Abstract
Organic matter (OM) is a key component of lake sediments, affecting carbon, nutrient and trace metal cycling at local and global scales. Yet little is known about long-term (millennial) changes in OM composition due to the inherent chemical complexity arising from multiple OM sources and from secondary transformations. In this study we explore how the molecular composition of OM changes throughout the Holocene in two adjacent boreal lakes in central Sweden, and compare molecular-level information with conventional OM variables, including total carbon (TC), total nitrogen (TN), C:N ratios, δ13C and δ15N. To characterize the molecular OM composition, we employed a new method based on pyrolysis-gas chromatography/mass spectrometry (Py-GC/MS), which yields semi-quantitative data on >100 organic compounds of different origin and degradation status. We identify large changes in OM composition after deglaciation (c. 8500 ± 500 B.C.), associated with early landscape development, and during the most recent 40–50 years, driven by degradation processes. With molecular-level information we can also distinguish between natural landscape development and human catchment disturbance during the last 1700 years. Our study demonstrates that characterization of the molecular OM composition by the high-throughput Py-GC/MS method is an efficient complement to conventional OM variables for identification and understanding of past OM dynamics in lake-sediment records. Holocene changes observed for pyrolytic compounds and compound classes known for having different reactivity indicate the need for further paleo-reconstruction of the molecular OM composition to better understand both past and future OM dynamics and associated environmental changes.
Original language | English |
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Pages (from-to) | 1423-1438 |
Number of pages | 17 |
Journal | Journal of geophysical research-Biogeosciences |
Volume | 122 |
Issue number | 6 |
Early online date | 15 Jun 2017 |
DOIs | |
Publication status | Published - 11 Jul 2017 |
Bibliographical note
This research was supported by grants from the Swedish Research Council (dnr. 2014-5219) and from the Umeå University research environment ‘The environment’s chemistry’. We would like to thank Umeå Plant Science Center for making the Py-GC/MS available to us, and Alexandra Rouillard and one anonymous reviewer for constructive comments on the manuscript. All data presented in the figures in the main manuscript can be found in the supporting information. Raw data will be provided upon request from thecorresponding authors.
Keywords
- organic matter composition
- lake sediment
- Holocene
- Pyrolysis-GC/MS
- carbon
- stable isotopes
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Timothy Mighall
- School of Geosciences, Geography & Environment - Personal Chair
- The North
Person: Academic