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Marine Fishery Development and
        Climate Change

 Dr.Rani Mary George & Dr.G.Syda Rao

Central Marine Fisheries Research Institute
              Kochi 682 018
Marine Fishery development


   Marine fisheries have very important roles for food supply,
    food security and income generation in India.
    About one million people work directly in this sector,
    producing 3.1 million tonnes annually.
    The value of the marine fish landings have been estimated
    at Rs. 36,964 crores in 2010 and India has earned a foreign
    exchange of Rs. 10,000 crores through the export of 6 lakh
    tonnes of sea food products.
    The fisheries sector, presently contributes around one
    percent to the GDP and 4.72 percent to Agricultural GDP of
    our country (Sathiadhas et al., 2012).
Table1: Profile of marine fisheries in India (source: CMFRI, 2010)

   Component                                Profile
   Physical Component
   Coastline length (km)                    8129
   Exclusive Economic Zone (million km2)   2.02
   Continental shelf area (million km2)    0.50
   Area within 50m depth (million km2)     0.18
   Human Component
   Marine fisher population (million)       4.0
   Active fisher population (million)       1.5
   Infrastructure Component
   Landing centres                          1511
   Mechanized vessels                      72559
   Motorized vessels                       71313
   Non-motorized vessels                   50618
   Fish Catches
   Annual landings (2010) (million t)      3.07
   Potential yield (million t)             3.92
Climate Change
   Concerns on global warming have been with us now for
    more than a decade. The global warming that is widely
    expected to occur over this century will not be confined to
    the atmosphere; the oceans would also get warmer.
    Over the next 50 years, sea surface temperature in the
    Indian seas is expected to rise by 1 to 3. The oceans are
    predicted to acidify, become more saline, and the sea level
    will rise, and currents may change. It has been recognised
    that it will have consequences, both benign and
    disadvantageous, on fisheries.
   The effects of environmental change on fisheries are likely,
    therefore, to be severe. Such changes are likely to affect
    fish migrations and habitat, augmenting fish stocks in some
    places and decreasing them in others, perhaps causing
    stocks to be displaced permanently to new habitats.
Causal factor for
    climate change

   CO2 emission in the
    atmosphere has
    increased from 275
    ppm in 1750 to 383
    ppm in 2005.
   At the present trend,
    it may reach 450 ppm
    by 2030.
   Co2 concentration of
    550 ppm may be
    irreversible, and is
    threshold for several
    life processes.
Climate Change in the Oceans: Rise in Sea
                  Temperature

   The global average air temperature rose 0.74°C
    during the 100 year period ending in 2005.
   If the trend continues, the atmospheric
    temperature will increase by 2.2 to 4.8o C by
    2100.
   Seawater mean temperature increased 0.06o C in
    the last 50 years.
   Increase is not even: upper 300 m of the oceans
    increased by 0.31o C.
   The mean sea surface temperature in the Indian
    Seas warmed by 0.2o C in the last 45 years.
Rise in Sea Surface Temperature in the Indian
                    Seas
Climate Change in the Oceans: Rise in Acidity

   When CO2 enters the oceans, it reacts with
    seawater to form carbonic acid, producing
    hydrogen ions, which cause the acidity of the
    seawater to increase.
   In the last 250 years, the concentration of H+
    ions in seawater has increased by 30%, equating
    to a fall in pH by 0.1 unit.
   Continued rises in the concentration           of
    atmospheric CO2 will lead to a global surface
    water pH reduction of up to 0.4 units by 2100.
Climate Change in the Oceans: Rise in Sea Level

   Sea level will increase due to seawater warming,
    which causes thermal expansion of ocean water
    (responsible for 70% of the increase); and
    melting of glaciers and ice sheets of polar regions
    (30% of the increase)
   Sea level is expected to rise by 9 to 30 cm by
    2050 and by 30 to 90 cm by 2100.
   A 25 cm rise would displace large number of
    people from the Ganges delta, and drown
    Maldives.
Coral Bleaching

   Coral bleaching results when the
    symbiotic    zooxanthellae   (single-
    celled algae) are expelled from the
    host coral organisms due to stress;
    may lead to mortality of corals
    depending upon the intensity of
    bleaching
Degree Heating Week
   Degree Heating Weeks (DHWs) indicate the
    accumulation of thermal stress that coral reefs
    have experienced over the past 12 weeks. One
    DHW is equivalent to one week of sea surface
    temperatures one degree Celsius greater than
    the expected summertime maximum. Two DHWs
    are equivalent to two weeks at one degree above
    the expected summertime maximum OR one
    week of two degrees above the expected
    summertime maximum.
Satellite bleaching alerts
     There are five status levels: No Stress, Bleaching Watch, Bleaching
     Warning, Bleaching Alert Level 1, and Bleaching Alert Level 2. These

    levels are defined in terms of the CRW HotSpot and Degree Heating
                            Weeks (DHW) products:
Temperature stress and bleaching

   El Nino event
   Green house gases
Causes of Coral Bleaching
Factors      Mechanism                                 Effects
Acidific
       ation Lowering of pH and carbonate ion          Calcification rates reduce
             concentration
Temperature Sea surface temperature increase due to    Coral bleaching
             greenhouse effect
Sea level    Rise in sea level because of warming      Coastal flooding, input of
                                                       sediments
Storm         Increase in storm frequency & intensity Species decline or shift
Dust         Iron dust enhances phytoplankton and      Light penetration decrease,
             macroalgal growth; transport of           macroalgae compete with
             pathogens                                 corals for space
Projected demise of coral reefs in the Indian
                      Seas

Region            Decline starts     Remnant

Andaman              2030 2040
                        -            2050 2060
                                        -
Nicobar              2020 2030
                        -            2050 2060
                                        -
Lakshadweep          2020 2030
                        -            2030 2040
                                        -
Gulf of Mannar       2030 2040
                        -            2050 2060
                                        -
Gulf of Kachchh      2030 2040
                        -            2060 2070
                                        -
Research Projects at CMFRI in
  relation to climate change
Projects completed
 Impact,adaptation and vulnerability of
 Indian marine fisheries to climate change
 – ICAR Network Project
 (2007-2012).

 Carbon  sequestration potential of Indian
 seaweeds – In-house research Project
 (April 2010 to March 2012).
On-going Project
•   National Initiative on climate resilient agriculture (NICRA)
    (April 2011 onwards & continuing)

The main focal areas in this project include:

•   Studies on the trends in marine capture fisheries, changes in biology
    and distribution pattern of fishes in relation to changing climate.

•   Studies on climate resilient species suitable for mariculture as a step
    towards adaptive measures.

•   Technology demonstration for the benefit of coastal communities in
    order to harness the benefits of climate change

Institutions involved:
  Since the NICRA project is a national initiative of ICAR, many
  agriculture, animal science and fishery Institutes of ICAR are
  involved.
Fisheries and Climate
1.   Climate affects fisheries
2.   Climate affects biodiversity
3.   Fisheries affect biodiversity

    Fishing has a bigger effect on
     biodiversity than does climate
     change
    Our time series of changes in fish
     populations mainly come from
     fisheries
Changes in Distribution and Phenology

 Category 1: Shift in latitudinal distribution
 Category 2: Extension of distributional
  boundary
 Category 3: No shift/extension of
  boundary, but change in biomass
 Category 4: Shift in depth of occurrence

 Category 5: Spatial shift in spawning

 Category   6: Temporal shift in spawning
Extension of northern boundary of oil sardine
               (the colored lines indicate percentage of All India oil sardine production)


                         1961-1976                          1977-1986
LATITUDE(°N)




                                                                                        0.1% - 1%
                                                                                        1% - 10%
                                                                                       10 % - 25%
                         1987-1996                          1997-2006                  25% - 50%
                                                                                        >50%




                                      LONGITUDE(°E]
Distributional Changes
   With warming of the sea, the fish is able to find
    temperature to its preference in the northern
    latitudes and eastern longitudes, thereby
    extending the distributional boundaries and
    establishing fisheries in larger coastal areas.
   It is expected that the abundance may increase
    along Gujarat and West Bengal coasts in the
    coming years assuming further increase in sea
    temperature.
   These distributional shifts are expected to result
    in drastic changes in species mix and ecosystem
    structures and functions.
   Will this trend pave the way for species
    replacement?
Shift/extension of depth of occurrence


The Indian mackerel, Rastrelliger kanagurta, the second important
resource contributing 7.9% of total landings for 2010 in addition
to extension of its northern boundary, is found to descend to
deeper waters in the last two decades. The fish normally occupies
surface and subsurface waters. During 1985-1989, only 2% of
mackerel catch was from bottom trawlers, and the rest of the
catch was contributed by pelagic gear such as drift gillnet. During
2003-2010, it is estimated that 15% of mackerel catch is
contributed by bottom trawlers along the Indian coast. The
Indian trawlers operate at a depth ranging from 20m to 80m by
employing high opening trawlers. In the last 25 years, the
specifications of trawlnet such as mouth opening, headrope
length, otterboard and mesh size have not been modified, and
hence the increase in the contribution of trawlers to the mackerel
catch is not gear-related. As the surface waters are also warming
up, it appears that the mackerel, being a tropical fish, has
extended its veridical boundary to deeper waters.
Phenological changes

   The phenology of species, i. e., the sequence and
    timing of events – growth, maturation,
    reproduction – in their life cycle, is affected.
   The peak spawning season of threadfin breams
    off Chennai is found to shift from warmer months
    of April & May towards relatively cooler months of
    January & February
   The shift in the timings of maturation and
    reproduction may cause mismatches between the
    production of planktonic propagules in one part,
    and the usual patterns of coastal circulation or
    the availability of appropriate food items in the
    other.
Phenological changes
   The threadfin breams Nemipterus japonicas and N.mesoprion are
    distributed along the entire Indian coast at depths ranging from 10 to 100
    m. They are short-lived (longevity: about 3 years), fast growing, highly
    fecund (annual egg production around 0.2 million per adult female) and
    medium-sized fishes (maximum length: 35 cm). Data on the number of
    female spawners collected every month off Chennai (south-east coast of
    India) from 1981 to 2010 indicated wide monthly fluctuations. However, a
    trend in the shifting of spawning season from warmer (April-September)
    to cooler months (October-March) was discernible. Whereas 35.3% of the
    spawners of N.japonicus occurred during warm months, the number of
    spawners gradually reduced and only 5.0% of the spawners occurred
    during the same season. A similar trend was observed in N.mesoprion
    too. The present occurrence of spawners of the two species linearly
    decreased with increasing temperature during April-September, but
    increased with increasing temperature during October-March over the time
    scale.
Options for fisheries and aquaculture sector for adaptation

Tackling overfishing

•     Options for adaptation are limited, but they do exist. The
    impact of climate change depends on the magnitude of change,
    and on the sensitivity of particular species or ecosystems
    (Brander 2008).
•     Fish populations are facing the familiar problems of overfishing,
    pollution and habitat degradation.
•    Food and Agriculture Organization has estimated that about
    25% of all fish stocks are overexploited and 50% are fully
    exploited (FAO 2007).
•    Reduction of fishing effort will benefit in relation to adaptation of
    fish stocks and marine ecosystems to climate impacts; and
    mitigation by reducing greenhouse gas emissions. Hence, some
    of the most effective actions which we can be taken to tackle
    climate impacts are to deal with the old familiar problems such as
    overfishing (Brander 2008) and adapt Code of Conduct for
    Responsible Fisheries (FAO 2007).
Cultivation of sea plants

• Sea plants are excellent carbon sequestration agents
and many of them sequester at a rate better than their
terrestrial counterparts (Zon 2005).
• CO2 sequestration by the common sea plants such
as the red algae Gracilaria corticata and G.edulis,
brown alga Sargassum polycystum and the green alga
Ulva lactuca has been qualified in laboratory studies
in India by Kaladharan et al. (2008).
• The seaweed Kappaphycus alvarezii has been
collected and experiments are in progress. Initial
results suggest that the seaweed has good carbon
sequestration potential (CMFRI, 2010).
Studied the carbon fixing efficiency of two macrophytes – Red alga
Kappaphycus alvarezii and brown alga Padina sp.




Stock of Kappaphycus alvarezii               Padina sp.
CO2 utilization by Kappaphycus

• In K. alvarezii, when the CO2 levels in the
  medium was increased from 10 to 50 ppm,
  the utilization gradually increased to 32
  ppm.

• With further increase in concentration (very
  high levels), the utilization was 90 ppm at a
  level of 185 ppm of CO2 in the medium.

• Thus, Kappaphycus is able to increase the
  utilization of CO2 upto a level of 185 ppm
  CO2 in the medium.
CO2 utilization by Padina
   The CO2 utilization increased with increasing
    concentration and the utilization was 100% at
    2, 10, 20, 30, 40 & 50 ppm CO2 levels in the
    medium.

   At very high concentration of 230 and 370ppm,
    the utilization remained stable at 140ppm;
    indicating that no increase in utilization would
    be possible with further increase of CO2 in the
    medium.

   Thus, Padina is able to increase utilization of
    CO2 upto 230 ppm CO2 level in the medium.
   Studies indicate that seaweeds are excellent source for
    fixing high levels of CO2.

   The current CO2 concentration in the atmosphere is 373
    ppm. Experiments have been conducted with this value as
    the maximum reference point.

   Kappaphycus is able to increase utilization of CO2 upto 185
    ppm concentration and Padina upto 230 ppm
    concentration.

   However, the CO2 utilization efficiency is maximum at a
    low concentration of 50 ppm and decreases beyond this
    concentration.

   The highest gross and net production of these two species
    were also at a low concentration of 20 ppm.
 Padina appears to be a better carbon
  sequestrating plant compared to
  Kappaphycus.
 This preliminary study has provided
  important clues on the carbon
  sequestration potential of seaweeds.
 These data will be useful for future research
  on estimating CO2 potential of Indian
  seaweeds.
 Direct in situ measurements on CO2
  utilization - if made in Kappaphycus farms
  in Mandapam area -will be useful to
  validate the results.
Cultivation of halophytes

•    In coastal areas and mudflats near the
    sea, where the salinity does not allow
    farming of the usual food crops, plants
    that grow and flourish those conditions are
    advocated.

•    One such plant is the sea asparagus,
    Salicornia.  The plant grows well with
    maximum yields in hot climates if the
    seeds are sown in cool season so as to
    reach maturity during the hot months
Concerns & Adaptive mechanisms

Uncertainties in fish availability and supply

•   Adapt Code of Conduct for Responsible Fisheries
•   Develop knowledge-base for climate change
    impact of fisheries and aquaculture
•   Predict medium and long term probabilistic
    production
•   Assess the adaptation capacity, resilience and
    vulnerability of marine production systems
•   Adjust fishing fleet and infrastructure capacity
New challenges for risk assessment

• Consider increasing frequency       of
  extreme weather events

• Consider past management practices
  to evolve robust adaptation systems

• Identify and address the vulnerability
  of specific communities; consider
  gender and equity issues.
Complexities of climate change interactions into
governance of frameworks to meet food security
objectives

•Recognition of climate-related processes, and their
interaction with others

•Action plans at national/regional level based on (a)
Code of Conduct for Responsible Fisheries; (b)
Integrated     ecosystem-based      fisheries    and
aquaculture management plans (c ) framework for
expansion of aquaculture (d) linkage among cross-
sectoral policy framework such as insurance,
agriculture, rural development and trade
Fisheries and aquaculture may be more
vulnerable in conflicts with other sectors

•   Action plans should involve not only
    fisheries institutions/departments, but
    also those for national development
    planning and finance

•   Sharing and exchange of information with
    other sectors

•   Existing management plans for fisheries
    need to be reviewed by considering
    climate change
Financing climate change adaptation and mitigation measures

•   Fishermen, fish farmers, processors, traders and exporters
    should increase self protection through financial mechanisms
•   Improving equity and economic access such as microcredit
    should be linked to adaptation responses
•   Investment of infrastructure such as construction of fishing
    harbor, should consider climate change
•   Financial allocation in national budget for risk reduction and
    prevention practices such as early warning systems and
    disaster recovery programmes and for relocation of villages
    from low lying area
•   Fiscal incentive for reducing the sector’s carbon footprint and
    other mitigation and adaptation options
•   Full potential of existing financial mechanisms has to adapt
    and mitigate the issue of climate change.
Conclusion
In the context of climate change, the primary challenge to the
fisheries and aquaculture sector will be to ensure food supply,
enhance nutritional security, and improve livelihood and
economic output, and ecosystem safety. These objectives call for
identifying and addressing the concerns arising out of climate
change; evolve adaptive mechanisms and implement action
across all stakeholders at national, regional and international
levels. In response to shifting fish population and species, the
fishing sector may have to respond with the right types of craft
and gear combinations, on-board processing equipments etc.
Governments should consider establishing Weather Watch
Groups and decision support systems on a regional basis.
Allocating research funds to analyze the impacts and establishing
institutional mechanisms to enable the sector are also important.
The relevance of active regional and international participation
and collaboration to exchange information and ideas is being felt
now as never before.
THANK YOU

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Marine fishery development & climate change_Dr Rani Mary George(The Kerala Environment Congress)_2012

  • 1. Marine Fishery Development and Climate Change Dr.Rani Mary George & Dr.G.Syda Rao Central Marine Fisheries Research Institute Kochi 682 018
  • 2. Marine Fishery development  Marine fisheries have very important roles for food supply, food security and income generation in India.  About one million people work directly in this sector, producing 3.1 million tonnes annually.  The value of the marine fish landings have been estimated at Rs. 36,964 crores in 2010 and India has earned a foreign exchange of Rs. 10,000 crores through the export of 6 lakh tonnes of sea food products.  The fisheries sector, presently contributes around one percent to the GDP and 4.72 percent to Agricultural GDP of our country (Sathiadhas et al., 2012).
  • 3. Table1: Profile of marine fisheries in India (source: CMFRI, 2010)  Component Profile  Physical Component  Coastline length (km) 8129  Exclusive Economic Zone (million km2) 2.02  Continental shelf area (million km2) 0.50  Area within 50m depth (million km2) 0.18  Human Component  Marine fisher population (million) 4.0  Active fisher population (million) 1.5  Infrastructure Component  Landing centres 1511  Mechanized vessels 72559  Motorized vessels 71313  Non-motorized vessels 50618  Fish Catches  Annual landings (2010) (million t) 3.07  Potential yield (million t) 3.92
  • 4. Climate Change  Concerns on global warming have been with us now for more than a decade. The global warming that is widely expected to occur over this century will not be confined to the atmosphere; the oceans would also get warmer.  Over the next 50 years, sea surface temperature in the Indian seas is expected to rise by 1 to 3. The oceans are predicted to acidify, become more saline, and the sea level will rise, and currents may change. It has been recognised that it will have consequences, both benign and disadvantageous, on fisheries.  The effects of environmental change on fisheries are likely, therefore, to be severe. Such changes are likely to affect fish migrations and habitat, augmenting fish stocks in some places and decreasing them in others, perhaps causing stocks to be displaced permanently to new habitats.
  • 5. Causal factor for climate change  CO2 emission in the atmosphere has increased from 275 ppm in 1750 to 383 ppm in 2005.  At the present trend, it may reach 450 ppm by 2030.  Co2 concentration of 550 ppm may be irreversible, and is threshold for several life processes.
  • 6. Climate Change in the Oceans: Rise in Sea Temperature  The global average air temperature rose 0.74°C during the 100 year period ending in 2005.  If the trend continues, the atmospheric temperature will increase by 2.2 to 4.8o C by 2100.  Seawater mean temperature increased 0.06o C in the last 50 years.  Increase is not even: upper 300 m of the oceans increased by 0.31o C.  The mean sea surface temperature in the Indian Seas warmed by 0.2o C in the last 45 years.
  • 7.
  • 8.
  • 9. Rise in Sea Surface Temperature in the Indian Seas
  • 10. Climate Change in the Oceans: Rise in Acidity  When CO2 enters the oceans, it reacts with seawater to form carbonic acid, producing hydrogen ions, which cause the acidity of the seawater to increase.  In the last 250 years, the concentration of H+ ions in seawater has increased by 30%, equating to a fall in pH by 0.1 unit.  Continued rises in the concentration of atmospheric CO2 will lead to a global surface water pH reduction of up to 0.4 units by 2100.
  • 11. Climate Change in the Oceans: Rise in Sea Level  Sea level will increase due to seawater warming, which causes thermal expansion of ocean water (responsible for 70% of the increase); and melting of glaciers and ice sheets of polar regions (30% of the increase)  Sea level is expected to rise by 9 to 30 cm by 2050 and by 30 to 90 cm by 2100.  A 25 cm rise would displace large number of people from the Ganges delta, and drown Maldives.
  • 12. Coral Bleaching  Coral bleaching results when the symbiotic zooxanthellae (single- celled algae) are expelled from the host coral organisms due to stress; may lead to mortality of corals depending upon the intensity of bleaching
  • 13. Degree Heating Week  Degree Heating Weeks (DHWs) indicate the accumulation of thermal stress that coral reefs have experienced over the past 12 weeks. One DHW is equivalent to one week of sea surface temperatures one degree Celsius greater than the expected summertime maximum. Two DHWs are equivalent to two weeks at one degree above the expected summertime maximum OR one week of two degrees above the expected summertime maximum.
  • 14. Satellite bleaching alerts There are five status levels: No Stress, Bleaching Watch, Bleaching Warning, Bleaching Alert Level 1, and Bleaching Alert Level 2. These  levels are defined in terms of the CRW HotSpot and Degree Heating Weeks (DHW) products:
  • 15. Temperature stress and bleaching El Nino event Green house gases
  • 16. Causes of Coral Bleaching Factors Mechanism Effects Acidific ation Lowering of pH and carbonate ion Calcification rates reduce concentration Temperature Sea surface temperature increase due to Coral bleaching greenhouse effect Sea level Rise in sea level because of warming Coastal flooding, input of sediments Storm Increase in storm frequency & intensity Species decline or shift Dust Iron dust enhances phytoplankton and Light penetration decrease, macroalgal growth; transport of macroalgae compete with pathogens corals for space
  • 17. Projected demise of coral reefs in the Indian Seas Region Decline starts Remnant Andaman 2030 2040 - 2050 2060 - Nicobar 2020 2030 - 2050 2060 - Lakshadweep 2020 2030 - 2030 2040 - Gulf of Mannar 2030 2040 - 2050 2060 - Gulf of Kachchh 2030 2040 - 2060 2070 -
  • 18. Research Projects at CMFRI in relation to climate change
  • 19. Projects completed  Impact,adaptation and vulnerability of Indian marine fisheries to climate change – ICAR Network Project (2007-2012).  Carbon sequestration potential of Indian seaweeds – In-house research Project (April 2010 to March 2012).
  • 20. On-going Project • National Initiative on climate resilient agriculture (NICRA) (April 2011 onwards & continuing) The main focal areas in this project include: • Studies on the trends in marine capture fisheries, changes in biology and distribution pattern of fishes in relation to changing climate. • Studies on climate resilient species suitable for mariculture as a step towards adaptive measures. • Technology demonstration for the benefit of coastal communities in order to harness the benefits of climate change Institutions involved: Since the NICRA project is a national initiative of ICAR, many agriculture, animal science and fishery Institutes of ICAR are involved.
  • 21. Fisheries and Climate 1. Climate affects fisheries 2. Climate affects biodiversity 3. Fisheries affect biodiversity  Fishing has a bigger effect on biodiversity than does climate change  Our time series of changes in fish populations mainly come from fisheries
  • 22. Changes in Distribution and Phenology  Category 1: Shift in latitudinal distribution  Category 2: Extension of distributional boundary  Category 3: No shift/extension of boundary, but change in biomass  Category 4: Shift in depth of occurrence  Category 5: Spatial shift in spawning  Category 6: Temporal shift in spawning
  • 23. Extension of northern boundary of oil sardine (the colored lines indicate percentage of All India oil sardine production) 1961-1976 1977-1986 LATITUDE(°N) 0.1% - 1% 1% - 10% 10 % - 25% 1987-1996 1997-2006 25% - 50% >50% LONGITUDE(°E]
  • 24. Distributional Changes  With warming of the sea, the fish is able to find temperature to its preference in the northern latitudes and eastern longitudes, thereby extending the distributional boundaries and establishing fisheries in larger coastal areas.  It is expected that the abundance may increase along Gujarat and West Bengal coasts in the coming years assuming further increase in sea temperature.  These distributional shifts are expected to result in drastic changes in species mix and ecosystem structures and functions.  Will this trend pave the way for species replacement?
  • 25. Shift/extension of depth of occurrence The Indian mackerel, Rastrelliger kanagurta, the second important resource contributing 7.9% of total landings for 2010 in addition to extension of its northern boundary, is found to descend to deeper waters in the last two decades. The fish normally occupies surface and subsurface waters. During 1985-1989, only 2% of mackerel catch was from bottom trawlers, and the rest of the catch was contributed by pelagic gear such as drift gillnet. During 2003-2010, it is estimated that 15% of mackerel catch is contributed by bottom trawlers along the Indian coast. The Indian trawlers operate at a depth ranging from 20m to 80m by employing high opening trawlers. In the last 25 years, the specifications of trawlnet such as mouth opening, headrope length, otterboard and mesh size have not been modified, and hence the increase in the contribution of trawlers to the mackerel catch is not gear-related. As the surface waters are also warming up, it appears that the mackerel, being a tropical fish, has extended its veridical boundary to deeper waters.
  • 26. Phenological changes  The phenology of species, i. e., the sequence and timing of events – growth, maturation, reproduction – in their life cycle, is affected.  The peak spawning season of threadfin breams off Chennai is found to shift from warmer months of April & May towards relatively cooler months of January & February  The shift in the timings of maturation and reproduction may cause mismatches between the production of planktonic propagules in one part, and the usual patterns of coastal circulation or the availability of appropriate food items in the other.
  • 27. Phenological changes  The threadfin breams Nemipterus japonicas and N.mesoprion are distributed along the entire Indian coast at depths ranging from 10 to 100 m. They are short-lived (longevity: about 3 years), fast growing, highly fecund (annual egg production around 0.2 million per adult female) and medium-sized fishes (maximum length: 35 cm). Data on the number of female spawners collected every month off Chennai (south-east coast of India) from 1981 to 2010 indicated wide monthly fluctuations. However, a trend in the shifting of spawning season from warmer (April-September) to cooler months (October-March) was discernible. Whereas 35.3% of the spawners of N.japonicus occurred during warm months, the number of spawners gradually reduced and only 5.0% of the spawners occurred during the same season. A similar trend was observed in N.mesoprion too. The present occurrence of spawners of the two species linearly decreased with increasing temperature during April-September, but increased with increasing temperature during October-March over the time scale.
  • 28. Options for fisheries and aquaculture sector for adaptation Tackling overfishing • Options for adaptation are limited, but they do exist. The impact of climate change depends on the magnitude of change, and on the sensitivity of particular species or ecosystems (Brander 2008). • Fish populations are facing the familiar problems of overfishing, pollution and habitat degradation. • Food and Agriculture Organization has estimated that about 25% of all fish stocks are overexploited and 50% are fully exploited (FAO 2007). • Reduction of fishing effort will benefit in relation to adaptation of fish stocks and marine ecosystems to climate impacts; and mitigation by reducing greenhouse gas emissions. Hence, some of the most effective actions which we can be taken to tackle climate impacts are to deal with the old familiar problems such as overfishing (Brander 2008) and adapt Code of Conduct for Responsible Fisheries (FAO 2007).
  • 29. Cultivation of sea plants • Sea plants are excellent carbon sequestration agents and many of them sequester at a rate better than their terrestrial counterparts (Zon 2005). • CO2 sequestration by the common sea plants such as the red algae Gracilaria corticata and G.edulis, brown alga Sargassum polycystum and the green alga Ulva lactuca has been qualified in laboratory studies in India by Kaladharan et al. (2008). • The seaweed Kappaphycus alvarezii has been collected and experiments are in progress. Initial results suggest that the seaweed has good carbon sequestration potential (CMFRI, 2010).
  • 30. Studied the carbon fixing efficiency of two macrophytes – Red alga Kappaphycus alvarezii and brown alga Padina sp. Stock of Kappaphycus alvarezii Padina sp.
  • 31. CO2 utilization by Kappaphycus • In K. alvarezii, when the CO2 levels in the medium was increased from 10 to 50 ppm, the utilization gradually increased to 32 ppm. • With further increase in concentration (very high levels), the utilization was 90 ppm at a level of 185 ppm of CO2 in the medium. • Thus, Kappaphycus is able to increase the utilization of CO2 upto a level of 185 ppm CO2 in the medium.
  • 32. CO2 utilization by Padina  The CO2 utilization increased with increasing concentration and the utilization was 100% at 2, 10, 20, 30, 40 & 50 ppm CO2 levels in the medium.  At very high concentration of 230 and 370ppm, the utilization remained stable at 140ppm; indicating that no increase in utilization would be possible with further increase of CO2 in the medium.  Thus, Padina is able to increase utilization of CO2 upto 230 ppm CO2 level in the medium.
  • 33. Studies indicate that seaweeds are excellent source for fixing high levels of CO2.  The current CO2 concentration in the atmosphere is 373 ppm. Experiments have been conducted with this value as the maximum reference point.  Kappaphycus is able to increase utilization of CO2 upto 185 ppm concentration and Padina upto 230 ppm concentration.  However, the CO2 utilization efficiency is maximum at a low concentration of 50 ppm and decreases beyond this concentration.  The highest gross and net production of these two species were also at a low concentration of 20 ppm.
  • 34.  Padina appears to be a better carbon sequestrating plant compared to Kappaphycus.  This preliminary study has provided important clues on the carbon sequestration potential of seaweeds.  These data will be useful for future research on estimating CO2 potential of Indian seaweeds.  Direct in situ measurements on CO2 utilization - if made in Kappaphycus farms in Mandapam area -will be useful to validate the results.
  • 35. Cultivation of halophytes • In coastal areas and mudflats near the sea, where the salinity does not allow farming of the usual food crops, plants that grow and flourish those conditions are advocated. • One such plant is the sea asparagus, Salicornia. The plant grows well with maximum yields in hot climates if the seeds are sown in cool season so as to reach maturity during the hot months
  • 36. Concerns & Adaptive mechanisms Uncertainties in fish availability and supply • Adapt Code of Conduct for Responsible Fisheries • Develop knowledge-base for climate change impact of fisheries and aquaculture • Predict medium and long term probabilistic production • Assess the adaptation capacity, resilience and vulnerability of marine production systems • Adjust fishing fleet and infrastructure capacity
  • 37. New challenges for risk assessment • Consider increasing frequency of extreme weather events • Consider past management practices to evolve robust adaptation systems • Identify and address the vulnerability of specific communities; consider gender and equity issues.
  • 38. Complexities of climate change interactions into governance of frameworks to meet food security objectives •Recognition of climate-related processes, and their interaction with others •Action plans at national/regional level based on (a) Code of Conduct for Responsible Fisheries; (b) Integrated ecosystem-based fisheries and aquaculture management plans (c ) framework for expansion of aquaculture (d) linkage among cross- sectoral policy framework such as insurance, agriculture, rural development and trade
  • 39. Fisheries and aquaculture may be more vulnerable in conflicts with other sectors • Action plans should involve not only fisheries institutions/departments, but also those for national development planning and finance • Sharing and exchange of information with other sectors • Existing management plans for fisheries need to be reviewed by considering climate change
  • 40. Financing climate change adaptation and mitigation measures • Fishermen, fish farmers, processors, traders and exporters should increase self protection through financial mechanisms • Improving equity and economic access such as microcredit should be linked to adaptation responses • Investment of infrastructure such as construction of fishing harbor, should consider climate change • Financial allocation in national budget for risk reduction and prevention practices such as early warning systems and disaster recovery programmes and for relocation of villages from low lying area • Fiscal incentive for reducing the sector’s carbon footprint and other mitigation and adaptation options • Full potential of existing financial mechanisms has to adapt and mitigate the issue of climate change.
  • 41. Conclusion In the context of climate change, the primary challenge to the fisheries and aquaculture sector will be to ensure food supply, enhance nutritional security, and improve livelihood and economic output, and ecosystem safety. These objectives call for identifying and addressing the concerns arising out of climate change; evolve adaptive mechanisms and implement action across all stakeholders at national, regional and international levels. In response to shifting fish population and species, the fishing sector may have to respond with the right types of craft and gear combinations, on-board processing equipments etc. Governments should consider establishing Weather Watch Groups and decision support systems on a regional basis. Allocating research funds to analyze the impacts and establishing institutional mechanisms to enable the sector are also important. The relevance of active regional and international participation and collaboration to exchange information and ideas is being felt now as never before.