Abstract

Abstract. This paper documents the picoplankton community's response to changes in oceanographic conditions in the period between October 2011 and September 2012 at two stations belonging to the South Adriatic Pit (SAP). The recorded data include the community's abundance, composition, prokaryotic production rates and bacterial metabolic capacity. The sampling period included an intense sea cooling with formation of exceptional, record-breaking dense water. We documented an especially intense winter convection episode that completely diluted the core of Levantine intermediate waters (LIW) in a large area encompassing the SAP's center and its margin. During this convection event the whole picoplankton community had significantly higher abundances with a recorded picoeukaryotic peak at the SAP margin. In the post-convection phase in March, prokaryotic heterotrophic production strongly increased in the entire SAP area (up to 50 times; 456.8 nM C day−1). An autotrophic biomass increase (up to 5 times; 4.86 μg L−1) and a disruption of a close correspondence between prokaryotic heterotrophic biomass production and cell replication rates were observed only in the center of the SAP, which was not under the influence of LIW. At the SAP's margin such an effect was attenuated by LIW, since the waters affected by LIW were characterized by decreased concentrations of dissolved inorganic nitrogen, decreased autotrophic biomasses, and by increased bacterial biomass production balanced with cell replication rates as well as by the domination of Synechococcus among autotrophic picoplankton. The metabolic capacity was lowest in spring when autotrophic biomass largely increased, while the highest levels found in the pre-convection phase (October 2011) suggest that the system was more oligotrophic before than after the convection event. Furthermore, we showed that metabolic capacity is a trait of bacterial community independent of environmental conditions and tightly linked to cell replication and substrate availability. In contrast, the bacterial community composition appears to be strongly influenced by physico-chemical characteristics of waters (e.g., temperature and nutrients) and environmental forcing (e.g., convection and LIW). Our results showed that the two oceanographic phenomena of the Southern Adriatic, strongly relevant for the total production of the Adriatic Sea, winter convection and LIW intrusion, regulate the changes in picoplankton community structure and activities.

Highlights

  • The Southern Adriatic includes the deepest part of the Adriatic basin, the South Adriatic Pit (SAP ∼ 1243 m)

  • Our results showed that winter convection events and Levantine intermediate waters (LIW) have different roles in the distribution and function of the picoplankton community

  • The winter convection induced a strong increase in prokaryotic heterotrophic production in March, an enormous increase in the autotrophic biomass, followed by a disruption of a close correspondence between Leu and TdR incorporation rates (L / T < 1) occurred only in the center of the SAP beyond the reach of LIW

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Summary

Introduction

The Southern Adriatic includes the deepest part of the Adriatic basin, the South Adriatic Pit (SAP ∼ 1243 m). The area above the pit is characterized by a quasi-permanent cyclonic gyre, the South Adriatic Gyre (Gacicet al., 1997). Due to convection processes, dense water (Adriatic Dense Water, AdDW) is formed as a mixture of fresher Adriatic and more saline Ionian waters. The convection rarely reaches the bottom layers of the pit, which are mainly under influence of colder and denser water formed in the Northern Adriatic (North Adriatic Dense water; NAdDW; Gacicand Civitarese, 2012). The East Adriatic Current, which partly belongs to the South Adriatic Gyre, brings waters from the Ionian Sea into the Adriatic (Artegiani et al, 1997)

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