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PAST-CLIMATE AS THE KEY TO
      UNDERSTAND THE FUTURE:
EXAMPLE FROM THE MEDITERRANEAN SEA




              VINCENZO PASCUCCI

   DIPARTIMENTO DI SCIENZE BOTANICHE, ECOLOGICHE E
                     GEOLOGICHE

                UNIVERSITA’ DI SASSARI
                    pascucci@uniss.it
Climate is changing?
         Which are the evidences?
         Is this a normal process?
Which have been recent past climatic changes?
       Which has been their impact?
          Can we say something?
PATHWAY…
-    ACTUALISM
     1. PRESENT CLIMAT
     2. CAUSES OF CLIMATE CHANGE
-    PAST
     1. GEOLOGICAL EVIDENCES OF
        CLIMATE CHANGES (SARDINIA)



    - CLIMATIC CHANGES OF THE LAST 125 KY
WHAT INFLUENCE THE CLIMATE OF THE EARTH:

      1. EARTH ORBIT AROUND THE SUN




                                  yearly
p
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                             e
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L                            t
T
    2. LATITUDE & ALTITUDE
3. GREAT OCEAN CONVEYOR BELT




          500 year to make the all circuit
WHAT INFLUENCE
CLIMATE CHANGES?



      ?
PLATE TECTONICS: long time
(millions of year = radical changes)
J
u
s
t

a
n

e
x
a
m
p
l
e
Orbital forces: short time
          (thousand of years = long lasting changes)
               today the Earth axis is 23°27’ inclined




Milankovitch
   cycles
Sun spots (hundreds to tens of years 500-11y)
  short time  climate changes = sensible
                 The change in the number of sunspots and in solar activity
                 (deduced from studies of carbon-14 concentrations in the wood of
                 tree rings and of beryllium-10 in ice cores) suggests that there
                 have been various exceptional periods of solar weakness during
                 the last millennium, namely, the Wolf (around 1300), Spoerer
                 (around 1500), Maunder (between 1645 and 1715) and Dalton
                 (1800-1830) periods.
                 These low points were most likely preceded by a period of
                 maximum solar activity, the Medieval Solar Maximum (between
                 1100 and 1250) (Jirikowic, 1994). According to some authors, a
                 similar maximum, the Contemporary Solar Maximum, is
                 occurring right now and is caused by a rise in the magnetic
                 activity of the solar corona during the 20th century (Lockwood,
                 1999). Basing their conclusions on models, some authors believe
                 that the solar activity of the last 70 years is the most intense of the
                 last 8,000 years (Solanki, 2004).




          2009
EARTH TEMPERATURE
ANTARTICA & GREENLAND

 ICE DRILLING PROJECT
EPICA & VOSTOK
(ice drilling project)
Main results are:
1. 8 glacial stages occurred during the last 740ky;
2. Interglacial past stages were as much warm as today;
3. Without human effect the present interglacial stage will last
   other 15ky;
4. CO2 concentration is the highest of the last 444ky
What about CO2?   Man has input more CO2
                  in the atmosphere in the
                  last 200y than the earth
                  system in 20ky… however
                  normally an increase of
                  CO2 into the system
                  precedes the beginning of
                  a glacial stage!!!!

                                   CO2
                                     T
Form Marine Isotopic Stages (MIS) to
Glacial and Interglacial stages: the last 300ky




 …. Isotopic stages MIS (even=caluroso; odds=frio)…simple!!!
The present interglacial stage: the last 11ky
1 warm every 1KY
Hannibal crosses the Alps with the elephants during the warm roman time
CLIMATE CHANGES OF THE LAST 1000 ANNI (ΔT = ±2 °C)
           important changes every 500y
THE LAST 30y
        ΔT = ± 0.774 °C
 last coldest years 2007-08-09
(the most sensible to humans)
TOOLS TO PERFORM
        PALEOCLIMATE STUDIES

•   Sedimentology  paleoenvironments
•   Stratigraphy  events order
•   Geomorphology  processes
•   Geochronology  time
•   Geochemistry  past atmosphere vs present (i.e. δ
    18/16O)
GEOLOGICAL ARCHIVES

• ANTARCTIC – GREENLAND (ICE)
• SARDINIA (ROCKS)
• ALPS (ROCKS & ICE)
ITALY  SARDINIA




Tectonically stable since Pliocene and in the Mid of the Mediterranean Sea
PAST GEOLOGICAL EVIDENCES OF CLIMATE CHANGES

         SARDINIA (ITALY) WEST COAST
             1. CAPO CACCIA CAVES
CAPO CACCIA SUBMERGED CAVES
CAPO CACCIA:
                 Partially submerged caves




sea level height reached about 125ky         + 4m
-7m




Cervo Sardo bones (deer extinguished around
40-30ky) are found into speleothems
-7m




Cervo Sardo bones (deer extinguished around
40-30ky) are found into speleothems
SEA LEVEL MARKERS AND DEER BONES INDICATE THAT
  CAPO CACCIA CAVES WHERE FLOODED BY SEA RISE
AROUND 125KY AND SUBSEQUENTLY EMERGED DUE TO
                SEA LEVEL FALL
WEST SARDINIA: 2. prograding ancient beaches




              SEDIMENTOLOGY
Detail: 2 relatively shallow water features
   today some meters above sea level



                                 2


                             1




ALGHERO
3



2
3



2       3


    2
3



    2            3


        23


             paleosoil




2
OSL ages

                           dunes
           3




               2



  Beaches and paleosoils
….moreover, tropical warm fauna in beach deposits




      STROMBUS
      BUBONIUS
Additional items: 3. tidal notch and dunes



                      4. Tidal notch(s) +2/4m




                  DUNES
Things to remember
• 1-4 features:
  – 1. fossiliferous/gravelly beach-shoreface (about
    125ky);
  – 2. silicoclastic beach (about 100ky);
  – 3. dunes (about 77-47 ky);
  – 4. tidal notch(s) partially covered by dunes (125-100
    ky);
PAST GEOLOGICAL EVIDENCES OF CLIMATE CHANGES
         SARDINIA (ITALY) EST COAST
         CALA GONONE (OROSEI GULF)
FEATURES INDICATING SEA LEVEL CHANGES




1. OLD NOTCH(S) (4/8 m asl)   MODERN NOTCH
2. Bue Marino Cave aeolian sediments
Medium-coarse grained                BUE 1 sample
bioclastic-rich sand, blown by the
wind into the cave from a marine
source (shelf/beach)


   BUE 5 sample




                                     BUE 2 sample
2. BUE MARINO CAVE SEDIMENTS: AGES




                                                                       BUE 1-5:
                                                                       80-100KY




AL: Speleothem samples, BUE: sediment samples
1: Jurassic limestone; 2: clastic sediments; 3: Lithophaga boreholes

OSL age Clastic sedimentary infill pre-date the notch referred at 125ky
FEATURES INDICATING CLIMATE CHANGES:
3. COARSE ALLUVIAL FAN (dated at 45ky OSL)
4. U-SHAPED VALLEY
5. PERIGLACIAL DEPOSITS “ÉBULIS ORDONNÉ” (18-20 ky)
now forming as cryo-clastic processes in the alps…
Things to remember
• 1-4 features:
  – 1. notch(s) (about 125ky) (sea level 4/6 m higher);
  – 2. cave sediments (aeolian) (about 100-80 ky) (input
    from an exposed sandy shelf during a relative sea
    level fall) ;
  – 3. coarse alluvial fan (about 40 ky);
  – 4. u-shaped valley (no age data);
  – 5. periglacial deposits (?18-20ky)
DATA INTERPRETATION
SEA LEVEL CHANGES
•   125ky (MIS 5) SL was at least +4m higher than today;
•   Since 80ky (end of MIS 5) sea level started to fall;
•   It reached the max of -130 bpsl about 20-18ky (MIS 2);
•   From 17-11ky sea level raised very fast (end MIS2);
•   We are in a highstand since 10ky (MIS 1) that should last for
    other about 15ky (without human influence)
TEMPERATURES AND CLIMATE
• 125-95 ky (MIS 5e) temp was at least +2/4 °C higher than today
  (subtropical climate and beaches formation). Apex of interglacial;
• 90-80ky (MIS 5a) temp cooled down (-3/4 °C lower than today,
  soils formation) (warm and humid). End of interglacial;
• 60-45ky (MIS 4) temp was -6/8 °C lower than today (cryoclast, u-
  shaped valley, exposure of shelf and dune formation) (cold and
  humiddry);
• 45-20ky (MIS 3-2) temp was -8/10 °C lower than today (wide
  cryoclast deposits and dune formation) (cold and very dry) Apex
  of glacial
C
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WHAT IS NEW?




1. SEA LEVEL CHANGES
SEA LEVEL FLUCTUATION DURING THE LAST
            INTERGLACIAL 130-80 KY
(5 SUBSTAGES ABOUT 10KY EACH SEPARATED BY A
STRONG EROSIONAL UNCONFORMITY; 2 ASL, 1 BSL)

              -bsl?   +1m   +4-6m
10 ky cycles may be referred to:
• Subprecessional (or sub Milankovitch cycles);

  – This short-time cycles can increase or decrease the
    temperature of some degrees;

  – At this moment it is not clear at all the origin of the
    short-time cycles because very often they are non
    linear and in cases they have been correlated to dust
    aerosols present in the atmosphere);

  – Solar irradiation variations;
Just an example: at the beginning of this interglacial,
in about 10 ky, the ice melted more or less completely.
  This fast event is related to solar radiation changes.
SEA LEVEL RISE AFTER THE LGM (18KY)




…1 m rise every 100 years up to about 7/6ky, after that sea level
         become more or less stable up to nowadays
…Y ITALIA SE CONVIRTIO’ EN BOTA!!!!




   20ky ago   In blu glaciers   6ky ago
Further studies
• Better characterize and explain the events occurred
  during the last interglacial;
• Amount of dust in the past atmosphere;
• Solar irradiation variations (long and short time);
• Human impact on climate;
• Better understanding of the Atlantic Multidecadal
  Oscillation (AMO) and if it existed also in the past (up
  to now not older than 150y)….

• More money to geological research because our
  future is written in the rocks and we only have
  to find the way to dig it out!!!
Last example… thermal fluctuation of the
      North Atlantic Ocean (AMO)




   last 100 years

 Mountain glaciers increase when AMO index is negative, and
 retreat when AMO is positive
Forecast based on past (BLU LINE)




Forecast based on global warming idea (RED LINE)
So what is going on?


        ?
We will fire in the hellish earth!!!
…or we will die iced!!!
A possibility is also that someone is joking with us using
climate change as personal purpose to become famous!!!
….but because
                                   everybody wants
                                   to speak about
                                   climate…

GLOBAL WARMING EXPERCTS!!!
                             I did it too!!!!!!!
GRACIas



          Le nuvole del cielo disegnano
          la mia strada del ritorno,ma
          solo tu raggio di sole sai quale
          sia davvero.
          Mi manca la tua luce, il tuo
          calore, la tua bocca, il tuo
          consiglio.
          Questa notte solo naufragherò
          tra i miei sogni dove spero di
          incontrare la mia stella.
          (Vince 07)

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Paleoclimate: past-climate as the key to understand the future. Example from the Mediterranean Sea

  • 1. PAST-CLIMATE AS THE KEY TO UNDERSTAND THE FUTURE: EXAMPLE FROM THE MEDITERRANEAN SEA VINCENZO PASCUCCI DIPARTIMENTO DI SCIENZE BOTANICHE, ECOLOGICHE E GEOLOGICHE UNIVERSITA’ DI SASSARI pascucci@uniss.it
  • 2. Climate is changing? Which are the evidences? Is this a normal process? Which have been recent past climatic changes? Which has been their impact? Can we say something?
  • 3. PATHWAY… - ACTUALISM 1. PRESENT CLIMAT 2. CAUSES OF CLIMATE CHANGE - PAST 1. GEOLOGICAL EVIDENCES OF CLIMATE CHANGES (SARDINIA) - CLIMATIC CHANGES OF THE LAST 125 KY
  • 4. WHAT INFLUENCE THE CLIMATE OF THE EARTH: 1. EARTH ORBIT AROUND THE SUN yearly
  • 5. p C L e I r M A m T a I C n e B E n L t T 2. LATITUDE & ALTITUDE
  • 6. 3. GREAT OCEAN CONVEYOR BELT 500 year to make the all circuit
  • 8. PLATE TECTONICS: long time (millions of year = radical changes)
  • 10. Orbital forces: short time (thousand of years = long lasting changes) today the Earth axis is 23°27’ inclined Milankovitch cycles
  • 11. Sun spots (hundreds to tens of years 500-11y) short time  climate changes = sensible The change in the number of sunspots and in solar activity (deduced from studies of carbon-14 concentrations in the wood of tree rings and of beryllium-10 in ice cores) suggests that there have been various exceptional periods of solar weakness during the last millennium, namely, the Wolf (around 1300), Spoerer (around 1500), Maunder (between 1645 and 1715) and Dalton (1800-1830) periods. These low points were most likely preceded by a period of maximum solar activity, the Medieval Solar Maximum (between 1100 and 1250) (Jirikowic, 1994). According to some authors, a similar maximum, the Contemporary Solar Maximum, is occurring right now and is caused by a rise in the magnetic activity of the solar corona during the 20th century (Lockwood, 1999). Basing their conclusions on models, some authors believe that the solar activity of the last 70 years is the most intense of the last 8,000 years (Solanki, 2004). 2009
  • 12.
  • 14. ANTARTICA & GREENLAND ICE DRILLING PROJECT
  • 15. EPICA & VOSTOK (ice drilling project)
  • 16. Main results are: 1. 8 glacial stages occurred during the last 740ky; 2. Interglacial past stages were as much warm as today; 3. Without human effect the present interglacial stage will last other 15ky; 4. CO2 concentration is the highest of the last 444ky
  • 17. What about CO2? Man has input more CO2 in the atmosphere in the last 200y than the earth system in 20ky… however normally an increase of CO2 into the system precedes the beginning of a glacial stage!!!! CO2 T
  • 18. Form Marine Isotopic Stages (MIS) to Glacial and Interglacial stages: the last 300ky …. Isotopic stages MIS (even=caluroso; odds=frio)…simple!!!
  • 19. The present interglacial stage: the last 11ky
  • 21. Hannibal crosses the Alps with the elephants during the warm roman time
  • 22. CLIMATE CHANGES OF THE LAST 1000 ANNI (ΔT = ±2 °C) important changes every 500y
  • 23. THE LAST 30y ΔT = ± 0.774 °C last coldest years 2007-08-09 (the most sensible to humans)
  • 24. TOOLS TO PERFORM PALEOCLIMATE STUDIES • Sedimentology  paleoenvironments • Stratigraphy  events order • Geomorphology  processes • Geochronology  time • Geochemistry  past atmosphere vs present (i.e. δ 18/16O)
  • 25. GEOLOGICAL ARCHIVES • ANTARCTIC – GREENLAND (ICE) • SARDINIA (ROCKS) • ALPS (ROCKS & ICE)
  • 26. ITALY  SARDINIA Tectonically stable since Pliocene and in the Mid of the Mediterranean Sea
  • 27. PAST GEOLOGICAL EVIDENCES OF CLIMATE CHANGES SARDINIA (ITALY) WEST COAST 1. CAPO CACCIA CAVES
  • 29. CAPO CACCIA: Partially submerged caves sea level height reached about 125ky + 4m
  • 30. -7m Cervo Sardo bones (deer extinguished around 40-30ky) are found into speleothems
  • 31. -7m Cervo Sardo bones (deer extinguished around 40-30ky) are found into speleothems
  • 32. SEA LEVEL MARKERS AND DEER BONES INDICATE THAT CAPO CACCIA CAVES WHERE FLOODED BY SEA RISE AROUND 125KY AND SUBSEQUENTLY EMERGED DUE TO SEA LEVEL FALL
  • 33. WEST SARDINIA: 2. prograding ancient beaches SEDIMENTOLOGY
  • 34. Detail: 2 relatively shallow water features today some meters above sea level 2 1 ALGHERO
  • 35. 3 2
  • 36. 3 2 3 2
  • 37. 3 2 3 23 paleosoil 2
  • 38. OSL ages dunes 3 2 Beaches and paleosoils
  • 39. ….moreover, tropical warm fauna in beach deposits STROMBUS BUBONIUS
  • 40. Additional items: 3. tidal notch and dunes 4. Tidal notch(s) +2/4m DUNES
  • 41. Things to remember • 1-4 features: – 1. fossiliferous/gravelly beach-shoreface (about 125ky); – 2. silicoclastic beach (about 100ky); – 3. dunes (about 77-47 ky); – 4. tidal notch(s) partially covered by dunes (125-100 ky);
  • 42. PAST GEOLOGICAL EVIDENCES OF CLIMATE CHANGES SARDINIA (ITALY) EST COAST CALA GONONE (OROSEI GULF)
  • 43. FEATURES INDICATING SEA LEVEL CHANGES 1. OLD NOTCH(S) (4/8 m asl) MODERN NOTCH
  • 44. 2. Bue Marino Cave aeolian sediments Medium-coarse grained BUE 1 sample bioclastic-rich sand, blown by the wind into the cave from a marine source (shelf/beach) BUE 5 sample BUE 2 sample
  • 45. 2. BUE MARINO CAVE SEDIMENTS: AGES BUE 1-5: 80-100KY AL: Speleothem samples, BUE: sediment samples 1: Jurassic limestone; 2: clastic sediments; 3: Lithophaga boreholes OSL age Clastic sedimentary infill pre-date the notch referred at 125ky
  • 46. FEATURES INDICATING CLIMATE CHANGES: 3. COARSE ALLUVIAL FAN (dated at 45ky OSL)
  • 48. 5. PERIGLACIAL DEPOSITS “ÉBULIS ORDONNÉ” (18-20 ky)
  • 49. now forming as cryo-clastic processes in the alps…
  • 50. Things to remember • 1-4 features: – 1. notch(s) (about 125ky) (sea level 4/6 m higher); – 2. cave sediments (aeolian) (about 100-80 ky) (input from an exposed sandy shelf during a relative sea level fall) ; – 3. coarse alluvial fan (about 40 ky); – 4. u-shaped valley (no age data); – 5. periglacial deposits (?18-20ky)
  • 52. SEA LEVEL CHANGES • 125ky (MIS 5) SL was at least +4m higher than today; • Since 80ky (end of MIS 5) sea level started to fall; • It reached the max of -130 bpsl about 20-18ky (MIS 2); • From 17-11ky sea level raised very fast (end MIS2); • We are in a highstand since 10ky (MIS 1) that should last for other about 15ky (without human influence)
  • 53. TEMPERATURES AND CLIMATE • 125-95 ky (MIS 5e) temp was at least +2/4 °C higher than today (subtropical climate and beaches formation). Apex of interglacial; • 90-80ky (MIS 5a) temp cooled down (-3/4 °C lower than today, soils formation) (warm and humid). End of interglacial; • 60-45ky (MIS 4) temp was -6/8 °C lower than today (cryoclast, u- shaped valley, exposure of shelf and dune formation) (cold and humiddry); • 45-20ky (MIS 3-2) temp was -8/10 °C lower than today (wide cryoclast deposits and dune formation) (cold and very dry) Apex of glacial
  • 54. C A C P A O P O C A C C A C C I C A I A 2 0 T K O Y D A A Y G O
  • 55. C A C P A O P O C A C C A C C I C A I A 2 0 T K O Y D A A Y G O
  • 56. WHAT IS NEW? 1. SEA LEVEL CHANGES
  • 57. SEA LEVEL FLUCTUATION DURING THE LAST INTERGLACIAL 130-80 KY (5 SUBSTAGES ABOUT 10KY EACH SEPARATED BY A STRONG EROSIONAL UNCONFORMITY; 2 ASL, 1 BSL) -bsl? +1m +4-6m
  • 58. 10 ky cycles may be referred to: • Subprecessional (or sub Milankovitch cycles); – This short-time cycles can increase or decrease the temperature of some degrees; – At this moment it is not clear at all the origin of the short-time cycles because very often they are non linear and in cases they have been correlated to dust aerosols present in the atmosphere); – Solar irradiation variations;
  • 59. Just an example: at the beginning of this interglacial, in about 10 ky, the ice melted more or less completely. This fast event is related to solar radiation changes.
  • 60. SEA LEVEL RISE AFTER THE LGM (18KY) …1 m rise every 100 years up to about 7/6ky, after that sea level become more or less stable up to nowadays
  • 61. …Y ITALIA SE CONVIRTIO’ EN BOTA!!!! 20ky ago In blu glaciers 6ky ago
  • 62. Further studies • Better characterize and explain the events occurred during the last interglacial; • Amount of dust in the past atmosphere; • Solar irradiation variations (long and short time); • Human impact on climate; • Better understanding of the Atlantic Multidecadal Oscillation (AMO) and if it existed also in the past (up to now not older than 150y)…. • More money to geological research because our future is written in the rocks and we only have to find the way to dig it out!!!
  • 63. Last example… thermal fluctuation of the North Atlantic Ocean (AMO) last 100 years Mountain glaciers increase when AMO index is negative, and retreat when AMO is positive
  • 64.
  • 65. Forecast based on past (BLU LINE) Forecast based on global warming idea (RED LINE)
  • 66. So what is going on? ?
  • 67. We will fire in the hellish earth!!!
  • 68. …or we will die iced!!!
  • 69. A possibility is also that someone is joking with us using climate change as personal purpose to become famous!!!
  • 70. ….but because everybody wants to speak about climate… GLOBAL WARMING EXPERCTS!!! I did it too!!!!!!!
  • 71. GRACIas Le nuvole del cielo disegnano la mia strada del ritorno,ma solo tu raggio di sole sai quale sia davvero. Mi manca la tua luce, il tuo calore, la tua bocca, il tuo consiglio. Questa notte solo naufragherò tra i miei sogni dove spero di incontrare la mia stella. (Vince 07)