Abstract

Lakes are a crucial component of the global carbon and nitrogen cycle. As a trend of enhanced human activities and climate change, the mechanisms of burial remain poorly understood. In this study, diverse biogeochemical techniques were applied to analyze the temporal variation of organic carbon and nitrogen burial rates in Chaohu Lake. The results showed that burial rates have ranged from 9.39 to 35.87 g C m−2 yr−1 for carbon and from 1.66 to 5.67 g N m−2 yr−1 for nitrogen since the 1860s. The average rates were 19.6 g C m−2 yr−1 and 3.14 g N m−2 yr−1 after the 1970s, which were significantly higher than the rate before the 1970s, showing an increasing trend. The decrease of C/N ratios as well as organic matter δ13C values indicates that the major organic matter source in sediment has been algal production since the 1970s. The increase of δ15N values indicated that the promotion in productivity was stimulated by nutrient input from sewage and agricultural runoff. The burial rates of organic carbon and nitrogen were significantly positively related to socio-economics and temperature, indicating that Chaohu Lake will become an increasing carbon and nitrogen pool under conditions of enhanced human activities and intensive precipitation.

Highlights

  • Lakes are hotspots for the carbon (C) and nitrogen (N) biogeochemical cycle due to their production, transformation, and transportation [1,2,3,4]

  • We investigated the temporal variability of carbon and nitrogen burial rates from two sediment cores in Chaohu Lake

  • Geochemical proxies in sediments were used to analyze the temporal changes of organic carbon and nitrogen burial rates as well as the driving factors over the last 150 years in Chaohu Lake

Read more

Summary

Introduction

Lakes are hotspots for the carbon (C) and nitrogen (N) biogeochemical cycle due to their production, transformation, and transportation [1,2,3,4]. Many studies have revealed that organic carbon burial rates in the sediment of lakes have increased in the last 100–150 years [7,9,13,14]. Human activities and climate change have been recognized as the primary driving factors that have a significant influence on the carbon and nitrogen cycle in lakes [15,16,17,18,19]. Increasing temperature can stimulate algal growth and lead to the increase of primary production [23], but it can accelerate decomposition and decrease the burial efficiency of organic matter after sedimentation [15]. Precipitation has no direct influence on the burial rates in lakes

Objectives
Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call