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. 2020 Aug 31;378(2181):20190366. doi: 10.1098/rsta.2019.0366

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© 2020 The Authors.

Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/4.0/, which permits unrestricted use, provided the original author and source are credited.

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Figure 4. — Partitioning of organic carbon between the dissolved and microbial pools for integrated water column of the Fram Strait during summer (left) and autumn (right). Phytoplankton release semi-labile DOM components like dCCHO and dHAA that can further partition into TEP and CSP. The decline in semi-labile DOC triggers a decrease in bacterial incorporation of semi-labile DOC (%SL-DOC d⁻¹) and the bacterial community composition from summer to autumn. HNA bacteria are coloured in red and LNA bacteria in black. PAR data are a monthly estimate from MODIS-Aqua satellite of a 4-km spatial resolution between 1–31 July 2018 for summer and 1–30 September 2018 within $78 - 80^{\circ} N$ and −2°W–13°E from https://giovanni.gsfc.nasa.gov. (Online version in colour.)