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Smoking guns and volcanic ash: the importance of sparse tephras in Greenland ice cores

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F20%3A00525290" target="_blank" >RIV/86652079:_____/20:00525290 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216224:14310/20:00116702

  • Result on the web

    <a href="https://polarresearch.net/index.php/polar/article/view/3511/11020" target="_blank" >https://polarresearch.net/index.php/polar/article/view/3511/11020</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.33265/polar.v39.3511" target="_blank" >10.33265/polar.v39.3511</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Smoking guns and volcanic ash: the importance of sparse tephras in Greenland ice cores

  • Original language description

    Volcanic ash (fine-grained tephra) within Greenland ice cores can complement the understanding of past volcanism and its environmental and societal impacts. The presence of ash in sparse concentrations in the ice raises questions about whether such material represents primary ashfall in Greenland or resuspended (remobilized) material from continental areas. In this article, we investigate this issue by examining tephra content in quasi-annual samples from two Greenland ice cores during a period of ca. 20 years and considering their relationships with sulphur and particulate data from the same cores. We focus on the interval 815-835 CE as it encompasses a phase (818-822 CE) of heightened volcanogenic sulphur previously ascribed to an eruption of Katla, Iceland. We find that tephra is a frequent but not continuous feature within the ice, unlike similarly sized particulate matter. A solitary ash shard whose major element geochemistry is consistent with Katla corroborates the attribution of the 822 +/- 1 CE sulphur peak to this source, clearly showing that a single shard can signify primary ashfall. Other tephras are present in similarly low abundances, but their geochemistries are less certainly attributable to specific sources. Although these tephra shards tend to coincide with elevated sulphur and fine (<10 mu m) particulates, they are not associated with increased coarse (>10 mu m) particle concentrations that might be expected if the shards had been transported by dust storms. We conclude that the sparse shards derive from primary ashfall, and we argue that low tephra concentrations should not be dismissed as insignificant.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10502 - Oceanography

Result continuities

  • Project

    <a href="/en/project/EF16_019%2F0000797" target="_blank" >EF16_019/0000797: SustES - Adaptation strategies for sustainable ecosystem services and food security under adverse environmental conditions</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2020

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Polar Research

  • ISSN

    0800-0395

  • e-ISSN

  • Volume of the periodical

    39

  • Issue of the periodical within the volume

    JUN

  • Country of publishing house

    NO - NORWAY

  • Number of pages

    11

  • Pages from-to

    3511

  • UT code for WoS article

    000539032900001

  • EID of the result in the Scopus database

    2-s2.0-85088263274