Published

2022-09-08

Climatic and hydrological changes in Gaoyou Lake, eastern China over the last millennium, inferred from pollen and grain size records

Detección de los cambios climáticos e hidrológicos en el último milenio del lago Gaoyou, al oriente de China, a través del polen, tamaño del grano y registros litológicos

DOI:

https://doi.org/10.15446/esrj.v26n2.68391

Keywords:

Paleoclimate；Lake sediment；Last millennium；Grain size ；Pollen ；Gaoyou Lake (en)
paleoclimate; sedimentos de lagos; último milenio; polen; lago Gaoyou. (es)

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Authors

  • Shuheng Li Northwest University, China
  • Wei Guo Department of Environmental Sciences and Technology, Xi’an Jiaotong University
  • Na Gao School of Urban and Environmental Sciences, Northwest University, Xi’an 710127, China

Numerous lakes formed in the area where the Huai River and the Grand Canal converged during the historical period, and it played a substantial role in the evolution of the regional environment. Gaoyou Lake is a vital detention reservoir in the lower reaches of the Huai River. Variations in hydrology and basin-wide environmental changes were analyzed based on pollen assemblages, grain size data, and lithology from sediment cores collected at Gaoyou Lake. This study focused on variations in the hydrodynamic processes of Gaoyou Lake that were responses to changes in climate, regio- nal hydrological events, and human activity. The high percentages of pollen from terrestrial herbs and results of prin- cipal component analysis suggested that the environment of eastern China was arid from AD 900 to 1300 and that this corresponded to the dry conditions of the Medieval Climate Anomaly. The subsequent period between AD 1300 and 1650 was more humid, as revealed by an increase in aquatic pollen and a decrease in grain size. A rise in xerophytic herb taxa (particularly Artemisia and Chenopodioideae) indicated that the climate became arid again from AD 1650 to 1850, during the Little Ice Age. The modern period (AD 1850 onwards) was characterized by another increase in moisture, as reflected by a decrease in herb pollen and grain sizes. The shifts in the course of the Yellow River in AD 1194 and AD 1855 were recorded by abrupt changes in lithology, sediment characteristics, and the percentages of alien pollen taxa. Intense human impacts were demonstrated by cereal-type pollen and an increase in pollen of other cultivated plants such as Cruciferae and Poaceae. This study provides a foundation for further analysis of the dynamic mechanisms between lake development, climate change, and the effects of significant river changes.

Varios lagos se formaron en el área donde convergen el río Huai y el Gran Canal durante el período histórico, lo que jue- ga un rol importante en la evolución del entorno regional. El lago Gaoyou es un importante reservorio en los segmentos bajos del río Huai. En este trabajo se analizaron las variaciones en hidrología y los cambios ambientales de la cuenca amplia con base en los grupos de polen, tamaño del grano y litología de las muestras de sedimento recolectadas en el lago Gaoyou. Este trabajo se enfoca en las variaciones de los procesos hidrodinámicos del lago Gaoyou que fueron las respuestas a los cambios del clima, los eventos hidrológicos regionales, y la actividad humana. Los altos porcentajes de polen de las hierbas terrestres y los resultados de los análisis de componentes principales sugieren que el ambiente de la China oriental fue árido entre los años 900 a 1300 DC y esto se corresponde con las condiciones de sequía del Período Cálido Medieval. El período subsecuente entre 1300 y 1650 fue más húmedo, como se revela por un incremento en el polen acuático y en el decrecimiento del tamaño del grano. Un incremento en el taxón de las hierbas xerófitas (espe- cialmente Artemisias y Chenopodioideaes) indica que el clima se tornó arido de nuevo entre 1650 y 1850, durante la Pequeña Edad de Hielo. El período moderno (de 1850 en adelante) se caracterizó por otro incremento en la húmedad, como se refleja en un decrecimiento del polen de hierbas y en los tamaños del grano. Los cambios en el curso del Río Amarillo entre 1194 y 1855 se registran por las variaciones abruptas en la litología, las características de los sedimentos y los porcentajes en los taxones de polen alienígena. Los impactos humanos intensos se demuestran con la ocurrencia de polen tipo cereal y un incremento en el polen de otras plantas cultivadas como las cruciferas y las poáceas. Este estudio presenta una base para análisis posteriores de los mecanismos dinámicos entre el desarrollo del lago, el cambio climático y los efectos de los mayores cambios de los ríos.

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How to Cite

APA

Li, S., Guo, W. and Gao, N. (2022). Climatic and hydrological changes in Gaoyou Lake, eastern China over the last millennium, inferred from pollen and grain size records. Earth Sciences Research Journal, 26(2), 173–182. https://doi.org/10.15446/esrj.v26n2.68391

ACM

[1]
Li, S., Guo, W. and Gao, N. 2022. Climatic and hydrological changes in Gaoyou Lake, eastern China over the last millennium, inferred from pollen and grain size records. Earth Sciences Research Journal. 26, 2 (Sep. 2022), 173–182. DOI:https://doi.org/10.15446/esrj.v26n2.68391.

ACS

(1)
Li, S.; Guo, W.; Gao, N. Climatic and hydrological changes in Gaoyou Lake, eastern China over the last millennium, inferred from pollen and grain size records. Earth sci. res. j. 2022, 26, 173-182.

ABNT

LI, S.; GUO, W.; GAO, N. Climatic and hydrological changes in Gaoyou Lake, eastern China over the last millennium, inferred from pollen and grain size records. Earth Sciences Research Journal, [S. l.], v. 26, n. 2, p. 173–182, 2022. DOI: 10.15446/esrj.v26n2.68391. Disponível em: https://revistas.unal.edu.co/index.php/esrj/article/view/68391. Acesso em: 28 mar. 2025.

Chicago

Li, Shuheng, Wei Guo, and Na Gao. 2022. “Climatic and hydrological changes in Gaoyou Lake, eastern China over the last millennium, inferred from pollen and grain size records”. Earth Sciences Research Journal 26 (2):173-82. https://doi.org/10.15446/esrj.v26n2.68391.

Harvard

Li, S., Guo, W. and Gao, N. (2022) “Climatic and hydrological changes in Gaoyou Lake, eastern China over the last millennium, inferred from pollen and grain size records”, Earth Sciences Research Journal, 26(2), pp. 173–182. doi: 10.15446/esrj.v26n2.68391.

IEEE

[1]
S. Li, W. Guo, and N. Gao, “Climatic and hydrological changes in Gaoyou Lake, eastern China over the last millennium, inferred from pollen and grain size records”, Earth sci. res. j., vol. 26, no. 2, pp. 173–182, Sep. 2022.

MLA

Li, S., W. Guo, and N. Gao. “Climatic and hydrological changes in Gaoyou Lake, eastern China over the last millennium, inferred from pollen and grain size records”. Earth Sciences Research Journal, vol. 26, no. 2, Sept. 2022, pp. 173-82, doi:10.15446/esrj.v26n2.68391.

Turabian

Li, Shuheng, Wei Guo, and Na Gao. “Climatic and hydrological changes in Gaoyou Lake, eastern China over the last millennium, inferred from pollen and grain size records”. Earth Sciences Research Journal 26, no. 2 (September 8, 2022): 173–182. Accessed March 28, 2025. https://revistas.unal.edu.co/index.php/esrj/article/view/68391.

Vancouver

1.
Li S, Guo W, Gao N. Climatic and hydrological changes in Gaoyou Lake, eastern China over the last millennium, inferred from pollen and grain size records. Earth sci. res. j. [Internet]. 2022 Sep. 8 [cited 2025 Mar. 28];26(2):173-82. Available from: https://revistas.unal.edu.co/index.php/esrj/article/view/68391

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