Response to review
نویسنده
چکیده
We thank Dr Severmann for her time invested in reviewing this manuscript. Dr Severmann's comments are centered around four aspects of our manuscript: 1) the general information on the Baltic Sea redox state and the overall redox profile; 2) processes related to the formation of Fesulfides and the Fe source in the basin's euxinic bottom layer; 3) the controls of Fe(II)-oxidation rates in the zone of the FeSPM maximum; and 4) the origin of low δ56Fe of suspended Fe at 100 m. Dr Severmann suggests an alternative interpretation with diffusive Fe efflux from shallow (shelf) oxic sediments surrounding the basin, subsequent oxidation, and suspended transport to the basin to form an Fe-rich particle maximum, based on her previous publication (Severmann et al. 2008). Additional comments relate to details of a reference on Fe isotope fractionation in hydrothermal plumes cited by us.
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تاریخ انتشار 2012