Middle Pleniglacial pedogenesis on the northwestern edge of the Carpathian basin: A multidisciplinary investigation of the Bíňa pedo-sedimentary section, SW Slovakia

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61388980%3A_____%2F17%3A00480373" target="_blank" >RIV/61388980:_____/17:00480373 - isvavai.cz</a>

Alternative codes found

RIV/67985831:_____/17:00480373 RIV/00216224:14310/17:00095144 RIV/62156489:43410/17:43911958 RIV/00216208:11310/17:10364509 RIV/00025798:_____/17:00000101

Result on the web

<a href="http://dx.doi.org/10.1016/j.palaeo.2017.09.017" target="_blank" >http://dx.doi.org/10.1016/j.palaeo.2017.09.017</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.palaeo.2017.09.017" target="_blank" >10.1016/j.palaeo.2017.09.017</a>

Result language

angličtina

Original language name

Middle Pleniglacial pedogenesis on the northwestern edge of the Carpathian basin: A multidisciplinary investigation of the Bíňa pedo-sedimentary section, SW Slovakia

Original language description

The Middle Pleniglacial on the northern hemisphere is characterized by millennial scale, frequent, and high amplitude environmental climatic shifts. This study tries to fill this gap in our knowledge through studying a pedo-sedimentary record from Bíňa, a site situated in a relatively poorly investigated area on the northwestern edge of the Carpathian Basin. We investigated a 12-m-high and more than 500-m-wide outcrop along the Hron River, where a well-structured sequence of fluvio-lacustrine sediments, paleosols, and loess is preserved. The paleoenvironmental development within the studied area is presented and discussed on the basis of soil micromorphology, rock-magnetic and geochemical measurements, grain size analyses, and a malacological record accomplished by luminescence dating. Based on the OSL dating of the central profile, the sequence provides a high resolution record of the time period 60–20 ka (MIS 3–MIS 2). The most developed paleosol horizons (Phaeozem and two Bw horizons of Gleyic Cambisols) were dated to the early stage of the MIS 3 (60–50 ka) and correlated with the Greenland interstadials GI-17/16, GI-14/13 and/or GI-12 (the northwestern European interstadials Oerel, Glinde and Moershoofd). Although soil development benefited from the specific local settings, we suggest that the recorded paleosols can also be related to the interregional climate differences of the Carpathian Basin: within the northerly located pericarpathian zones, a moister climate predominated during the last Pleniglacial, in contrast to the drier continental areas to the South. Thus, a sharp climatic transition existed separating a semi-arid steppe region from a climatic zone under the persistent influence of Atlantic air masses.

Czech name

—

Czech description

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Type

J_imp - Article in a specialist periodical, which is included in the Web of Science database

CEP classification

—

OECD FORD branch

10505 - Geology

Project

<a href="/en/project/GAP504%2F11%2F0429" target="_blank" >GAP504/11/0429: Environmental gradients, vegetation dynamics and landscape changes in the West Carpathians from the Late Glacial up to present times</a><br>

Continuities

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year

2017

Confidentiality

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

Name of the periodical

Palaeogeography, Palaeoclimatology, Palaeoecology

ISSN

0031-0182

e-ISSN

—

Volume of the periodical

487

Issue of the periodical within the volume

1 December 2017

Country of publishing house

NL - THE KINGDOM OF THE NETHERLANDS

Number of pages

19

Pages from-to

321-339

UT code for WoS article

000414881100027

EID of the result in the Scopus database

2-s2.0-85030645036