Seasonal nutrient dynamics in the P depleted Eastern Mediterranean Sea

Tal Ben Ezra, Michael D. Krom, Anat Tsemel, Ilana Berman-Frank, Barak Herut, Yoav Lehahn, Eyal Rahav, Tom Reich, T. Frede Thingstad, Daniel Sher

Research output: Contribution to journalArticlepeer-review

Abstract

The Eastern Mediterranean Sea (EMS), is ultra-oligotrophic with unusual anti-estuarine circulation. It is P depleted and the limited enrichment studies which have been carried out, suggest seasonal changes in nutrient limitation. In this study high sensitivity dissolved nutrients (and associated parameters) were determined monthly over an annual cycle at a pelagic location in the SE Levantine basin. Nitrate & Nitrite (Nox) concentrations were high (300–500 nM) during the winter mixing period and enabled a concurrent phytoplankton increase in which larger picoeukaryotes and eukaryotes were dominant. After the thermal stratification of the water column commenced, Nox decreased through early summer transition period to low values (generally 50 nM or less) in the late summer. DIP remained at low nM concentrations the entire year while DOP decreased from 40 nM in winter to 30 nM in summer. Prochlorococcus, the smallest picocyanobacteria, that does not typically utilize nitrate, dominated during the summer when both Nox and DIP concentrations were lowest. Ammonium concentrations were low (10–100 nM) with no systematic changes with season or depth. As a result, the DIN:DIP ratios were high (20–825) in winter and low (2–66) in summer, showing that these ratios vary seasonally. The dynamics of nutrient availability combined with the temporal changes in total chlorophyll and the altered dominance of the predominant phytoplankton species (i.e. nitrate-metabolizing Synechococcus during winter versus the smaller Prochlorococcus abundant in summer), leads to our hypothesis that the seasonal change in DIN:DIP indicates a switch from P limitation in winter during the annual phytoplankton increase to N&P or even N limitation in summer. Export Production (172 mmol N m−2 y−1) determined from the calculated loss of Nox from the photic zone, was similar to previous estimates in the EMS. Our results in terms of seasonally changing nutrient dynamics and resulting productivity confirm that the EMS has many of the characteristics found in P starved ocean gyre systems.

Original languageEnglish
Article number103607
JournalDeep-Sea Research Part I: Oceanographic Research Papers
Volume176
DOIs
StatePublished - Oct 2021

Bibliographical note

Funding Information:
We thank the captains and crew of the R/V Mediterranean Explorer and R/V Bat Galim, Oshra Yosef, Elad Rachmilovitz, Or Bialik, and Guy Sisma-Ventura for help with the sampling. The SoMMoS (THEMO) ship-time was funded by the Leon H. Charney School of Marine Sciences with help from EcoOcean and IOLR. This study was supported by grant RGP0020/2016 from the Human Frontiers Science Program (to DS) and by grant number 1635070/2016532 from the NSF-BSF program in Oceanography (NSFOCE-BSF, to DS). The dust leaching experiments were funded by ISF grant (# 1211/17 to ER and BH). We thank two anonymous reviewers for their insightful comments and suggestions. This study was first submitted on the week that TBE became engaged and resubmitted after review the day after she announced her wedding day.

Publisher Copyright:
© 2021

Keywords

  • Eastern Mediterranean Sea
  • Export production
  • Ocean gyre
  • P depleted
  • Seasonal nutrient limitation

ASJC Scopus subject areas

  • Oceanography
  • Aquatic Science

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