Biogenic-silica accumulation in the Ross Sea and the importance of Antarctic continental-shelf deposits in the marine silica budget
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Cited by (83)
Glaciomarine sediment deposition on the continental slope and rise of the central Ross Sea since the Last Glacial Maximum
2022, Marine GeologyCitation Excerpt :Conversely, the residual glaciomarine sediments that lie at the top of the banks were mostly deposited via the reworking of surface sediments by the strong bottom current (e.g., Prothro et al., 2018). The total organic carbon (TOC) content of the surface sediments on the present-day continental shelf of the Ross Sea is between ~0.2% and ~2.0% (Ledford-Hoffman et al., 1986; Frignani et al., 1998; Langone et al., 1998; McKay et al., 2008; Tolotti et al., 2013), while that of the continental slope/margin areas range between ~0.1% and ~0.5% (Melis et al., 2021; Khim et al., 2021). The total nitrogen (TN) content is ~0.1% and the biogenic opal content varies from ~10% to >30%.
Biological productivity and glaciomarine sedimentation in the Central Basin of the northwestern Ross Sea since the last glacial maximum
2021, Polar ScienceCitation Excerpt :The Ross Sea continental shelf including its polynyas is a biological ‘hot spot’ of increased productivity marked by the highest phytoplankton concentration (10–40 mg Chl a m−3) in the Southern Ocean (e.g., Arrigo et al., 2000). The biogenic silica production in the water column is a primary factor used to determine present-day patterns of biosiliceous sediment accumulation on the continental shelf of the Ross Sea, with the southwestern area being the most productive (~41% of biogenic silica; Ledford-Hoffman et al., 1986). According to Frignani et al. (1998), the present-day sedimentation on the continental shelf of the Ross Sea is dominated by biosiliceous mud and ooze ranging from 0.5 to 32.7% (13.5% on average) of biogenic silica and from 0.2 to 2.8% (0.88% on average) of TOC.
The Global Marine Silica Budget: Sources and Sinks
2019, Encyclopedia of Ocean Sciences, Third Edition: Volume 1-5The global marine silica budget: Sources and sinks
2019, Encyclopedia of Ocean SciencesPolar Phytoplankton
2013, Polar Oceanography: Chemistry, Biology, and Geology