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  • 1
    Publication Date: 2023-07-07
    Keywords: AGE; COMPCORE; Composite Core; CON01-6; CON01-605; Diatoms, δ18O; Lake Baikal, Russia; Precipitation, annual total; Vereshchagin
    Type: Dataset
    Format: text/tab-separated-values, 66 data points
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  • 2
    Publication Date: 2023-07-07
    Keywords: Age; BAIK13-1C; BAIK13-4F; BAIK13-7A; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatoms, δ18O; Event label; Lake Baikal, Russia; PCUWI; Piston corer, UWITEC; Precipitation, annual total
    Type: Dataset
    Format: text/tab-separated-values, 126 data points
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  • 3
    Publication Date: 2023-07-07
    Keywords: AGE; AWI Arctic Land Expedition; DEPTH, sediment/rock; Diatoms, δ18O; Diatoms, δ30Si; ELGYGYTGYN; Elgygytgyn2003; Elgygytgyn crater lake, Sibiria, Russia; Event label; GCUWI; Gravity corer, UWITEC; Lake Elgygytgyn - Climate History of the Arctic since 3.6 Million Years; Lz1029-5; Lz1029-9; Mass spectrometer, Finnigan, MAT 253; PCUWI; Piston corer, UWITEC; RU-Land_2003_Elgygytgyn
    Type: Dataset
    Format: text/tab-separated-values, 101 data points
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  • 4
    Publication Date: 2023-07-07
    Keywords: Age, 14C AMS; Age, 14C calibrated; Age, dated; Age, dated standard error; AWI Arctic Land Expedition; COMPCORE; Composite Core; DEPTH, sediment/rock; ELGYGYTGYN; Elgygytgyn2003; Elgygytgyn crater lake, Sibiria, Russia; Laboratory code/label; Lake Elgygytgyn - Climate History of the Arctic since 3.6 Million Years; Lz1029; RU-Land_2003_Elgygytgyn
    Type: Dataset
    Format: text/tab-separated-values, 25 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Swann, George E A; Leng, Melanie J; Juschus, Olaf; Melles, Martin; Brigham-Grette, Julie; Sloane, Hilary J (2010): A combined oxygen and silicon diatom isotope record of Late Quaternary change in Lake El'gygytgyn, North East Siberia. Quaternary Science Reviews, 29(5-6), 774-786, https://doi.org/10.1016/j.quascirev.2009.11.024
    Publication Date: 2023-07-07
    Description: Determining the response of sites within the Arctic Circle to long-term climatic change remains an essential pre-requisite for assessing the susceptibility of these regions to future global warming and Arctic amplification. To date, existing records from North East Russia have demonstrated significant spatial variability across the region during the late Quaternary. Here we present diatom d18O and d30Si data from Lake El'gygytgyn, Russia, and suggest environmental changes that would have impacted across West Beringia from the Last Glacial Maximum to the modern day. In combination with other records, the results raise the potential for climatic teleconnections to exist between the region and sites in the North Atlantic. The presence of a series of 2-3 per mil decreases in d18Odiatom during both the Last Glacial and the Holocene indicates the sensitivity of the region to perturbations in the global climate system. Evidence of an unusually long Holocene thermal maximum from 11.4 ka BP to 7.6 ka BP is followed by a cooling trend through the remainder of the Holocene in response to changes in solar insolation. This is culminated over the last 900 years by a significant decrease in d18Odiatom of 2.3 per mil, which may be related to a strengthening and easterly shift of the Aleutian Low in addition to possible changes in precipitation seasonality.
    Keywords: ELGYGYTGYN; Lake Elgygytgyn - Climate History of the Arctic since 3.6 Million Years
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 6
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    PANGAEA
    In:  Supplement to: Swann, George E A; Mackay, Anson W; Vologina, Elena G; Jones, Matthew D; Panizzo, Virginia N; Leng, Melanie J; Sloane, Hilary J; Snelling, Andrea M; Sturm, Michael (2018): Lake Baikal isotope records of Holocene Central Asian precipitation. Quaternary Science Reviews, 189, 210-222, https://doi.org/10.1016/j.quascirev.2018.04.013
    Publication Date: 2023-07-07
    Description: Climate models currently provide conflicting predictions of future climate change across Central Asia. With concern over the potential for a change in water availability to impact communities and ecosystems across the region, an understanding of historical trends in precipitation is required to aid model development and assess the vulnerability of the region to future changes in the hydroclimate. Here we present a record from Lake Baikal, located in the southern Siberian region of central Asia close to the Mongolian border, which demonstrates a relationship between the oxygen isotope composition of diatom silica (δ18Odiatom) and precipitation to the region over the 20th and 21st Century. From this, we suggest that annual rates of precipitation in recent times are at their lowest for the past 10,000 years and identify significant long-term variations in precipitation throughout the early to late Holocene interval. Based on comparisons to other regional records, these trends are suggested to reflect conditions across the wider Central Asian region around Lake Baikal and highlight the potential for further changes in precipitation with future climate change.
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 7
    ISSN: 1573-0417
    Keywords: stable isotopes ; authigenic carbonate ; ostracods ; palaeolimnology ; Konya Basin ; Turkey
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences
    Notes: Abstract The Konya plain in south central Anatolia, Turkey, which is now largely dry, was occupied around the time of the Last Glacial Maximum by a fresh-oligosaline lake covering more than 4000 km2. Sediment cores from three residual water bodies (Pinarbaşi, Akgöl and Süleymanhaci) within the larger Pleistocene lake basin, have been analysed using a multidisciplinary approach. The sediment sequences are dated as spanning the last 50 Ka years, although breaks in sedimentation mean that there is only partial chronological overlap between them. Carbon and oxygen isotope analyses on lacustrine carbonate from the three cores give contrasting isotope profiles which reflect the different ages and independent hydrological behaviour of different sub-basins through the late Quaternary. Distinguishing changes that are regional from local effects is aided by modern isotope hydrology studies and by comparing the carbonate δ13C and δ18O values to diatom and other analyses undertaken on the same cores.
    Type of Medium: Electronic Resource
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  • 8
    Publication Date: 2011-12-01
    Description: Multiproxy analysis of a well-dated 25 ka lake sediment sequence from Lake Challa, on the eastern flank of Mount Kilimanjaro (East Africa), reveals the climatic controls that govern both the lake's paleohydrology and the climate-proxy record contained in the mountain's receding ice cap. The oxygen isotope record extracted from diatom silica ({delta}18Odiatom) in Lake Challa sediments captured dry conditions during the last glacial period and a wet late-glacial transition to the Holocene interrupted by Younger Dryas drought. Further, it faithfully traced gradual weakening of the southeastern monsoon during the Holocene. Overall, {delta}18Odiatom matches the branched isoprenoid tetraether (BIT) index of rainfall-induced soil runoff, except during 25-22 ka and the past 5 k.y. when insolation forcing due to orbital precession enhanced the northeastern monsoon. This pattern arises because during these two periods, a weakened southeastern monsoon reduced the amount of rainfall during the long rainy season and enhanced the opposing effect of evaporation intensity and/or length of the austral winter dry season. Importantly, our lake-based reconstruction of moisture-balance seasonality in equatorial East Africa also helps us understand the oxygen isotope record contained in Mount Kilimanjaro ice. Negative correlation between ice core {delta}18O and Lake Challa {delta}18Odiatom implies that moisture balance is not the primary climate control on the long-term trend in ice core {delta}18O.
    Print ISSN: 0091-7613
    Electronic ISSN: 1943-2682
    Topics: Geosciences
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  • 9
    Publication Date: 2022-05-26
    Description: Author Posting. © The Author(s), 2010. This is the author's version of the work. It is posted here by permission of Cambridge University Press for personal use, not for redistribution. The definitive version was published in Antarctic Science 23 (2011): 34-42, doi:10.1017/S0954102010000593.
    Description: Cycling of deep-water silicon (Si) within the Southern Ocean, and its transport into other ocean basins, may be an important player in the uptake of atmospheric carbon, and global climate. Recent work has shown that the Si isotope (denoted by δ29Si or δ30Si) composition of deep-sea sponges reflects the availability of dissolved Si during growth, and is a potential proxy for past deep and intermediate water silicic acid concentrations. As with any geochemical tool, it is essential to ensure analytical precision and accuracy, and consistency between methodologies and laboratories. Analytical bias may exist between laboratories, and sponge material may have matrix effects leading to offsets between samples and standards. Here, we report an interlaboratory evaluation of Si isotopes in Antarctic and subAntarctic sponges. We review independent methods for measuring Si isotopes in sponge spicules. Our results show that separate subsamples of non-homogenised sponges measured by three methods yield isotopic values within analytical error for over 80% of specimens. The relationship between δ29Si and δ30Si in sponges is consistent with kinetic fractionation during biomineralisation. Sponge Si isotope analyses show potential as palaeoceaongraphic archives, and we suggest Southern Ocean sponge material would form a useful additional reference standard for future spicule analyses.
    Description: Cruise NBP0805 was funded by NSF Office of Polar Programs (OPP) Antarctic Sciences (grant number ANT-0636787). KH is funded by a Doherty Postdoctoral Scholarship at WHOI, and the work has also been funded by the Natural Environment Research Council (NERC) grant NE/F005296/1 and an Antarctic Science Bursary.
    Keywords: Biogeochemistry ; Porifera ; Nutrient ; Calibration ; Silicic acid
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 10
    Publication Date: 2022-05-26
    Description: © The Author(s), 2012. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Geochimica et Cosmochimica Acta 96 (2012): 174-192, doi:10.1016/j.gca.2012.08.002.
    Description: Despite a growing body of work that uses diatom δ30Si to reconstruct past changes in silicic acid utilisation, few studies have focused on calibrating core top data with modern oceanographic conditions. In this study, a microfiltration technique is used to divide Southern Ocean core top silica into narrow size ranges, separating components such as radiolaria, sponge spicules and clay minerals from diatoms. Silicon isotope analysis of these components demonstrates that inclusion of small amounts of non-diatom material can significantly offset the measured from the true diatom δ30Si. Once the correct size fraction is selected (generally 2–20 μm), diatom δ30Si shows a strong negative correlation with surface water silicic acid concentration (R2 = 0.92), highly supportive of the qualitative use of diatom δ30Si as a proxy for silicic acid utilisation. The core top diatom δ30Si matches well with mixed layer filtered diatom δ30Si from published in situ studies, suggesting little to no effect of either dissolution on export through the water column, or early diagenesis, on diatom δ30Si in sediments from the Southern Ocean. However, the core top diatom δ30Si shows a poor fit to simple Rayleigh or steady state models of the Southern Ocean when a single source term is used. The data can instead be described by these models only when variations in the initial conditions of upwelled silicic acid concentration and δ30Si are taken into account, a caveat which may introduce some error into quantitative reconstructions of past silicic acid utilisation from diatom δ30Si.
    Description: The Oxford isotope geochemistry lab is supported by an ERC grant to Halliday. This work was carried out as part of Natural Environmental Research Council (NERC) Grant NE/F005296/1, and Antarctic Peninsula core tops collected thanks to the Antarctic Funding Initiative Grant AFI4-02.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Format: application/msword
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