| 1. |
- Kylander, Malin E., 1977-, et al.
(författare)
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Storm chasing : Tracking Holocene storminess in southern Sweden using mineral proxies from inland and coastal peat bogs
- 2023
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Ingår i: Quaternary Science Reviews. - : Elsevier BV. - 0277-3791 .- 1873-457X. ; 299, s. 107854-
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Tidskriftsartikel (refereegranskat)abstract
- Severe extratropical winter storms are a recurrent feature of the European climate and cause widespread socioeconomic losses. Due to insufficient long-term data, it remains unclear whether storminess has shown a notable response to changes in external forcing over the past millennia, which impacts our ability to project future storminess in a changing climate. Reconstructing past storm variability is essential to improving our understanding of storms on these longer, missing timescales. Peat sequences from coastal ombrotrophic bogs are increasingly used for this purpose, where greater quantities of coarser grained beach sand are deposited by strong winds during storm events. Moving inland however, storm intensity decreases, as does sand availability, muting potential paleostorm signals in bogs. We circumvent these issues by taking the innovative approach of using mid-infrared (MIR) spectral data, supported by elemental information, from the inorganic fraction of Store Mosse Dune South (SMDS), a 5000-year-old sequence from a large peatland located in southern Sweden. We infer past changes in mineral composition and thereby, the grain size of the deposited material. The record is dominated by quartz, whose coarse nature was confirmed through analyses of potential local source sediments. This was supported by further mineralogical and elemental proxies of atmospheric input. Comparison of SMDS with within-bog and regionally relevant records showed that there is a difference in proxy and site response to what should be similar timing in shifts in storminess over the-100 km transect considered. We suggest the construction of regional storm stacks, built here by applying changepoint modelling to four transect sites jointly. This modelling approach has the effect of reinforcing signals in common while reducing the influence of random noise. The resulting Southern Sweden-Storm Stack dates stormier periods to 4495-4290, 3880-3790, 2885-2855, 2300-2005, 1175-1065 and 715-425 cal yr BP. By comparing with a newly constructed Western Scotland-Storm Stack and proximal dune records, we argue that regional storm stacks allow us to better compare past storminess over wider areas, gauge storm track movements and by extension, increase our understanding of the drivers of storminess on centennial to millennial timescales.
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| 2. |
- Hallin, Caroline, et al.
(författare)
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Stormfloder - en kunskapsöversikt av metoder för att identifiera och kvantifiera extrema havsvattenstånd
- 2022
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Rapport (övrigt vetenskapligt/konstnärligt)abstract
- Stormfloder är tillfälligt förhöjda vattennivåer orsakade av meteorologiska fenomen som kan ge upphov till översvämningar utmed kusten. När havsnivån stiger till följd av klimatförändringarna och befolkningen utmed kusten ökar, leder det till en ökad översvämningsrisk. Risk kan beskrivas som en kombination av sannolikhet och konsekvens. För att kunna bestämma var som är säkert att bygga och hur befintlig bebyggelse kan skyddas behövs kunskap om hur höga vattenstånd som kan uppstå, hur stora vågorna kan bli och hur länge en storm varar. Vanligtvis utgår man från en sannolikhetsnivå, till exempel att ett område kan tillåtas att översvämmas i genomsnitt vart hundrade år, och bestämmer sedan vilken vattennivå det motsvarar genom extremvärdesanalys av tillgängliga mätdata. För att göra en så säker förutsägelse som möjligt behövs en lång tidserie (i förhållande till den beräknade frekvensen). Det är även viktigt att veta om observationerna är representativa även för framtida förhållanden. Vid stadsplanering och dimensionering av kustskydd är planeringshorisonten i storleksordningen 25 – 200 år, och känsliga byggnader, till exempel vattenverk, kärnkraftverk, och sjukhus dimensioneras för långa återkomsttider, i storleksordningen 200 – 10 000 år. I dagsläget är det svårt att med rimlig säkerhet bedöma konsekvenserna av så ovanliga händelser och hur de kommer att utvecklas i framtiden. Problemet är att mätserierna av stormfloder ofta är för korta för att göra en robust analys. I den här rapporten undersöks hur analyser av stormfloder kan förbättras genom att ta hänsyn till händelser som inträffade innan vattenståndsmätningarna började samt hur de påverkas av klimatvariationer och klimatförändringar.Genom en internationell litteraturstudie undersöks vilka metoder som kan användas för att utöka dataserierna genom att studera historiska dokument, geologiska undersökningar, samt hydrodynamisk modellering. Vidare studeras hur olika statistiska modeller kan användas för att inkludera dessa faktorer i extremvärdesanalys. En fördjupad studie görs av utvalda länder runt Nordsjön och Östersjön (Danmark, England, Schleswig-Holstein och Nederländerna). Analysen visar på stora skillnader, både mellan de studerade länderna och i jämförelse med Sverige, avseende dimensionerande händelser, metoder för extremvärdesanalys, samt hur historiska stormfloder beaktas i riskanalyser.Om översvämningsrisker underskattas, föreligger risk för stora materiella skador och i värsta fall människors liv och hälsa. Om översvämningsrisker å andra sidan överskattas innebär det en suboptimal markanvändning i kustnära områden och att översvämningsskydd överdimensioneras med negativa samhällsekonomiska och miljömässiga effekter till följd. För att möjliggöra en hållbar utveckling av kustnära områden är därför korrekta bedömningar av översvämningsrisken en nyckelfaktor. Metoderna som presenteras i den här studien kan appliceras på Sveriges kuster för öka kunskapsunderlaget om stormfloder och möjliggöra mer robusta riskanalyser och dimensioneringsunderlag för kustskydd.
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| 3. |
- Lindvall, Alma, et al.
(författare)
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Bleaching of quartz OSL signals under natural and laboratory light conditions
- 2017
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Ingår i: Ancient TL. - 0735-1348. ; 35:2, s. 12-20
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Tidskriftsartikel (refereegranskat)abstract
- Resetting or bleaching of the luminescence signal is a fundamental factor in luminescence dating. It must occur in nature during the event or process to be dated for an accurate age, but if it happens during sample processing in the laboratory it destroys the sample for dating purposes. In this study, we look into bleaching of quartz optically stimulated luminescence by light in nature and in the laboratory. Unsieved quartz-rich extracts and 180–250 µm quartz grains with known doses wereexposed to outdoor light and laboratory light sources, respectively, and the change in dose with exposure time was measured. The outdoor conditions included direct sunlight, diffuse light from a cloud-covered sky and weak twilight, while indoor light sources were white fluorescent light, light from a computer screen and red darkroom light. Complete resetting took place only in daylight and was faster during sunny than cloudy conditions, and with bleaching rates that changed with exposure time. For all other light sources, including the darkroom lights, bleaching occurred to various degrees but was not complete after the longest exposure, which ranged from 15 min to 24 hours. The results show that some bleaching occurs even by low-intensity light with a limited spectrum. This implies that care should be taken in the laboratory not to expose samples to any light unnecessarily, but at the same time gives hope for bleaching in nature even in settings with limited or variable light conditions.
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| 4. |
- Alexanderson, Helena, et al.
(författare)
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An Arctic perspective on dating Mid-Late Pleistocene environmental history
- 2014
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Ingår i: Quaternary Science Reviews. - : Elsevier BV. - 0277-3791 .- 1873-457X. ; 92, s. 9-31
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Forskningsöversikt (refereegranskat)abstract
- To better understand Pleistocene climatic changes in the Arctic, integrated palaeoenvironmental andpalaeoclimatic signals from a variety of marine and terrestrial geological records as well as geochronologicage control are required, not least for correlation to extra-Arctic records. In this paper we discuss,from an Arctic perspective, methods and correlation tools that are commonly used to date ArcticPleistocene marine and terrestrial events. We review the state of the art of Arctic geochronology, withfocus on factors that affect the possibility and quality of dating, and support this overview by examples ofapplication of modern dating methods to Arctic terrestrial and marine sequences.Event stratigraphy and numerical ages are important tools used in the Arctic to correlate fragmentedterrestrial records and to establish regional stratigraphic schemes. Age control is commonly provided byradiocarbon, luminescence or cosmogenic exposure ages. Arctic Ocean deep-sea sediment successionscan be correlated over large distances based on geochemical and physical property proxies for sedimentcomposition, patterns in palaeomagnetic records and, increasingly, biostratigraphic data. Many of theseproxies reveal cyclical patterns that provide a basis for astronomical tuning.Recent advances in dating technology, calibration and age modelling allow for measuring smallerquantities of material and to more precisely date previously undatable material (i.e. foraminifera for 14C,and single-grain luminescence). However, for much of the Pleistocene there are still limits to the resolutionof most dating methods. Consequently improving the accuracy and precision (analytical andgeological uncertainty) of dating methods through technological advances and better understanding ofprocesses are important tasks for the future. Another challenge is to better integrate marine andterrestrial records, which could be aided by targeting continental shelf and lake records, exploringproxies that occur in both settings, and by creating joint research networks that promote collaborationbetween marine and terrestrial geologists and modellers.
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| 5. |
- Alexanderson, Helena, et al.
(författare)
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MIS 3 age of the Veiki moraine in N Sweden – Dating the landform record of an intermediate-sized ice sheet in Scandinavia
- 2022
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Ingår i: Arctic, Antarctic and Alpine research. - : Informa UK Limited. - 1523-0430 .- 1938-4246. ; 54:1, s. 239-261
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Tidskriftsartikel (refereegranskat)abstract
- The Veiki moraine in northern Sweden, a geomorphologically distinct landscape of ice-walled lake plains, has been interpreted to represent the former margin of an intermediate-sized pre–Last Glacial Maximum (LGM) Fennoscandian ice sheet, but its age is debated as either marine isotope stage (MIS) 5c or MIS 3. We have applied optically stimulated luminescence (OSL) and radiocarbon dating to four sites within the northern part of the Veiki moraine to establish its chronology. The radiocarbon ages provide only minimum ages and most OSL ages have low precision due to poor luminescence characteristics and problems with incomplete bleaching, leading to two alternative ages. In either case, the OSL dating places the Veiki moraine formation in MIS 3 (best estimate 56–39 ka). Sedimentation continued in the low-lying centers of some plateaus (ice-walled lake plains) during MIS 3 and during the Holocene, with a break during the Last Glacial Maximum when the area was ice covered. We speculatively constrain the broad timing further by relating the sequence of events to other climate records. We suggest that ice margin retreat to the west of the Veiki area took place during Greenland Interstadial (GI) 16.1 (58.0–56.5 ka) and that limited ice advances, which led to debris-covered ice margins in the Veiki zone, occurred during the following stadials GS-16.1 to 15.1 (56.5–54.2 ka). The GI-14 interstadial, which began 54.2 ka and lasted ~5.9 ka, could then be the period when the ice within the dead-ice landscape melted, first leading to ice-walled lakes and later to the inversed topography characteristic of the Veiki landscape.
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| 6. |
- Blomdin, Robin, et al.
(författare)
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Timing of the deglaciation in Southern Patagonia : testing the applicability of k feldspar irsl
- 2012
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Ingår i: Quaternary Geochronology. - : Elsevier BV. - 1871-1014 .- 1878-0350. ; 10, s. 264-272
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Tidskriftsartikel (refereegranskat)abstract
- The timing of the ice margin retreat of the Late Glacial Patagonian Ice Sheet (PIS) in southern Patagonia has been the object of discussion for many years. In order to resolve questions about the complex response of the PIS to past climate change, any geological interpretation and data modelling need evaluation against an absolute chronology. The aim of this project is to investigate the applicability of OSL dating to sediments from southern Patagonia; in particular, we examine the dating potential of K-feldspar IRSL signals. Samples were collected from landforms interpreted as being deposited during deglaciation of the PIS, with an expected age range of 17 and 22 ka, and from recently deposited sediment. We measure small aliquots and single grain distributions using an IR50 SAR protocol with IRSL stimulation at 50 degrees C following a preheat at 250 degrees C (held for 60 s). Uncertainties are assigned to our individual dose estimates based on the over-dispersion (OD) observed in laboratory gamma dose recovery experiments (22% for small aliquots and 18% for single grains). Then the possible effects of incomplete bleaching and differential fading are examined. For our natural samples we observe environmental ODs between 30 and 130% and mean residual doses between similar to 30 and 80 Gy. Minimum age models are used to identify the part of the dose population that is most likely to have been well-bleached and results from these models are compared. The models give ages that are consistent with each other; this may imply that they successfully identified the fully-bleached grains in the distributions, although there are some discrepancies between our small aliquot and single grain data. We observe large fading rates (on average 7.9 +/- 0.6%/decade for large aliquots) but nevertheless a comparison of our fading corrected ages with the expected age range shows that 2 out of 3 ages are consistent with geological interpretation and an established radiocarbon and cosmogenic nuclide chronology. We conclude that these investigations suggest that fading corrections can be based on laboratory average small aliquot/single grain fading rates. The third age is supported by an alternative geological interpretation, and the two ages consistent with the existing chronology imply that in the Strait of the Magellan the hills of the Brunswick peninsula (>70 m.a.s.l) were deglaciated at around 22 ka.
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| 7. |
- Håkansson, Lena, et al.
(författare)
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The late Pleistocene glacial history of Jameson Land peninsula, central East Greenland, derived from cosmogenic 10Be and 26Al exposure dating
- 2009
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Ingår i: Boreas. - : Wiley. - 0300-9483 .- 1502-3885. ; 38, s. 244-260
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Tidskriftsartikel (refereegranskat)abstract
- Previous work has presented contrasting views of the last glaciation on Jameson Land, central East Greenland, and still there is debate about whether the area was: (i) ice-free, (ii) covered with a local non-erosive ice cap(s), or (iii) overridden by the Greenland Ice Sheet during the Last Glacial Maximum (LGM). Here, we use cosmogenic exposure ages from erratics to reconcile these contrasting views. A total of 43 erratics resting on weathered sandstone and on sediment-covered surfaces were sampled from four areas on interior Jameson Land; they give 10Be ages between 10.9 and 269.1 kyr. Eight erratics on weathered sandstone and till-covered surfaces cluster around ∼70 kyr, whereas 10Be ages from erratics on glaciofluvial landforms are substantially younger and range between 10.9 and 47.2 kyr. Deflation is thought to be an important process on the sediment-covered surfaces and the youngest exposure ages are suggested to result from exhumation. The older (>70 kyr) samples have discordant 26Al and 10Be data and are interpreted to have been deposited by the Greenland Ice Sheet several glacial cycles ago. The younger exposure ages (≤70 kyr) are interpreted to represent deposition by the ice sheet during the Late Saalian and by an advance from the local Liverpool Land ice cap in the Early Weichselian. The exposure ages younger than Saalian are explained by periods of shielding by non-erosive ice during the Weichselian glaciation. Our work supports previous studies in that the Saalian Ice Sheet advance was the last to deposit thick sediment sequences and western erratics on interior Jameson Land. However, instead of Jameson Land being ice-free throughout the Weichselian, we document that local ice with limited erosion potential covered and shielded large areas for substantial periods of the last glacial cycle.
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| 8. |
- West, Gabriel, 1978-
(författare)
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A multimethod approach to dating Quaternary sediments from the Arctic Ocean
- 2022
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Doktorsavhandling (övrigt vetenskapligt/konstnärligt)abstract
- The marine sedimentary environment in the polar regions is different from the rest of the world’s oceans, as it is greatly influenced by the cryosphere. In the Arctic, sea ice and icebergs can transport vast amounts of sediments, delivered by extensive fluvial systems from the surrounding continents, which have been shaped by the waxing and waning of large terrestrial ice sheets during the Quaternary period. Reconstructing palaeoenvironmental changes in the Arctic Ocean during this time requires the accurate dating of marine sediment cores, something that has been more difficult than in most other marine environments.This thesis investigates and integrates less developed methods to date marine sediments in the Arctic Ocean. It focuses on applying amino acid racemization geochronology and optically stimulated luminescence dating to sediments from across the Arctic Ocean, accompanied by palaeo- and rock magnetic measurements, and sedimentological analyses.The presented results show that racemization of aspartic and glutamic acids in foraminifera follow a predictable rate at the Yermak Plateau and the Greenland and Iceland Seas, and existing calibrated age equations can be used to confidently date late Quaternary sediments in these regions. Purportedly high rates of racemization are observed in the benthic foraminifera, Cibicidoides wuellerstorfi from central Arctic sediments, confirming that the high rates cannot be attributed to taxonomic effects. Their possible causes, which include variable environmental and diagenetic conditions are considered. Optically stimulated luminescence dating of quartz grains from the Lomonosov Ridge provide much needed absolute age control for sediments from this area, further constraining the timing of glacial activity near the Siberian margin and illustrating the potentials of luminescence dating as a geochronological tool in the Arctic. Palaeomagnetic and rock magnetic analyses provide additional evidence that putative polarity reversals and excursions are not always due to geomagnetic field behaviour but are possibly linked to glacial/interglacial modulation of the magnetic mineralogy.
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| 9. |
- West, Gabriel, et al.
(författare)
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Optically stimulated luminescence dating supports pre-Eemian age for glacial ice on the Lomonosov Ridge off the East Siberian continental shelf
- 2021
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Ingår i: Quaternary Science Reviews. - : Elsevier BV. - 0277-3791 .- 1873-457X. ; 267
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Tidskriftsartikel (refereegranskat)abstract
- Establishing a solid chronological framework for Arctic marine sediments is a critical first step towards glacial and palaeoceanographic reconstructions. However, this has historically been more challenging than elsewhere in the world, and often results in core chronologies and subsequent paleoenvironmental reconstructions being questioned and overturned. Optically stimulated luminescence (OSL) dating provided important constraints on late Quaternary ages for central Arctic marine sediments, and has considerable potential to underpin chronologies in other parts of the Arctic Ocean. This study applies OSL and infrared stimulated luminescence (IRSL) geochronology to multi-grain quartz and feldspar samples from a sediment core collected from the Lomonosov Ridge off the Siberian shelf during the 2014 SWERUS-C3 Expedition. Testing and advancing the proposed chronology of late Quaternary sediments in this part of the Arctic is essential to better constrain the timing of ice sheet growth on the Siberian Arctic shelf and subsequent ice shelf development in the Arctic Ocean. The results of luminescence dating support a pre-Eemian age for extensive ice grounding and scouring of the southern Lomonosov Ridge. Furthermore, we combine the OSL ages with data from rock magnetic measurements and propose an age-depth model for cores in this region. As in other areas in the Arctic, magnetic grain size/mineralogy profiles resemble the global oxygen isotope curve and may have the potential to be a dating tool. This can be tested and further refined in future studies that obtain longer sedimentary archives. Our results also indicate that changes in the inclination of the natural remanent magnetisation do not reflect geomagnetic field variation in the investigated sediment cores.
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| 10. |
- Heyman, Jakob, 1979-, et al.
(författare)
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A paleoglaciological reconstruction for Bayan Har Shan, NE Tibetan Plateau
- 2009
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Konferensbidrag (refereegranskat)abstract
- The paleoglaciology of the Tibetan Plateau has remained elusive because extensive areas still lack detailed scrutiny. We here present a paleoglaciological reconstruction for the Bayan Har Shan region, NE Tibetan Plateau, which could serve as a working model to investigate other poorly investigated regions. The reconstruction is primarily based on three methods for revealing the glacial history; 1) remote sensing (geomorphology), 2) field studies (stratigraphy), and 3) numerical dating techniques. Remote sensing (SRTM elevation data, Landsat ETM+ satellite imagery and Google Earth) of a 136 500 km2 area reveals an abundance of glacial landforms in the highest mountain areas and an absence of glacial landforms on intervening plateau surfaces. Stratigraphical data collected during three field seasons supplement the picture emerging from remote sensing. Glacial deposits (including erratic boulders and till) occur in the elevated mountain areas but are absent on the intervening plateau areas. Marginal moraines in central Bayan Har can be grouped to represent at least three separate glacial extents and scattered observations of glacial deposits indicate the presence of a fourth (and maximum) glacial extent. To tie the glacial geological record to a chronology we have employed terrestrial cosmogenic nuclide (TCN) exposure and optically stimulated luminescence (OSL) dating. Beryllium apparent exposure ages of 65 glacial boulders, surface cobbles/pebbles and depth profile samples yield minimum ages for the three youngest glacial extents of 40-65 ka, 60-100 ka, and 95-165 ka (with the wide age ranges due to TCN dating uncertainties). A preliminary OSL age of c. 160 ka from glacial sediments of the oldest of these glacial extents supports our interpretation based on TCN dating. The glacial extent presented here is more restricted than most previous reconstructions, most notably with very restricted glaciers over at least the last 40-65 ka. These results indicate that while continental-scale ice sheets evolved and disappeared in North America and Eurasia over the last half of the last glacial cycle, the NE corner of the Tibetan Plateau experienced relatively minor glacial fluctuations.
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