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BIOGEOCHEMISTRY OF THE ANAXIMENES SEAMOUNT
   (E.MEDITERRANEAN): MOLECULAR EVIDENCE FOR A
“SEAMOUNT EFFECT” IN PARTICULATE ORGANIC MATTER
                    QUALITY?


             Kostas Kiriakoulakis1,2 and George Wolff2
 1Liverpool John Moores University, School of Natural Sciences and
 Psychology, K.Kiriakoulakis@ljmu.ac.uk
 2   University of Liverpool, School of Environmental Sciences,, wolff@liverpool.ac.uk
Global estimates of seamounts
33452 seamounts (4.7%) and 138412 knolls (16.3%) globally (Yesson et al. 2011)




    seamounts




                                                             (Yesson et al. 2011)



      knolls
Observations and theories
• Less than 300 have been studied in some degree
• “Hotspots” of marine life and diversity
– Large pelagic (fish stocks and zooplankton) and
  benthic biomass (e.g. cold water corals etc.)
– ‘Island’ theory: Endemism – not much evidence
– ‘Oasis’ theory: productive in an otherwise
  nutrient depleted ocean – open question
Complex physics

Upwelling ⇒               Closed circulation :Taylor columns
High primary production   (e.g. White et al. 2007)
                          • Particle retention?
                          • Zooplankton migration blockage?
Effect on carbon cycling?
                    Mather 2009

36°N
CD171
2005




DOC




        Downwelling of DOC above topography
Is there a “Seamount effect” in the ocean?

• Enhanced local primary/secondary productivity, trapping of
  advected particles?
• Temporal variability?
   • Primary production is seasonal
   • Taylor columns are (thought to be) transient features
• Nutritional status of the ecosystems?
   • Quality of organic matter
   • Can be assessed by molecular studies (e.g. lipid biomarkers)
PUFAs: markers of POM quality
          Lipids of known biological origin

              Docosahexaenoic acid (DHA) - Dinoflagellates




               Eicosapentaenoic acid (EPA) - Diatoms




PUFAs: Poly-Unsaturated Fatty Acids
  • Essential fatty acids
  • Very labile (1/2 life ~ < 1 week) and energy rich
• Markers of (high) OM quality
Quality of POM: link with zooplankton?
POC               Data from Kiriakoulakis et al. 2009         PUFAs
µg L-1                               North
                       top                                    % lipids
 25       South                                         Far    60
 20                                                            50
                                                               40
 15
                                                               30
 10                                                            20
  5                                                            10
                                                                0
  0

                     Zooplankton biomass Spring 2003
  day




                      Seine
                    seamount
  night




                      Seine
                    seamount

                       Martin and Christiansen 2009
Anaximenes Seamount
•   Within very oligotrophic, warm (even at depth) waters
•   Part of Anaximander Mountains complex
•   Elongated summit at ~700 m, eastern trough at ~1600 m
•   Comparison with a reference site (Northern Rhodes Basin ~4300 m)
•   Suspended particles (best sampled with SAPS)
                                                         In situ pump (SAPS)




          Map is modified from ten Veen et al. (2004).
Sampling scheme
                           Between
Northern
                           Anaximenes
Rhodes        Anaximenes
                           and
Basin
                           Anaxagoras
Control (1)   Summit (3)   Trough (2)
                                        50m euphotic layer
                                        150m below euphotic layer




                                        Close to bottom (10-20mab)
Particulate Organic C and N
                                       POC                                                                              PN
                                            µg L-1 water                                                                    µg L-1 water
                             0    5    10       15         20     25       30                                0     1        2         3     4         5
                        10                                                                              10
Sampling Depth (m)




                                                                                Sampling Depth (m)
                       100                                                                             100




                      1000                                                                            1000



                                  control       summit 1        summit 2                                         control        summit 1   summit 2
                                  summit 3      trough 1        trouph 2                                         summit 3       trough 1   trouph 2
                     10000                                                                           10000


                             •   Variable POC and PN concentrations close to surface
                             •   Lowest POC at reference site (one sample only)
                             •   Exponential decrease of POC with depth but not for PN
                             •   Unclear interpretation for PN: relation to atmospheric N input
                                 and P limitation in the region?
Particulate Lipids




Modified OM
markers
(zooplankton
+ faecal
pellets)




          •    Lowest [lipids] at reference site
          •    Fatty acids (and PUFAs) almost disappear below euphotic layer
          •    Simultaneously heterotrophic signal increases at depth
          •    Lower quality suspended POM at depth
Particulate Lipids




• Statistically significant compositional differences between
  surface (50 m) and deeper waters
• Except surface sample at control site (Northern Rhodes Basin):
  similar composition to deeper waters = not good OM quality

            Seamount effect?
Seamount effect?
• Can’t say with only one sample (although 50 variables!) but intriguing
• Denda and Christiansen 2011 did not find ‘seamount effect’ in
  zooplankton (same cruise)
• They suggest that larger-scale structures of cyclones and
  anticyclones, dominate circulation in the area




                                                        AMC: Asia Minor Current;
                                                        MMJ: Mid-Mediterranean Jet




                          Denda and Christiansen 2011



                      The jury is still out
Thank you for listening!



• Many thanks to:
• The Crew and Master of RV Meteor 71/1
• CENSEAM for funding this research

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Biogeochemistry of the Anaximenes Seamount (E. Mediterranean): molecular evidence for a "Seamount effect" in particulate organic matter quality? Kiriakoulakis, K.

  • 1. BIOGEOCHEMISTRY OF THE ANAXIMENES SEAMOUNT (E.MEDITERRANEAN): MOLECULAR EVIDENCE FOR A “SEAMOUNT EFFECT” IN PARTICULATE ORGANIC MATTER QUALITY? Kostas Kiriakoulakis1,2 and George Wolff2 1Liverpool John Moores University, School of Natural Sciences and Psychology, K.Kiriakoulakis@ljmu.ac.uk 2 University of Liverpool, School of Environmental Sciences,, wolff@liverpool.ac.uk
  • 2. Global estimates of seamounts 33452 seamounts (4.7%) and 138412 knolls (16.3%) globally (Yesson et al. 2011) seamounts (Yesson et al. 2011) knolls
  • 3. Observations and theories • Less than 300 have been studied in some degree • “Hotspots” of marine life and diversity – Large pelagic (fish stocks and zooplankton) and benthic biomass (e.g. cold water corals etc.) – ‘Island’ theory: Endemism – not much evidence – ‘Oasis’ theory: productive in an otherwise nutrient depleted ocean – open question
  • 4. Complex physics Upwelling ⇒ Closed circulation :Taylor columns High primary production (e.g. White et al. 2007) • Particle retention? • Zooplankton migration blockage?
  • 5. Effect on carbon cycling? Mather 2009 36°N CD171 2005 DOC Downwelling of DOC above topography
  • 6. Is there a “Seamount effect” in the ocean? • Enhanced local primary/secondary productivity, trapping of advected particles? • Temporal variability? • Primary production is seasonal • Taylor columns are (thought to be) transient features • Nutritional status of the ecosystems? • Quality of organic matter • Can be assessed by molecular studies (e.g. lipid biomarkers)
  • 7. PUFAs: markers of POM quality Lipids of known biological origin Docosahexaenoic acid (DHA) - Dinoflagellates Eicosapentaenoic acid (EPA) - Diatoms PUFAs: Poly-Unsaturated Fatty Acids • Essential fatty acids • Very labile (1/2 life ~ < 1 week) and energy rich • Markers of (high) OM quality
  • 8. Quality of POM: link with zooplankton? POC Data from Kiriakoulakis et al. 2009 PUFAs µg L-1 North top % lipids 25 South Far 60 20 50 40 15 30 10 20 5 10 0 0 Zooplankton biomass Spring 2003 day Seine seamount night Seine seamount Martin and Christiansen 2009
  • 9. Anaximenes Seamount • Within very oligotrophic, warm (even at depth) waters • Part of Anaximander Mountains complex • Elongated summit at ~700 m, eastern trough at ~1600 m • Comparison with a reference site (Northern Rhodes Basin ~4300 m) • Suspended particles (best sampled with SAPS) In situ pump (SAPS) Map is modified from ten Veen et al. (2004).
  • 10. Sampling scheme Between Northern Anaximenes Rhodes Anaximenes and Basin Anaxagoras Control (1) Summit (3) Trough (2) 50m euphotic layer 150m below euphotic layer Close to bottom (10-20mab)
  • 11. Particulate Organic C and N POC PN µg L-1 water µg L-1 water 0 5 10 15 20 25 30 0 1 2 3 4 5 10 10 Sampling Depth (m) Sampling Depth (m) 100 100 1000 1000 control summit 1 summit 2 control summit 1 summit 2 summit 3 trough 1 trouph 2 summit 3 trough 1 trouph 2 10000 10000 • Variable POC and PN concentrations close to surface • Lowest POC at reference site (one sample only) • Exponential decrease of POC with depth but not for PN • Unclear interpretation for PN: relation to atmospheric N input and P limitation in the region?
  • 12. Particulate Lipids Modified OM markers (zooplankton + faecal pellets) • Lowest [lipids] at reference site • Fatty acids (and PUFAs) almost disappear below euphotic layer • Simultaneously heterotrophic signal increases at depth • Lower quality suspended POM at depth
  • 13. Particulate Lipids • Statistically significant compositional differences between surface (50 m) and deeper waters • Except surface sample at control site (Northern Rhodes Basin): similar composition to deeper waters = not good OM quality Seamount effect?
  • 14. Seamount effect? • Can’t say with only one sample (although 50 variables!) but intriguing • Denda and Christiansen 2011 did not find ‘seamount effect’ in zooplankton (same cruise) • They suggest that larger-scale structures of cyclones and anticyclones, dominate circulation in the area AMC: Asia Minor Current; MMJ: Mid-Mediterranean Jet Denda and Christiansen 2011 The jury is still out
  • 15. Thank you for listening! • Many thanks to: • The Crew and Master of RV Meteor 71/1 • CENSEAM for funding this research