Zell, Claudia; Kim, Jung-Hyun; Dorhout, Denise J C; Baas, Marianne; Sinninghe Damsté, Jaap S (2015): Organic geochemistry of SPM and surface sediments along the Portuguese continental margin [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.881067,

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Supplement to: Zell, C et al. (2015): Sources and distributions of branched tetraether lipids and crenarchaeol along the Portuguese continental margin: Implications for the BIT index. Continental Shelf Research, 96, 34-44, https://doi.org/10.1016/j.csr.2015.01.006

The branched vs. isoprenoid tetraethers (BIT) index, which is based on the relative abundance of non-isoprenoidal, so-called branched glycerol dialkyl glycerol tetraethers (brGDGTs) versus a structurally related isoprenoid GDGT "crenarchaeol", has been used to trace soil organic carbon (OC) from the continent to the ocean. However, it has been found in some locations that the BIT index can be primarily influenced by crenarchaeol concentrations and brGDGT production in fresh water rather than by soil-derived brGDGT concentrations. This may hamper the application of this proxy as an indicator for the input of soil OC. Here we examined the concentration and distribution of brGDGTs as well as variations in the BIT index in marine surface sediments from five transects (Douro, Mondego, Estremadura, Tagus, and Sado) along the southern Portuguese continental margin and in marine suspended particulate matter (SPM) from the Douro and Tagus transects. Higher BIT values and brGDGT concentrations (normalized to OC content) were found close to the river mouths and coast than in deep offshore sites. This clearly indicated the continental input of brGDGTs and revealed that, at least in this setting, the BIT index was primarily influenced by the delivery of brGDGTs from the rivers. However, the BIT index was also, to a minor extent, influenced by crenarchaeol concentrations. This shows that the brGDGT concentration may provide a more straightforward indication of continental OC input than the BIT index. BrGDGT concentrations and distributions in sediments and SPM close to the rivers were similar to those of SPM in the Tagus River. This indicates that degradation processes in the estuaries had no significant effect on the riverine brGDGTs. Therefore, brGDGTs should be a good indicator for the rigid OC fraction transported from the continent to the ocean. Our results also indicate that there are multiple sources of brGDGTs in the marine environment, which complicates the use of the brGDGT distribution as an indicator for terrestrial vs. marine produced brGDGTs.