Effects of physical constraints on the lability of POM during summer in the Ross Sea

• Published in: Journal of Marine Systems
• Main Authors: MISIC, CRISTINA, Covazzi Harriague, Anabella, Mangoni, Olga, Aulicino, Giuseppe, Castagno, Pasquale, Cotroneo, Yuri
• Other Authors: Misic, Cristina
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier B.V. 2017
• Subjects: Antarctica; Biochemical composition; Particulate organic matter; Physical structure; Phytoplankton bioma; Ross Sea; Oceanography; Ecology; Evolution; Behavior and Systematic; Aquatic Science; Antarc*; Ice Shelf; Ross Ice Shelf
• Online Access: http://hdl.handle.net/11567/858884; https://doi.org/10.1016/j.jmarsys.2016.06.012

The 0–200 m surface layer of the Ross Sea was studied during summer 2014 to investigate the lability of the particulate organic matter (POM) in response to physical parameters. With the use of satellite information, we selected three zones, characterised by different physical setting: a northern offshore area, crossing the summer-polynya area of the Ross Sea (hereafter called ROME 1), a more coastal area next to the Terra Nova Bay polynya (ROME 2); a southern offshore area, towards the Ross Ice Shelf (ROME 3). Ice-maps showed that the seasonal ice retreat had already occurred in early December for most of the stations. Statistical analysis of the quantitative and qualitative characteristics of the POM pointed to significant differences between the stations, especially in the upper mixed layer (UML). A comparison with previous studies showed that the localised pulses of POM accumulation in the UML were similar to those recorded at the highly productive marginal ice zones, providing notable trophic support to the ecosystem. The UML, although rather thin and easily subjected to alterations, confirmed its pivotal role in the ecosystem dynamics. A POM quality favourable to consumers was highlighted at several stations in ROME 1 and ROME 3. Reduced trophic support was, instead, found in ROME 2. Limited POM consumption where deep-water formation takes place would increase the POM role in the transfer of C to the depths.