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Giulia Gatti, Fiorenza Roghi, Valeriano Parravicini, Monica Montefalcone, Alessio
         Rovere, Carla Morri, Andrea Peirano, Eva Salvati, Marco Firpo,
                      Giancarlo Albertelli, Carlo Nike Bianchi



                       VII Incontro dei Dottorandi in Ecologia
                            e Scienze dei Sistemi Acquatici
                            Roma, 27 Febbraio - 1 Marzo 2012
MARINE COASTAL ECOSYSTEMS ARE DEEPLY
 INFLUENCED BY GLOBAL CHANGE

COMBINATION OF NATURAL AND ANTHROPOGENIC
 EFFECTS


 HOW CAN WE EVALUATE LONG TERM VARIATION
        OF BENTHIC COMMUNITIES?



           HISTORICAL DATA-SETS
PUNTA MESCO (CINQUE TERRE, LIGURIAN SEA)

ROCKY REEF SESSILE ASSEMBLAGES
20 m TO 45 m DEPTH
GROSS MORPHOLOGY OF THE PUNTA MESCO SHOAL
WHY PUNTA MESCO?
•PRIORITY HABITAT UNDER EC DIRECTIVE (‘REEF’)
•DESCRIPTIVE STUDIES SINCE 1937
•DISCONTINUOUS QUANTITATIVE DATA SINCE 1961
 THANKS TO UNDERWATER PHOTOGRAPHIC SURVEYS



    POSSIBILITY OF RECONSTRUCTING
   EVOLUTION OVER THE LAST 50 YEARS
YEAR                           AUTHOR(S)                                INFORMATION

1937                 Tortonese and Faraggiana 1937                       qualitative
                                                                          qualitative
1959                            Rossi 1961
                                                                        (anthozoans)
1961                           Rossi 1965a                               qualitative

1961                           Rossi 1965b                               quantitative

1975                          Parmasub 1978                              qualitative

1978                       Andreoli et al. 1979                          qualitative

1985                         Relini et al. 1986                          qualitative
                                                                         quantitative
1988                     Peirano and Tunesi 1989
                                                                        (anthozoans)
                                                                          qualitative
1989                         Tunesi et al. 1989
                                                                        (anthozoans)
1990                   Peirano and Sassarini 1990                        quantitative

1996   Peirano et al. 2000, Bianchi et al. 2001, Morri & Bianchi 2001    quantitative

2008                         PRESENT WORK                                quantitative
Savalia savaglia
   80s       DISAPPEARS, Eunicella singularis
             AND Paramuricea clavata
             DIMINISH

             DRASTIC CHANGE IN THE
   90s       UNDERSTOREY ASSEMBLAGES
             (SPONGES, BRYOZOANS)


1999, 2003   DIE-OFFS OF Paramuricea clavata
FEGINA (MONTEROSSO AL MARE)
1990           2008
              1961




                                        1996




MEAN AIR TEMPERATURE IN GENOA.
THE   VARIABLE LINE REPRESENTS MEAN ANNUAL VALUES, THE
CONTINUOUS LINE REPRESENTS THE GENERAL TREND.
1961
LUCIA ROSSI, GIANNI ROGHI
 PHOTOGRAPHIC SURVEYS
 (SQUARED FRAMES OF 1 m2)




FIRST QUANTITATIVE WORK     Gianni Roghi (1927-1967)
                               www.gianniroghi.it
• COVER INDEX FROM 0.5 TO 5 FOR EACH SPECIES
• 8 DIFFERENT ASSEMBLAGES BASED ON SLOPE AND
 DEPTH OF THE SUBSTRATE
SUCCESSIVE SURVEYS
 PEIRANO AND SASSARINI 1990

 ENEA (MARINE ENVIRONMENT RESEARCH
  CENTRE, LA SPEZIA) AND UNIVERSITY OF ROME
 1996
 UNIVERSITY OF GENOA 2008
6 OUT OF THE 8 ASSEMBLAGES DESCRIBED
             BY L. ROSSI
      3 PHOTOS FOR EACH SURVEY
!!!
THE DATA-SETS DIFFER FOR:
PHOTOGRAPHIC TECHNIQUE
 TAXONOMIC RESOLUTION
    SAMPLING DESIGN
RECONSTRUCTING THE
HISTORY OF EACH
ASSEMBLAGE...

 PCO   ANALYSIS

 FREQUENCY-RANK   DIAGRAMS
INCREASING
SEDIMENTATION
INCREASING
              SEDIMENTATION




     RISING
TEMPERATURE
REDUCTION OF THE
UNDERSTOREY
REDUCTION OF THE
                   UNDERSTOREY




LITTLE INFLUENCE
OF TEMPERATURE
ASSEMBLAGES MAINLY INFLUENCED BY
        THE INCREASE IN:

          WATER COLUMN TURBIDITY
       SEDIMENTATION RATE (TURF)
      SURFACE WATER TEMPERATURE


      MAJOR CHANGES IN THE 1990S
 (ARRIVAL OF Womersleyella setacea?)
SURFACE WATER WARMING AND
LOWERING OF THE THERMOCLINE


CAUSED
           MASS MORTALITY OF
           Paramuricea clavata

FAVOURED   APPEARANCE OF
           Caulerpa racemosa
STRESSED NATIVE SPECIES FAIL TO RESIST
  THE SPREAD OF ALIEN SPECIES




Caulerpa racemosa OVERGROWTHS THE NATIVE CORAL
Cladocora caespitosa AT PUNTA MESCO, SEPTEMBER 2008
THE ROCKY REEF ECOSYSTEM OF PUNTA
   MESCO SHOAL IS STILL EVOLVING



 THIS PRECIOUS LONG TERM
STUDY HAS TO BE CONTINUED!
THANK YOU

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Decadal evolution of a temperate rocky reef ecosystem under the influence of climate change

  • 1. Giulia Gatti, Fiorenza Roghi, Valeriano Parravicini, Monica Montefalcone, Alessio Rovere, Carla Morri, Andrea Peirano, Eva Salvati, Marco Firpo, Giancarlo Albertelli, Carlo Nike Bianchi VII Incontro dei Dottorandi in Ecologia e Scienze dei Sistemi Acquatici Roma, 27 Febbraio - 1 Marzo 2012
  • 2. MARINE COASTAL ECOSYSTEMS ARE DEEPLY INFLUENCED BY GLOBAL CHANGE COMBINATION OF NATURAL AND ANTHROPOGENIC EFFECTS HOW CAN WE EVALUATE LONG TERM VARIATION OF BENTHIC COMMUNITIES? HISTORICAL DATA-SETS
  • 3. PUNTA MESCO (CINQUE TERRE, LIGURIAN SEA) ROCKY REEF SESSILE ASSEMBLAGES 20 m TO 45 m DEPTH
  • 4.
  • 5. GROSS MORPHOLOGY OF THE PUNTA MESCO SHOAL
  • 6. WHY PUNTA MESCO? •PRIORITY HABITAT UNDER EC DIRECTIVE (‘REEF’) •DESCRIPTIVE STUDIES SINCE 1937 •DISCONTINUOUS QUANTITATIVE DATA SINCE 1961 THANKS TO UNDERWATER PHOTOGRAPHIC SURVEYS POSSIBILITY OF RECONSTRUCTING EVOLUTION OVER THE LAST 50 YEARS
  • 7. YEAR AUTHOR(S) INFORMATION 1937 Tortonese and Faraggiana 1937 qualitative qualitative 1959 Rossi 1961 (anthozoans) 1961 Rossi 1965a qualitative 1961 Rossi 1965b quantitative 1975 Parmasub 1978 qualitative 1978 Andreoli et al. 1979 qualitative 1985 Relini et al. 1986 qualitative quantitative 1988 Peirano and Tunesi 1989 (anthozoans) qualitative 1989 Tunesi et al. 1989 (anthozoans) 1990 Peirano and Sassarini 1990 quantitative 1996 Peirano et al. 2000, Bianchi et al. 2001, Morri & Bianchi 2001 quantitative 2008 PRESENT WORK quantitative
  • 8. Savalia savaglia 80s DISAPPEARS, Eunicella singularis AND Paramuricea clavata DIMINISH DRASTIC CHANGE IN THE 90s UNDERSTOREY ASSEMBLAGES (SPONGES, BRYOZOANS) 1999, 2003 DIE-OFFS OF Paramuricea clavata
  • 10. 1990 2008 1961 1996 MEAN AIR TEMPERATURE IN GENOA. THE VARIABLE LINE REPRESENTS MEAN ANNUAL VALUES, THE CONTINUOUS LINE REPRESENTS THE GENERAL TREND.
  • 11. 1961 LUCIA ROSSI, GIANNI ROGHI PHOTOGRAPHIC SURVEYS (SQUARED FRAMES OF 1 m2) FIRST QUANTITATIVE WORK Gianni Roghi (1927-1967) www.gianniroghi.it
  • 12. • COVER INDEX FROM 0.5 TO 5 FOR EACH SPECIES • 8 DIFFERENT ASSEMBLAGES BASED ON SLOPE AND DEPTH OF THE SUBSTRATE
  • 13. SUCCESSIVE SURVEYS  PEIRANO AND SASSARINI 1990  ENEA (MARINE ENVIRONMENT RESEARCH CENTRE, LA SPEZIA) AND UNIVERSITY OF ROME 1996  UNIVERSITY OF GENOA 2008
  • 14. 6 OUT OF THE 8 ASSEMBLAGES DESCRIBED BY L. ROSSI 3 PHOTOS FOR EACH SURVEY
  • 15. !!! THE DATA-SETS DIFFER FOR: PHOTOGRAPHIC TECHNIQUE TAXONOMIC RESOLUTION SAMPLING DESIGN
  • 16. RECONSTRUCTING THE HISTORY OF EACH ASSEMBLAGE...  PCO ANALYSIS  FREQUENCY-RANK DIAGRAMS
  • 18. INCREASING SEDIMENTATION RISING TEMPERATURE
  • 19.
  • 20.
  • 21.
  • 22.
  • 24. REDUCTION OF THE UNDERSTOREY LITTLE INFLUENCE OF TEMPERATURE
  • 25.
  • 26.
  • 27.
  • 28. ASSEMBLAGES MAINLY INFLUENCED BY THE INCREASE IN:  WATER COLUMN TURBIDITY  SEDIMENTATION RATE (TURF)  SURFACE WATER TEMPERATURE MAJOR CHANGES IN THE 1990S (ARRIVAL OF Womersleyella setacea?)
  • 29. SURFACE WATER WARMING AND LOWERING OF THE THERMOCLINE CAUSED MASS MORTALITY OF Paramuricea clavata FAVOURED APPEARANCE OF Caulerpa racemosa
  • 30. STRESSED NATIVE SPECIES FAIL TO RESIST THE SPREAD OF ALIEN SPECIES Caulerpa racemosa OVERGROWTHS THE NATIVE CORAL Cladocora caespitosa AT PUNTA MESCO, SEPTEMBER 2008
  • 31. THE ROCKY REEF ECOSYSTEM OF PUNTA MESCO SHOAL IS STILL EVOLVING THIS PRECIOUS LONG TERM STUDY HAS TO BE CONTINUED!