Towards quantitative reconstruction of past monsoon precipitation based on tetraether membrane lipids in Chinese loess
<p>Variations in the oxygen isotope composition (<span class="inline-formula"><i>δ</i><sup>18</sup></span>O) of cave speleothems and numerous proxy records from loess–paleosol sequences have revealed past variations in East Asian monsoon (EAM) inte...
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| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2025-02-01
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| Series: | Climate of the Past |
| Online Access: | https://cp.copernicus.org/articles/21/343/2025/cp-21-343-2025.pdf |
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| Summary: | <p>Variations in the oxygen isotope composition (<span class="inline-formula"><i>δ</i><sup>18</sup></span>O) of cave speleothems and numerous proxy records from loess–paleosol sequences have revealed past variations in East Asian monsoon (EAM) intensity. However, challenges persist in reconstructing precipitation changes quantitatively. Here, we use the positive relationship between the degree of cyclization (DC) of branched glycerol dialkyl glycerol tetraethers (brGDGTs) in modern surface soils from the Chinese Loess Plateau (CLP) and mean annual precipitation (MAP) to quantify past monsoon precipitation changes on the CLP. We present a new <span class="inline-formula">∼</span> 130 000-year-long DC-based MAP record for the Yuanbao section on the western edge of the CLP, which closely tracks the orbital- and millennial-scale variations in available records of both speleothem <span class="inline-formula"><i>δ</i><sup>18</sup></span>O and the hydrogen isotope composition of plant waxes (<span class="inline-formula"><i>δ</i><sup>2</sup></span>H<span class="inline-formula"><sub>wax</sub></span>) from the same section. Combing our new data with existing brGDGT records from other CLP sites reveals a spatial gradient in MAP that is most pronounced during glacials, when the western CLP experiences more arid conditions and receives up to <span class="inline-formula">∼</span> 250 mm less precipitation than in the southeast, whereas MAP is <span class="inline-formula">∼</span> 850 mm across the CLP during the Holocene optimum. Furthermore, the DC records show that precipitation amount on the CLP varies at both the precession scale and the obliquity scale, as opposed to the primarily precession-scale variations in speleothem <span class="inline-formula"><i>δ</i><sup>18</sup></span>O and <span class="inline-formula"><i>δ</i><sup>2</sup></span>H<span class="inline-formula"><sub>wax</sub></span> at Yuanbao and the 100 kyr cycle in other loess proxies, such as magnetic susceptibility, which rather indicates the relative intensity of the EAM. At the precession scale, the DC record is in phase with <span class="inline-formula"><i>δ</i><sup>2</sup></span>H<span class="inline-formula"><sub>wax</sub></span> from the same section and the speleothem <span class="inline-formula"><i>δ</i><sup>18</sup></span>O record, which supports the hypothesis that monsoon precipitation is driven by Northern Hemisphere summer insolation.</p> |
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| ISSN: | 1814-9324 1814-9332 |