on Earth, and paleoclimate data are key to place this amplified response in a long-term context. But most past temperature proxies record growing season conditions, when their biological signal carriers are produced. This bias is important, as model simulations suggest that future Arctic warming will be strongest in winter. We help close this gap by presenting a 6.7 ka long record of Arctic cold season climate change. For this purpose, we characterize siderite mineral concretions in Svalbard Lake sediments that form under anoxic conditions, prompted by lingering lake ice coverage after severe winters. To do so with high micrometer-scale precision, we integrate hyperspectral imagery with X-Ray Fluorescence and Computed Tomography core scanning characteristics. This novel approach finds non-linear transitions in response to a complex interplay between abrupt (volcanic) and gradual (cyclic) paleoclimate forcings. |
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Subject
| Earth and Environmental Sciences |
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Keyword
| paleoclimate
holocene
svalbard
sediments
arctic |
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Related Publication
| Is Supplement To: van der Bilt, W. G. M., Csiszár, B., Bulínová, M., Pedersen, L.-E. R., Rouillard, A., Røthe, T. O., Strzelecki, M. C., & Schomacker, A. (2025). Siderite concretions in Svalbard lake sediments capture 7000 years of extreme Arctic cold season climate change. Authorea Preprints. doi https://doi.org/10.22541/essoar.176617193.36041880/v1 https://essopenarchive.org/doi/full/10.22541/essoar.176617193.36041880/v1 |
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Language
| English |
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Producer
| University of Bergen (UiB) https://www.uib.no/en |
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Distributor
| University of Bergen (UiB) https://dataverse.no/dataverse/uib |
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Depositor
| van der Bilt, Willem Godert Maria |
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Deposit Date
| 2026-03-19 |
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Date of Collection
| Start Date: 2022-01-08 |
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Data Type
| sediment core proxy data |
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Software
| PAST, Version: 4.17
XLSTAT, Version: 2025
MATLAB, Version: R2023b |