XRF, XRD, grainsize and total organic carbon in core Konar Sandal peat bog, SE Iran

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Hauptverfasser: Safaierad, Reza, Mohtadi, Mahyar, Zolitschka, Bernd, Yokoyama, Yusuke, Vogt, Christoph, Schefuß, Enno
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2020
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author Safaierad, Reza
Mohtadi, Mahyar
Zolitschka, Bernd
Yokoyama, Yusuke
Vogt, Christoph
Schefuß, Enno
author_facet Safaierad, Reza
Mohtadi, Mahyar
Zolitschka, Bernd
Yokoyama, Yusuke
Vogt, Christoph
Schefuß, Enno
collection Datos científicos de ciencias marinas y ambientales
contents Rapid North Atlantic cooling events during the last deglaciation caused atmospheric reorganizations on global and regional scales. Their impact on Asian climate has been investigated for monsoonal domains, but remains largely unknown in westerly wind-dominated semi-arid regions. Here we generate a dust record from southeastern Iran spanning the period 19-7 cal. ka BP. We find a direct link between frequent occurrences of dust plumes originating from the Arabian Peninsula and North Africa, and rapid southward shifts of the westerlies associated with changes of the winter stationary waves during Heinrich Stadial 1, the Younger Dryas, the Preboreal Oscillation and the 8.2 ka event. Dust input rises and falls abruptly at the transitions into and out of these cooling events, which we attribute to changes in the ocean circulation strength and modulated by the North Atlantic winter sea-ice cover. Our findings reveal that waxing and waning of North American ice sheets have a stronger influence than those of European ice sheets on the winter climate over West Asia.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_918548
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle XRF, XRD, grainsize and total organic carbon in core Konar Sandal peat bog, SE Iran
Safaierad, Reza
Mohtadi, Mahyar
Zolitschka, Bernd
Yokoyama, Yusuke
Vogt, Christoph
Schefuß, Enno
Atmospheric dust; North Atlantic cooling; Northern Hemisphere Westerlies; sea-ice; West Asia
Rapid North Atlantic cooling events during the last deglaciation caused atmospheric reorganizations on global and regional scales. Their impact on Asian climate has been investigated for monsoonal domains, but remains largely unknown in westerly wind-dominated semi-arid regions. Here we generate a dust record from southeastern Iran spanning the period 19-7 cal. ka BP. We find a direct link between frequent occurrences of dust plumes originating from the Arabian Peninsula and North Africa, and rapid southward shifts of the westerlies associated with changes of the winter stationary waves during Heinrich Stadial 1, the Younger Dryas, the Preboreal Oscillation and the 8.2 ka event. Dust input rises and falls abruptly at the transitions into and out of these cooling events, which we attribute to changes in the ocean circulation strength and modulated by the North Atlantic winter sea-ice cover. Our findings reveal that waxing and waning of North American ice sheets have a stronger influence than those of European ice sheets on the winter climate over West Asia.
title XRF, XRD, grainsize and total organic carbon in core Konar Sandal peat bog, SE Iran
topic Atmospheric dust; North Atlantic cooling; Northern Hemisphere Westerlies; sea-ice; West Asia
url https://doi.org/10.1594/PANGAEA.918548