| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6429845 | Earth and Planetary Science Letters | 2013 | 13 Pages |
•Salinity proxies Ba/Ca and δOWATER18 show diverging spatial patterns.•Orinoco influence is best tracked by Ba/Ca.•δOWATER18 is dominated by local precipitation balance.•Ba/Ca is strongly influenced by desorption processes at estuarine settings.
Past river run-off is an important measure for the continental hydrological cycle and the assessment of freshwater input into the ocean. However, paleosalinity reconstructions applying different proxies in parallel often show offsets between the respective methods. Here, we compare the established foraminiferal Ba/Ca and δOWATER18 salinity proxies for their capability to record the highly seasonal Orinoco freshwater plume in the eastern Caribbean. For this purpose we obtained a data set comprising Ba/Ca and δOWATER18 determined on multiple species of planktonic foraminifera from core tops distributed around the Orinoco River mouth.Our findings indicate that interpretations based on either proxy could lead to different conclusions. In particular, Ba/Ca and δOWATER18 diverge in their spatial distribution due to different governing factors. Apparently, the Orinoco freshwater plume is best tracked by Ba/Ca ratios of G. ruber (pink and sensu lato morphotypes), while δOWATER18 based on the same species is more related to the local precipitation-evaporation balance overprinting the riverine freshwater contribution. Other shallow dwelling species (G. sacculifer, O. universa) show a muted response to the freshwater discharge, most likely due to their ecological and habitat preferences. Extremely high Ba/Ca ratios recorded by G. ruber are attributed to Ba2+-desorption from suspended matter derived from the Orinoco.Samples taken most proximal to the freshwater source do not show pronounced Ba/Ca or δOWATER18 anomalies. Here, the suspension loaded freshwater lid developing during maximum discharge suppresses foraminiferal populations. Both proxies are therefore biased towards dry season conditions at these sites, when surface salinity is only minimally reduced.
