oa Fate of Terrigenous Nitrogen in East Siberian Arctic Shelf Sediments

References

1. Batista, et al.
   (2014) Compound specific amino acid δ15N in marine sediments: A new approach for studies of the marine nitrogen cycle', Geochimica et Cosmochimica Acta, 142, 553–569.
   [Google Scholar]
2. Bröder, et al.
   (2016) Fate of terrigenous organic matter across the Laptev Sea from the mouth of the Lena River to the deep sea of the Arctic interior, Biogeosciences, 13, 5003–5019.
   [Google Scholar]
3. Carstens, et al.
   (2013) Amino acid nitrogen isotopic composition patterns in lacustrine sedimenting matter, Geochimica et Cosmochimica Acta.121, 328–338.
   [Google Scholar]
4. Karlsson, et al.
   (2016) Different sources and degradation state of dissolved, particulate, and sedimentary organic matter along the Eurasian Arctic coastal margin, Global Biogeochemical Cycles, 898–919
   [Google Scholar]
5. Sánchez-García, et al.
   (2011) Inventories and behavior of particulate organic carbon in the Laptev and East Siberian seas, Global Biogeochemical Cycles, 25
   [Google Scholar]
6. Sparkes, et al.
   (2016) Macromolecular composition of terrestrial and marine organic matter in sediments across the East Siberian Arctic Shelf, Cryosphere, 10, 2485–2500.
   [Google Scholar]
7. Tesi, et al.
   (2016) Matrix association effects on hydrodynamic sorting and degradation of terrestrial organic matter during cross-shelf transport in the Laptev and East Siberian shelf seas, Journal of Geophysical Research: Biogeosciences, 121, 731–752.
   [Google Scholar]
8. Vonk, et al.
   (2012) Activation of old carbon by erosion of coastal and subsea permafrost in Arctic Siberia, Nature, 489, 137–140.
   [Google Scholar]
9. Vonk, J. E. and Gustafsson, Ö
   . (2013) Permafrost-carbon complexities', Nature Geoscience, 6, 675–676.
   [Google Scholar]