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Winterfeld, Maria; Laepple, Thomas; Mollenhauer, Gesine (2015): Particulate organic matter (POM) of samples from the Lena River delta. PANGAEA, https://doi.org/10.1594/PANGAEA.855439, Supplement to: Winterfeld, M et al. (2015): Characterization of particulate organic matter in the Lena River delta and adjacent nearshore zone, NE Siberia - Part I: Radiocarbon inventories. Biogeosciences, 12(12), 3769-3788, https://doi.org/10.5194/bg-12-3769-2015

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Abstract:
Particulate organic matter (POM) derived from permafrost soils and transported by the Lena River represents a quantitatively important terrestrial carbon pool exported to Laptev Sea sediments (next to POM derived from coastal erosion). Its fate in a future warming Arctic, i.e., its remobilization and remineralization after permafrost thawing as well as its transport pathways to and sequestration in marine sediments, is currently under debate. We present one of the first radiocarbon (14C) data sets for surface water POM within the Lena Delta sampled in the summers of 2009 - 2010 and spring 2011 (n = 30 samples). The bulk D14C values varied from -55 to -391 per mil translating into 14C ages of 395 to 3920 years BP. We further estimated the fraction of soil-derived POM to our samples based on (1) particulate organic carbon to particulate nitrogen ratios (POC : PN) and (2) on the stable carbon isotope (d13C) composition of our samples. Assuming that this phytoplankton POM has a modern 14C concentration, we inferred the 14C concentrations of the soil-derived POM fractions. The results ranged from -322 to -884 per mil (i.e., 3060 to 17 250 14C years BP) for the POC : PN-based scenario and from -261 to -944 per mil (i.e., 2370 to 23 100 14C years BP) for the d13C-based scenario. Despite the limitations of our approach, the estimated D14C values of the soil-derived POM fractions seem to reflect the heterogeneous 14C concentrations of the Lena River catchment soils covering a range from Holocene to Pleistocene ages better than the bulk POM D14C values. We further used a dual-carbon-isotope three-end-member mixing model to distinguish between POM contributions from Holocene soils and Pleistocene Ice Complex (IC) deposits to our soil-derived POM fraction. IC contributions are comparatively low (mean of 0.14) compared to Holocene soils (mean of 0.32) and riverine phytoplankton (mean of 0.55), which could be explained with the restricted spatial distribution of IC deposits within the Lena catchment. Based on our newly calculated soil-derived POM D14C values, we propose an isotopic range for the riverine soil-derived POM end member with D14C of -495 ± 153 per mil deduced from our d13C-based binary mixing model and d13C of -26.6 ± 1 per mil deduced from our data of Lena Delta soils and literature values. These estimates can help to improve the dual-carbon-isotope simulations used to quantify contributions from riverine soil POM, Pleistocene IC POM from coastal erosion, and marine POM in Siberian shelf sediments.
Coverage:
Median Latitude: 70.984168 * Median Longitude: 126.438706 * South-bound Latitude: 56.370000 * West-bound Longitude: 72.830000 * North-bound Latitude: 73.525800 * East-bound Longitude: -148.740000
Date/Time Start: 2009-08-14T00:00:00 * Date/Time End: 2011-07-02T00:00:00
Size:
7 datasets

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Datasets listed in this publication series

  1. Winterfeld, M; Laepple, T; Mollenhauer, G (2015): (Table 3) Stable carbon isotope and radiocarbon composition of Lena Delta first terrace soil profiles and surface water particulate organic matter (2009–2011). https://doi.org/10.1594/PANGAEA.855102
  2. Winterfeld, M; Laepple, T; Mollenhauer, G (2015): (Table 5) Soil fractions calculated based on POC : PN ratios and δ¹³C values and associated estimated 14C concentrations of the soil-derived POM fraction. https://doi.org/10.1594/PANGAEA.855438
  3. Winterfeld, M; Laepple, T; Mollenhauer, G (2015): (Table S1) Compilation of OC:TN soil end-member source data from the literature. https://doi.org/10.1594/PANGAEA.855288
  4. Winterfeld, M; Laepple, T; Mollenhauer, G (2015): (Table S2) Compilation of δ¹³C source data from the literature and this study for the soil end - member. https://doi.org/10.1594/PANGAEA.855353
  5. Winterfeld, M; Laepple, T; Mollenhauer, G (2015): (Table S3) Compilation of D14C source data from the literature and this study for the Holocene soil end - member. https://doi.org/10.1594/PANGAEA.855431
  6. Winterfeld, M; Laepple, T; Mollenhauer, G (2015): (Table S4) Total suspended matter concentrations (TSM), particulate organic carbon contents (POC) as well as atomic particulate organic carbon to total particulate nitrogen ratios (POC:PN) of individual Lena Delta surface water samples from 2009 - 2011. https://doi.org/10.1594/PANGAEA.855172
  7. Winterfeld, M; Laepple, T; Mollenhauer, G (2015): (Table S5) Results of the dual - carbon isotope (δ¹³C, D14C) mixing model for the three organic matter fractions contributing to the Lena Delta suspended matter samples from 2009 - 2011. https://doi.org/10.1594/PANGAEA.855249