Influence of atmospheric deposition and climate change on lake eutrophication and environment in Lake Buir (eastern Mongolia) over the last century

• Enhanced river input since the 1940s was caused by increasing rainfall. • Hypolimnion was oxidized after the 1950s with enhanced river input. • Depletion of δ 15 N since the 1960s is due to agricultural activity in NE China. • Primary productivity resulted from climatic warming and atmospheric nutrient supply. • Atmospheric transport of pollutants from NE China began in the 1950s. Multiple proxies from a sediment core taken from the deepest part of Lake Buir in the eastern Mongolian Plateau, situated at the China–Mongolia border, were used in this study to investigate paleoenvironmental changes and climatic and anthropogenic factors that primarily control variability over the past 100 years. A typical upward-fining turbidite bed was found in 1947–1954 CE based on the combined age of excess 210 Pb and 137 Cs, which coincided with high annual precipitation. The median grain sizes of the mineral fraction and TS/TOC ratio indicate enhanced river inflow since the 1940s–1950s with increasing rainfall, leading to changes in the hypolimnion from anoxic to oxic conditions. The gradual increase in carbonate content suggests that regional warming since the 1960s has resulted in a decrease in dissolved CO 2 solubility and an increase in primary productivity in the epilimnion. The C/N molar ratio (8.3–12.0) and Suess-corrected δ 13 C TOC value (–24.9 ‰ to –22.0 ‰) indicate that the sedimentary organic matter mainly originated from algae and phytoplankton. The depletion of δ 15 N (6.5–5.4 ‰) with increasing TN content from the 1960s to the 2000s CE indicates enhanced atmospheric nutrient deposition from northeast China. These findings suggest that climate warming and anthropogenic loading have affected lake eutrophication. Furthermore, the depletion of δ 34 S values (9.1–7.0 ‰) with low TS contents since the 1960s CE indicates that atmospheric pollution of sulfates was transported with the rapid economic and industrial development in northeast China.

Authors

Institutions

Publication Details

Journal
CATENA
Published
2025-07-24
DOI
https://doi.org/10.1016/j.catena.2025.109297
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Influence of atmospheric deposition and climate change on lake eutrophication and environment in Lake Buir (eastern Mongolia) over the last century

Masayo Minami, Nagayoshi Katsuta, Niiden Ichinnorov, Ichiro Tayasu et al.
CATENA
Geology and Paleoclimatology Research
article

Influence of atmospheric deposition and climate change on lake eutrophication and environment in Lake Buir (eastern Mongolia) over the last century

Masayo Minami, Nagayoshi Katsuta, Niiden Ichinnorov, Ichiro Tayasu, Masakazu Niwa, Shinya Ochiai, Seiya Nagao, Davaadorj Davaasuren, Chikage Yoshimizu, Yuma Masuki, Yui Itayama, Minoru Uchida
article en

Abstract

• Enhanced river input since the 1940s was caused by increasing rainfall. • Hypolimnion was oxidized after the 1950s with enhanced river input. • Depletion of δ 15 N since the 1960s is due to agricultural activity in NE China. • Primary productivity resulted from climatic warming and atmospheric nutrient supply. • Atmospheric transport of pollutants from NE China began in the 1950s. Multiple proxies from a sediment core taken from the deepest part of Lake Buir in the eastern Mongolian Plateau, situated at the China–Mongolia border, were used in this study to investigate paleoenvironmental changes and climatic and anthropogenic factors that primarily control variability over the past 100 years. A typical upward-fining turbidite bed was found in 1947–1954 CE based on the combined age of excess 210 Pb and 137 Cs, which coincided with high annual precipitation. The median grain sizes of the mineral fraction and TS/TOC ratio indicate enhanced river inflow since the 1940s–1950s with increasing rainfall, leading to changes in the hypolimnion from anoxic to oxic conditions. The gradual increase in carbonate content suggests that regional warming since the 1960s has resulted in a decrease in dissolved CO 2 solubility and an increase in primary productivity in the epilimnion. The C/N molar ratio (8.3–12.0) and Suess-corrected δ 13 C TOC value (–24.9 ‰ to –22.0 ‰) indicate that the sedimentary organic matter mainly originated from algae and phytoplankton. The depletion of δ 15 N (6.5–5.4 ‰) with increasing TN content from the 1960s to the 2000s CE indicates enhanced atmospheric nutrient deposition from northeast China. These findings suggest that climate warming and anthropogenic loading have affected lake eutrophication. Furthermore, the depletion of δ 34 S values (9.1–7.0 ‰) with low TS contents since the 1960s CE indicates that atmospheric pollution of sulfates was transported with the rapid economic and industrial development in northeast China.

CATENAVol. 258
Japan Atomic Energy Agency (JP), Kanazawa Institute of Technology (JP), Mongolian Academy of Sciences (MN), Research Institute for Humanity and Nature (JP), Gifu University (JP), Nagoya University (JP), National University of Mongolia (MN)
Climate action
Openalex Percentile: Top 77%
Geology and Paleoclimatology Research
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.