Tamara Shiganova P.P.Shirshov Institute of Oceanology RAS Moscow, Russia

Slides:



Advertisements
Similar presentations
Unit 9 It's warm 清丰县第一实验小学 唐利娟.
Advertisements

Water Quality Indicators
Assessment of the main drivers of the Black Sea ecosystem functioning Mnemiopsis leidyi and Beroe ovata impact on the Black Sea ecosystem. Modeling approach.
Chapter 16 The Dynamic Ocean.
Seasonal and Interannual Variability of Peruvian anchovy Population Dynamics --progress report-- Yi Xu and Fei Chai June 2007.
Eutrophication of the Black Sea
The Changing Climate and Ecology in Narragansett Bay Candace Oviatt 10/12/12.
Royal Netherlands Institute for Sea Research 1 Seasonal timing of reproduction in the bivalve Macoma balthica: a model study of fitness consequences NVTB.
Chesapeake Bay: An Introduction to an Ecosystem Section 4: Communities II-1E3: Plankton View this quiz as a slide show from “the beginning” During the.
Chapter 13 Biological Productivity and Energy Transfer
Nutrient Cycles Eutrophication Nitrogen –Chemical Forms in the Aquatic Environment –Chemical Transformations –Cycle f-ratio Carbon.
1 The role of Anthropogenic and Climatic Forcing in the Long-term Changes of the Black Sea Ecosystem Temel Oguz
Population Interactions Competition for Resources: –Exploitative competition: Both organisms competing for the same resource(s). –Interference competition.
Increase in Jellyfish Blooms Hanad Duale Jeff Falcone Omar Laroussi.
BULGARIAN ACADEMY OF SCIENCES Institute of Oceanology — Varna, Bulgaria LONG – TERM SHIFTS IN THE BLACK SEA PLANKTON COMMUNITY (BULGARIAN COAST) K. Stefanova,
Carbon Isotope Variations in Aquatic Plants: Applications Onshore-Offshore (Benthic vs. Pelagic?) Kelp forest ecology Decreased productivity in the Bering.
Potential Approaches Empirical downscaling: Ecosystem indicators for stock projection models are projected from IPCC global climate model simulations.
G. Nolan 1, K.Lyons 1, S.Fennell 1, T. Mc Grath 1, D.Guihen 2, C.Cusack 1, C. Lynam 3 G. Nolan 1, K.Lyons 1, S.Fennell 1, T. Mc Grath 1, D.Guihen 2, C.Cusack.
INTERANNUAL DYNAMICS OF THE BLACK SEA ANOXIC ZONE BOUNDARY IN CONNECTION WITH CLIMATIC VARIABILITY E. V. YAKUSHEV, O.I.PODYMOV Southern Branch of P.P.Shirshov.
Succession in a water column An adapting ecosystem maneuvering between autotrophy and heterotrophy Jorn Bruggeman Theoretical biology Vrije Universiteit.
Zooplankton processes Puget Sound Oceanography Jan. 28, 2011.
Phytoplankton Translates from Greek “free-floating plants”
Jędrasik J., Kowalewski M., Ołdakowski B., University of Gdansk, Institute of Oceanography Impact of the Vistula River waters on the Gulf of Gdańsk during.
NILE PERCH Lates niloticus
P.P.Shirshov Institute of Oceanology Russian Academy of Sciences Tamara Shiganova.
Ecological processes in a changing climate: winners and losers Third US GLOBEC Pan Regional Workshop 20 February 2009 J. Runge, presenter.
State of the Oceans Portfolio Committee 13 February 2013.
Main goals of time series analysis: (a) identifying the nature of the phenomenon studied (b) forecasting (predicting future values of the time series.
Effects of hypoxia on gelatinous zooplankton predation of copepods in the Chesapeake Bay Wen-Cheng Liu 1, Mary Beth Decker 2, James J. Pierson 1 1. Horn.
Stratification on the Eastern Bering Sea Shelf, Revisited C. Ladd 1, G. Hunt 2, F. Mueter 3, C. Mordy 2, and P. Stabeno 1 1 Pacific Marine Environmental.
Centre for Ecological and Evolutionary Synthesis ICES/NAFO Decadal Symposium Santander, Spain May 12th 2011 The serial recruitment failure to North Sea.
Comparison of Synchronous Ecological Regime Shifts in the Humboldt and Kuroshio Currents Jürgen Alheit Baltic Sea Research Institute Warnemünde, Germany.
A Pollution Case Study: The Black Sea. Background  Enclosed sea with only the Bosphorus as communicating waterway with Aegean and Mediterranean Bosphorus.
Imagery.
Arctic Operational Oceanography at IMR Einar Svendsen Arctic GOOS planning meeting, September 2006 at NERSC, Bergen.
Summary Euphausiids (krill) are important food items of fish, seabirds and whales: consequently, it is important to understand their seasonal cycles. The.
1 State of San Lorenzo River Symposium Nicole Beck, PhD 2NDNATURE April San Lorenzo Lagoon A Decade of Dry Season WQ Monitoring.
Interannual Time Scales: ENSO Decadal Time Scales: Basin Wide Variability (e.g. Pacific Decadal Oscillation, North Atlantic Oscillation) Longer Time Scales:
ECODRIVE Ecosystem Change in the North Sea: Processes, Drivers, Future Scenarios 2009 – 2012 Overarching Theme Impact of Climate.
Mesozooplankton-microbial food web interactions in a climatically changing sea ice environment Evelyn & Barry Sherr, Oregon State University Carin Ashjian,
The management of small pelagics. Comprise the 1/3 of the total world landings Comprise more than 50% of the total Mediterranean landings, while Two species,
Factors contributing to variability in pCO 2 and omega in the coastal Gulf of Maine. J. Salisbury, D. Vandemark, C. Hunt, C. Sabine, S. Musielewicz and.
Seasonal variations in mean water column temperatures in the northern GOA (obtained from IMS GLOBEC website ). The temperature.
*Minagawa M, Usui T, Miura Y, Nagao S, Irino T, Kudo I, and Suzuki K, Graduate School of Environmental Science, Hokkaido University, Sapporo ,
Ocean Acidification Is aquaculture in a pickle? Andrew Forsythe Chief Scientist, Aquaculture and Biotechnology National Institute of Water and Atmospheric.
Interannual Time Scales: ENSO Decadal Time Scales: Basin Wide Variability (e.g. Pacific Decadal Oscillation, North Atlantic Oscillation) Longer Time Scales:
Ecosystem Research Initiative (ERI) for the Gulf of Maine Area (GoMA)
Marine Ecosystem Simulations in the Community Climate System Model
Ocean-scale modelling of Calanus finmarchicus
DRV/RH/Ecohal The influence of climate change on commercial flatfish populations in the Bay of Biscay O. Le Pape, D. Guérault and Y. Désaunay Bergen ICES.
Simulation labs for Biology 4263 I gave an introductory lab talk on Keystone Predators and Barnacles and Tides on Thursday, April 16 th. These labs are.
FIGURE 11.1 Size classification of plankton based on Sieburth et al. (1978). Note the logarithmic scale on the size axis. Most estuarine zooplankton range.
Daily Variation in Ctenophore Abundance during Summer 2012 in the long term Skidaway River Monitoring Program (SRIMP) Site Mariya Campbell.
Environmental Monitoring in the Black Sea Meeting Name, Dates, Venue Joint Survey Prepared by: Alexander Mikaelyan with contribution of Jaroslav Slobodnik,
Growth Rates of Euphausiids in the Northern Gulf of Alaska in A.I. Pinchuk *, R.R. Hopcroft, K.O. Coyle Institute of Marine Science, University.
Nutrients in sea water Introduction Distribution of Phosphorus and seasonal variation Distribution of nitrogen compounds Distribution of silicates and.
Modeling phytoplankton seasonal variation and nutrients budget of a Semi-Arid region ecosystem in the Southern Mediterranean Sea: -Case of the Bizerte.
Anthropogenic and natural impacts on the Si-flows in the Danube catchment and the Western Black Sea Christoph Lampert, Jos van Gils, Matthias Zessner,
Date of download: 6/22/2016 Copyright © 2016 SPIE. All rights reserved. Sampling transects conducted in the southern Caspian Sea in the period of 2001.
Tracking life history of each particle Particles could be divided into three groups (Fig. 7) The red group’s period of copepodite stage shortened when.
Mortality by Gelatinous Zooplankton
Food web and microbial loop Eutrophic vs. Oligotrophic food webs
Sea Surface Temperature as a Trigger of Butterfish Migration: A Study of Fall Phenology Amelia Snow1, John Manderson2, Josh Kohut1, Laura Palamara1, Oscar.
Laura Boicenco National Institute for Marine Research and Development
Diagram.
The effect of ship Nox deposition on cyanobacteria blooms
Relationship Between NO3 and Salinity:
Korea Ocean Research & Development Institute, Ansan, Republic of Korea
Indicators of Stream Health
P.P.Shirshov Institute of oceanology Russian Academy of Sciences
Presentation transcript:

Tamara Shiganova P.P.Shirshov Institute of Oceanology RAS Moscow, Russia

Main large scale events, which changed ecosystem functioning and provoked first gelatinous species blooms runoff regulation of the major rivers; increase in the input of dissolved mineral forms of phosphates and nitrates from large rivers accompanied by reduced silicate supply. This resulted in a decrease in the Si : P and Si : N ratios, which are important for the functioning of phytoplankton; changes in the composition of phytoplankton species and dominance of dinoflagellates instead of dominance of diatoms, significant growth in the phytoplankton biomass and outburst of harmful algae; Subsequent eutrophication overfishing of large predator fish and dolphins, resulted in decrease of top-down control

Enterannual changes mean summer temperature upper and intermedial layers Data of Hydrophysics lab SB IORAS

Subdivision of the Black Sea fish, zoo- and gelatinous plankton species in their relation to mean seasonal, annual and minimal winter SST: blue-cold water, red-warm water, between euryterm species (analyses own field data according to method main components) Cold-water species Warm-water species Euryterm species

With respect to their origin native gelatinous species belong to moderately cold-water species: the ctenophore Pleurobrachia pileus, scyphomedusa Aurelia aurita, and the pyrophyte alga Noctiluca scintillans. Two warm water invasive ctenophores arrived and established in upper layer Cold water species Warm water species Subdivision of the gelatinous species in their relation to mean seasonal, annual and minimal winter SST: analyses of field data according to main component method )

Noctiluca scintillans increased abundance in late 1970s (eutrophication and cold period) Aurelia aurita increased abundance in late 1970s (eutrophication and cold period) Ctenophore Mnemiopsis leidyi arrived in 1982 and its huge population development started in 1988 (eutrophication and warm period) ctenophore Beroe ovata arrived and its development started around the sea in 1999 (warm period) Chronolody of the gelatinous species blooms

Vertical distribution Noctiluca scintillansAurelia aurita Mnemiopsis leidyi and Beroe ovata Termocline P. pileus

Interannual Mnemiopsis leidyi and surface water temperature variabilities in the Black Sea B.ovata In spring In summer Mnemiopsis leidyi Beroe ovata

? Map of first Mnemiopsis leidyi findings

Shiganova et al, in preparation Beroe ovata Beroe cucumis Beroe forskalii Beroe gracilis

Haplotype distribution and frequency map for Mnemiopsis leidyi. Allele (inner circle for ITS) and haplotype (outer donut for COI) distribution map of Mnemiopsis leidyi. Each color indicates a different allele/haplotype. Private alleles/haplotypes are highlighted in grey (Ghabooli et al.2013).

Morphological differences of M. leidyi individuals from the Black, Azov, Caspian and Aegean seas Upper row of our data below after Mayer (1912). Black Sea Sea of AzovAegean Sea М.leidyi M.gardeni M.mccradyi

Phenological stages of M.leidyi and B.ovata After Shiganova et al., 2000, 2003; Vinogradov et al.,

Seasonal distribution of M.leidyi and B.ovata larvae in warm (2001) and cool (2003) year Shiganova et al., 2000, 2003; Vinogradov et al.,

Expansion of gelatinous species from the Mediterranean Sea Rhopilema nomadica Cassiopea andromeda Cassiopea andromeda (2008) Chrysaora hysoscella Chrysaora hysoscella (2002) Cotylorhiza tuberculata Chrysaora hysoscella (2009) Bolinopsis vitrea (2009) Shiganova, Ozturk,2010; Ozturk, Shiganova,2010

Mnemiopsis leidyi Beroe ovata Bolinopsis vitrea Pleurobrachia pileus

Aurelia aurita Rhisostoma pulmo Chrysaura hysoscella Native species Possible invader

Conclusion During the last three decades, first native than invasive gelatinous species have become the main drivers of the Black Sea ecosystem functioning subjected to ecosystem disturbance With respect to their origin, all the Black Sea species may be subdivided into cold water (boreal) warm-water, eurythermal (Mediterranean species). Correspondingly, their spatial and vertical distribution, seasonal dynamics, and phenology depend on their origin. Three native gelatinous species belong to moderately cold- water species: the ctenophore Pleurobrachia pileus, scyphomedusa Aurelia aurita Warm water invader Mnemiopsis leidyi arrived and established in the upper layer of the Black Sea, where there was not any predator or gelatinous competitor. It could reach high abundance at optimal upper layer temperature in high prey concentration. Its predator warm water species Beroe ovata established in the same upper layer in conditions of high M.leidyi concentrations. According to indicator of GES abundance M.leidyi and A.aurita >5 ind.m-3 is characterizated as bloom and “bad environmental status”