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Ba cterial si ngle- c ell approaches to the relationship between diversity and function in the S ea. EVK3-CT2002-00078 November 2002 - October 2005. Marine Biodiversity Cluster Meeting - Brussels-July’03. Image: K. Jürgens. 1 µm. Roundicoccus southamptii. Dalibacter - PowerPoint PPT Presentation
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BaBacterial cterial sisingle-ngle-ccell ell approaches to the approaches to the relationship between relationship between diversity and function diversity and function in the in the SSeaea
Marine Biodiversity Cluster Meeting - Brussels-July’03Marine Biodiversity Cluster Meeting - Brussels-July’03
EVK3-CT2002-00078EVK3-CT2002-00078November 2002 - October 2005November 2002 - October 2005
1 µm1 µm
Image:
K. Jü
rgens
The project’s ultimate goalThe project’s ultimate goal
Roundicoccus Roundicoccus southamptiisouthamptii
TinymonasTinymonas bremenensisbremenensis
Dalibacter Dalibacter banyuleusbanyuleus
(all names are fiction)(all names are fiction)
SpirovibrioSpirovibrio kalmariensiskalmariensis
75% of BCD75% of BCD
dominates dominates DMSP uptakeDMSP uptake
preferentiallypreferentiallygrazed by HNFgrazed by HNF
very sensitivevery sensitiveto viral attackto viral attack
C) Single-cell approachesC) Single-cell approaches
linkagelinkageB) Bacterial diversityB) Bacterial diversity
A) Bacterial biogeochemical A) Bacterial biogeochemical functionfunction
BaBacterial cterial sisingle-ngle-ccell ell approaches to the approaches to the relationship between relationship between diversity and function diversity and function in the in the SSeaea
By developing new methodologies, sampling By developing new methodologies, sampling different European seas and through laboratory and different European seas and through laboratory and mesocosm experiments, we will address the main mesocosm experiments, we will address the main objectives of BASICS:objectives of BASICS:
The identification of the most important prokaryotic organisms associated with the
biogeochemical functioning (in the carbon and sulfur cycling) of the sea, through the development of single-cell analysis techniques applied to pelagic microbes. BASICS will also study how resilient the
link is between the diversity and the C and S biogeochemical cycling by bacterioplankton, in the face of the most important global environmental changes expected in European coastal waters.
Objective 1: To describe bacterioplankton diversity in the coastal seas of Europe
Objective 2: To describe the seasonal changes in the cycling of carbon and sulfur mediated by planktonic bacteria in surface waters of European coastal seas
Objective 3: To design, test and fine-tune different methods and research strategies for the single-cell analysis of natural bacterioplankton organisms
Objective 4: To link bacterial diversity and biogeochemical function (in the cycles of C and S) and identify the bacterial phylotypes responsible for the crucial steps in oceanic biogeochemical cycling, and to refine recently developed conceptual frameworks for the links between species richness (number of dominant coexisting species) and biogeochemical cycling
Objective 5: To estimate the effect of environmental changes affecting the ocean’s bacterially-mediated biogeochemical function, global bacterial diversity and the link between bacterial diversity and C and S cycling
-) Why bacteria ?-) Why bacteria ?A) Why bacterial diversity ? A) Why bacterial diversity ? B) Why biogeochemical function ?B) Why biogeochemical function ?
• • why the C cyclewhy the C cycle• • why the S cyclewhy the S cycle
C) Why study the linkage ?C) Why study the linkage ?D) The key: Single-Cell methodsD) The key: Single-Cell methodsE) Project organizationE) Project organizationF) Project partnershipF) Project partnership
• • The sampling sitesThe sampling sites• • A few of the first resultsA few of the first results
• • Most of Earth’s living biomassMost of Earth’s living biomass• • Most abundant living particles in the seaMost abundant living particles in the sea• • Only significant DOM transformers Only significant DOM transformers • • Responsible for most of ocean’s respirationResponsible for most of ocean’s respiration• • Largest living surface in the oceanLargest living surface in the ocean
• • The largest “unknown pool” of genomic and The largest “unknown pool” of genomic and metabolic (i.e. functional) diversitymetabolic (i.e. functional) diversity
Bacteria are...Bacteria are...
• • bacteria play far more important ecological roles in naturalbacteria play far more important ecological roles in natural environments than their small sizes would suggest (Brock environments than their small sizes would suggest (Brock et al.’88) • “L’essentiel est invisible pour les yeux” (Antoine et al.’88) • “L’essentiel est invisible pour les yeux” (Antoine de Saint-Exupéry)de Saint-Exupéry)• “• “small is beautiful !”small is beautiful !”
Chis
holm
20
00
-) Why bacteria ?-) Why bacteria ?A) Why bacterial diversity ? A) Why bacterial diversity ? B) Why biogeochemical function ?B) Why biogeochemical function ?
• • why the C cyclewhy the C cycle• • why the S cyclewhy the S cycle
C) Why study the linkage ?C) Why study the linkage ?D) The key: Single-Cell methodsD) The key: Single-Cell methodsE) Project organizationE) Project organizationF) Project partnershipF) Project partnership
• • The sampling sitesThe sampling sites• • A few of the first resultsA few of the first results
Trying to make VISIBLE what is invisible
BacteriaBacteria
ArchaeaArchaea
Stéphan Daigle National Geographic
Pure culture
GenesProteinsActivity
Molecular biology
Hey, it’s me !
SYSTEM CULTURABILITY (%)
Marine 0.001 - 0.1
Freshwater 0.25
Mesotrophic lake 0.1 - 1
Estuary 0.1 - 3
Activated sludge 1 - 15
Sediments 0.25
Soil 0.3
Culturing native prokaryotesCulturing native prokaryotes
Are these few isolated bacteria relevant in plankton biogeochemistry ?Are these few isolated bacteria relevant in plankton biogeochemistry ?
Overview of techniques in molecular Overview of techniques in molecular ecologyecology
Species compositionFingerprinting
DGGE ARDRA T-RFLP
Cloning and sequencing
Bulk nucleic acid extract
Quantitative rRNA hybridization
Microbial biomass
Sea water microbes
Biomass collection
In situ hybridization Detection
single cells
Nucleic acid extraction
DNA reassociation kineticsDNA cross-hybridization Abundance
some phylotypes
Comparison among
communities
PCR amplification
PCR productComparison
among communities
Fingerprinting: lmw RNA
BASICS partners will follow the BASICS partners will follow the seasonality of bacterial diversity in seasonality of bacterial diversity in several sites in the North, several sites in the North, Mediterranean and Baltic Seas and the Mediterranean and Baltic Seas and the English ChannelEnglish Channel
We will use a variety of techniques:We will use a variety of techniques:
- fingerprinting techniques (DGGE, T-RFLP, SSCP...)- fingerprinting techniques (DGGE, T-RFLP, SSCP...)- detection of single phylotypes/groups (FISH)- detection of single phylotypes/groups (FISH)- cloning and sequencing- cloning and sequencing- culture isolation- culture isolation
• • Describe seasonality in “diversity” (what is there, who’s Describe seasonality in “diversity” (what is there, who’s the most abundant)the most abundant)
• • Usage of different techniques (fingerprinting &clon Usage of different techniques (fingerprinting &clon libraries & isolation...)libraries & isolation...)
• • Common frameworkCommon framework• • Characterization of isolatesCharacterization of isolates• • Biotechnological exploitation of the isolatesBiotechnological exploitation of the isolates
Objective 1: To describe bacterioplankton diversity in the coastal seas of Europe
The BactLibThe BactLib(Bacterial (Bacterial Culture database)Culture database)
The ecologically-The ecologically-referencedreferencedphylotype databasephylotype database
-) Why bacteria ?-) Why bacteria ?A) Why bacterial diversity ? A) Why bacterial diversity ? B) Why biogeochemical function ?B) Why biogeochemical function ?
• • why the C cyclewhy the C cycle• • why the S cyclewhy the S cycle
C) Why study the linkage ?C) Why study the linkage ?D) The key: Single-Cell methodsD) The key: Single-Cell methodsE) Project organizationE) Project organizationF) Project partnershipF) Project partnership
• • The sampling sitesThe sampling sites• • A few of the first resultsA few of the first results
To know the main To know the main routes of C circulationroutes of C circulationis a prerequisite... is a prerequisite...
... for understanding... for understandingthe fluxes of C in the oceanthe fluxes of C in the ocean
JGO
FS
It is the belief of BASICS that too muchIt is the belief of BASICS that too mucheffort has been put in the past in describingeffort has been put in the past in describingbacterial diversity in the ocean...bacterial diversity in the ocean...
... barely telling what the position and... barely telling what the position anddepth of the sample was...depth of the sample was...
How can we understand the role that specificHow can we understand the role that specificbacteria will play in nature then ???bacteria will play in nature then ???
Fig. 2.2. The feedback linking oceanic plankton and climate through the production of atmospheric sulfur. The original hypothesis postulated that production of dimethylsulfide (DMS) by phytoplankton, and its subsequent ventilation and oxidation in the atmosphere feeds cloud condensation nuclei in marine stratus, thereby increasing cloud albedo. If the consequent reduction in solar irradiance forced phytoplankton toproduce less DMS, then a negative feedback would operate, thus stabilizing climate. Recent advances suggest that it is not only phytoplankton but the whole food web (with bacteria playing a crucial role) that releases DMS.
- DMSP is a labile organic molecule which can represent 15% of - DMSP is a labile organic molecule which can represent 15% of BCD BCD and close to 100% of S demandand close to 100% of S demand- DMS participates in climate feedback- DMS participates in climate feedback
Kie
ne e
t al. 2
000
Kie
ne e
t al. 2
000
BASICS partners will follow the BASICS partners will follow the seasonality of microbial seasonality of microbial biogeochemical cycling in several sites biogeochemical cycling in several sites in the North, Mediterranean and Baltic in the North, Mediterranean and Baltic Seas and the English ChannelSeas and the English Channel
We will measure a large We will measure a large amount of stocks and rates:amount of stocks and rates:
- Bulk DOC and nutrients- Bulk DOC and nutrients- Algal activity and biomass- Algal activity and biomass- Viral and protozoan stocks and activity- Viral and protozoan stocks and activity- DMS and DMSP stocks and rates- DMS and DMSP stocks and rates- etc.- etc.
• • Seasonal studies in C and S cyclingSeasonal studies in C and S cycling• • Key biogeochemical steps little studiedKey biogeochemical steps little studied
Objective 2: To describe the seasonal changes in the cycling of carbon and sulfur mediated by planktonic bacteria in surface waters of European coastal seas
Ocean Projects in IGBP II
BASICSBASICS
-) Why bacteria ?-) Why bacteria ?A) Why bacterial diversity ? A) Why bacterial diversity ? B) Why biogeochemical function ?B) Why biogeochemical function ?
• • why the C cyclewhy the C cycle• • why the S cyclewhy the S cycle
C) Why study the linkage ?C) Why study the linkage ?D) The key: Single-Cell methodsD) The key: Single-Cell methodsE) Project organizationE) Project organizationF) Project partnershipF) Project partnership
• • The sampling sitesThe sampling sites• • A few of the first resultsA few of the first results
Nitrate
Phyto
Zoop
P-Z-N Dynamics: Populations Change through TimeP-Z-N Dynamics: Populations Change through Time
PhytoplanktonPhytoplankton
ZooplanktonZooplankton
T. M
ichaels
Does it matter what biology is hidden within each box?Does it matter what biology is hidden within each box?
Phyto
DiatomsPrasinophytesPrymnesiophytes
ProchlorococcusSynechococcus
Phyto
T. M
ichaels
PhytoPhyto
ZooZoo
Dynamic Green Ocean Model
Buitenhuis et al. 2003
N2 fixersDMS
producers
coccolith.Nano
phytoplankton
Fe NO3Si
CaCO3
PO4 NH4
DOM
diatoms
Biogeochemical fluxes are a function of community structureBiogeochemical fluxes are a function of community structure
Bacteria & Nutrients
Stays Suspended
Sinking Particle
s
Pico-Phyto
Nano-Phyto
Micro-Phyto
Micro-Zoo
Meso-Zoo
Bacteria & Nutrients
Sinking Particles
SALPS
T. M
ichaels
1 mm
salp
euphausiid
copepod
Fecal PelletsD
. S
tein
berg
Bacteria are abundant and importantBacteria are abundant and important
ButBut
We are unable of grouping them in We are unable of grouping them in biogeochemically relevant and biogeochemically relevant and distinctdistinct““boxes”boxes”
we don’t know whether they all do the same, or we don’t know whether they all do the same, or not...not...
BecauseBecause
• • Multistep strategyMultistep strategy• • Coocurrence analysis (Synthesis workshop !)Coocurrence analysis (Synthesis workshop !)• • Design of oligonucleotide probesDesign of oligonucleotide probes• • Test of BGQ function in isolatesTest of BGQ function in isolates• • Test during an experimental algal bloomTest during an experimental algal bloom
• • Each approach is partial and has some risk of failureEach approach is partial and has some risk of failure
Objective 4: To link bacterial diversity and biogeochemical function (in the cycles of C and S) and identify the bacterial phylotypes responsible for the crucial steps in oceanic biogeochemical cycling, and to refine recently developed conceptual frameworks for the links between species richness (number of dominant coexisting species) and biogeochemical cycling
-) Why bacteria ?-) Why bacteria ?A) Why bacterial diversity ? A) Why bacterial diversity ? B) Why biogeochemical function ?B) Why biogeochemical function ?
• • why the C cyclewhy the C cycle• • why the S cyclewhy the S cycle
C) Why study the linkage ?C) Why study the linkage ?D) The key: Single-Cell methodsD) The key: Single-Cell methodsE) Project organizationE) Project organizationF) Project partnershipF) Project partnership
• • The sampling sitesThe sampling sites• • A few of the first resultsA few of the first results
• • Flow cytometry sorting: standarization & controlsFlow cytometry sorting: standarization & controls• • FISH improvementsFISH improvements• • Combination of techniques: MicroFISH, MicroACT, etc...Combination of techniques: MicroFISH, MicroACT, etc...• • Capillary electrophoresisCapillary electrophoresis• • X-Ray microanalysisX-Ray microanalysis• • .... ???.... ???
Objective 3: To design, test and fine-tune different methods and research strategies for the single-cell analysis of natural bacterioplankton organisms
The power is in the combination of methodsThe power is in the combination of methods
Hybridized
DAPI-stained
Fluorescence in situ Hybridization:("phylogenetic staining")
Environmental sample
Extracted nucleic acidsDNA rRNA
rDNA clonesNucleic acid probe
rDNA Sequences
rDNAdatabase
Comparative Analysis
Hybridization Sequencing
MPIMMMPIMM
DAPI + AU
Roseobacter + AU
MicroFISH
35S DMSP
ICMICM
Cottrell & Kirchman 2000Cottrell & Kirchman 2000
HMW-DOMHMW-DOM
LMW-DOMLMW-DOM
CytophagaCytophaga
-Proteobacteria-Proteobacteria
-Proteobacteria-Proteobacteria
% a
ctiv
e c
ells
% a
ctiv
e c
ells
% cells in sample
0
20
40
60
0 20 40 60
Protein
C C
0
20
40
60
0 20 40 60
Aminoacids
C CAtlanticAtlanticOceanOcean
Cell sorting by FCM
Further analyses of sorted fractions
* Activity (radioactivity)* Identification* Isolation* Chemical analyses (C; N; P,….)
PrelabelingRadioactive substratesNucleic acid probesPhysiological probes
Laser(488 nm)
Trash
FACSCalibur FACSVantageHigh speed cell sorter
OOBOOB
PML/SOC/MPIMMPML/SOC/MPIMM
Blu
e fl
uore
scence
(D
NA
)
103
102
Threshold101
100 101 102 103
Red fluorescence (protein)
Flow Citometry
DMSP producing phytoplankton bloom in the North SeaEmiliania huxleyi y Prorocentrum minimum
FISH
Roseobacter
Cytophaga/Flavovacterium
SAR86
Zubkov et al. 2001Zubkov et al. 2001
PML/SOC/MPIMMPML/SOC/MPIMM
Abundance highly correlated with
DMSP consumption
Capillary electrophoresis
Sample
Data recording
+ -Power Supply
Inlet buffer reservoir Outlet buffer reservoir
Absorbance detector
Capillary
Basic scheme
NIOZNIOZ
Protein separation
Sample
Injection
Separation
Detection
Detection window
UV absorbance
SDS+
---
+++
++ +
+
+-
-
- --
- -
-
- -
-
-
-
-
+
+
+
+
NIOZNIOZ
• • Functional redundancy, ecosystem stability...Functional redundancy, ecosystem stability... ... effects of env. change on ... effects of env. change on
- diversity- diversity- BGQ function- BGQ function- their linkage- their linkage
• • Environmental perturbations in microcosmsEnvironmental perturbations in microcosms
Objective 5: To estimate the effect of environmental changes affecting the ocean’s bacterially-mediated biogeochemical function, global bacterial diversity and the link between bacterial diversity and C and S cycling
-) Why bacteria ?-) Why bacteria ?A) Why bacterial diversity ? A) Why bacterial diversity ? B) Why biogeochemical function ?B) Why biogeochemical function ?
• • why the C cyclewhy the C cycle• • why the S cyclewhy the S cycle
C) Why study the linkage ?C) Why study the linkage ?D) The key: Single-Cell methodsD) The key: Single-Cell methodsE) Project organizationE) Project organizationF) Project partnershipF) Project partnership
• • The sampling sitesThe sampling sites• • A few of the first resultsA few of the first results
WP 4: SCA method developmentWP1: Seasonal studies of bacterial diversity
WP3: Seasonal studies of biogeochemical C & S cycling
WP7: Functional stability of the link facing global change
WP6: Experimental determination of the factors that regulate the link between bacterial diversity and function
WP5: Linking bacterial diversity with biogeochemical function
WP2: Explotaition of phylotypes and isolate information
WS0: Coordination
WS1: Synthesis WS on bacterial diversity in coastal european seas and C & S cycling
WS3: Synthesis WS on SCA
WS5: Summary
Phase 1
Phase 2
Phase 3
WS2: Mesocosm experiment
WS4: Microcosm experiments
WP2:WP2:ExploitationExploitation
WP6:WP6:Factors regulateFactors regulate
WP5: WP5: LinkingLinking
WP7:WP7: Funct. stabil.Funct. stabil.
WP3:WP3:C/S-CyclingC/S-Cycling
WP1:WP1:DiversityDiversity
WP4:WP4: SCA devSCA dev
-) Why bacteria ?-) Why bacteria ?A) Why bacterial diversity ? A) Why bacterial diversity ? B) Why biogeochemical function ?B) Why biogeochemical function ?
• • why the C cyclewhy the C cycle• • why the S cyclewhy the S cycle
C) Why study the linkage ?C) Why study the linkage ?D) The key: Single-Cell methodsD) The key: Single-Cell methodsE) Project organizationE) Project organizationF) Project partnershipF) Project partnership
• • The sampling sitesThe sampling sites• • A few of the first resultsA few of the first results
BarcelonaBarcelonaBanyulsBanyuls
TexelTexel
KalmarKalmar
ToulouseToulouseVillefrancheVillefranche
SouthamptonSouthampton
BergenBergen
BremenBremen
PlymouthPlymouth
BarcelonaBarcelona Pep Gasol / Rafel SimóPep Gasol / Rafel Simó
BanyulsBanyuls Philippe LebaronPhilippe Lebaron
TexelTexel Gerhard HerndlGerhard Herndl
KalmarKalmar Åke HagströmÅke Hagström
ToulouseToulouse Pascal BordatPascal Bordat
VillefrancheVillefranche Markus WeinbauerMarkus Weinbauer
SouthamptonSouthampton Mike Zubkov / Peter BurkillMike Zubkov / Peter Burkill
BergenBergen Frede Thingstad / Mikal HeldalFrede Thingstad / Mikal Heldal
BremenBremen J. Pernthaler / B. FuchsJ. Pernthaler / B. Fuchs
PlymouthPlymouth Steve ArcherSteve Archer
-) Why bacteria ?-) Why bacteria ?A) Why bacterial diversity ? A) Why bacterial diversity ? B) Why biogeochemical function ?B) Why biogeochemical function ?
• • why the C cyclewhy the C cycle• • why the S cyclewhy the S cycle
C) Why study the linkage ?C) Why study the linkage ?D) The key: Single-Cell methodsD) The key: Single-Cell methodsE) Project organizationE) Project organizationF) Project partnershipF) Project partnership
• • The sampling sitesThe sampling sites• • A few of the first resultsA few of the first results
• Shelf = 20% of Ocean NPP; supports 90% of Marine Fisheries Production
• Coastal population = 2.2 billion (40% of total)
(Jackson et al. 2001)
Before fishingAfter fishing
• Nutrient inputs microbialization of food chains
Sampling sitesSampling sites
• • Blanes Bay (ICM)Blanes Bay (ICM)• • Banyuls - MOLA & MILA station (OOB)Banyuls - MOLA & MILA station (OOB)• • Baltic proper landsort (UNIK)Baltic proper landsort (UNIK)• • North Sea Texel site (NIOZ)North Sea Texel site (NIOZ)• • Villefranche point “B” (LOV)Villefranche point “B” (LOV)• • L4 English Channel station (PML & SOC)L4 English Channel station (PML & SOC)• • Helgoland site G (MPIMM)Helgoland site G (MPIMM)
General characteristics of Blanes BayGeneral characteristics of Blanes Bay
• Typical Mediterranean waters: warm, salty and nutrient-poor• Typical Mediterranean waters: warm, salty and nutrient-poor
• Oligotrophic coastal system (annual average chlorophyll of 0.5 µg l• Oligotrophic coastal system (annual average chlorophyll of 0.5 µg l -1-1) )
• Relatively unaffected by human or freshwater influence• Relatively unaffected by human or freshwater influence
• Separated from oceanic waters by a southwest current associated with • Separated from oceanic waters by a southwest current associated with a front in the continental slope (10-20 miles offshore)a front in the continental slope (10-20 miles offshore)
• Episodic intrusions of oceanic waters caused by the Blanes canyon• Episodic intrusions of oceanic waters caused by the Blanes canyon
Half mile from
harbour
Depth of 20 m
ICMICM
Seasonality of Seasonality of phytoplanktonphytoplankton
Main peak of chlorophyll Main peak of chlorophyll aa during late winter, during late winter, driven by high driven by high atmospheric pressures atmospheric pressures together with irradiances together with irradiances and temperatures higher and temperatures higher than similar latitudes in than similar latitudes in the Atlanticthe Atlantic
ICMICM
5•10•12•14•17•23•27•35•40•34•33•48•54•13•28•36•31•38•18•22•41•43•50•24•49•2227512192531118262932293941Dec97Jan Feb AprJun Jul SepOctNovDec Mar
3 September
2July
29 July
9 October
4 November
1 Desember
26 March
29 April
3 June
27 January
22 Desember 97
25 February
5 February
12 February
19 February
3 March
18 March
11 March
1.0
SummerFall
Spring
Winter
Seasonal succession of Seasonal succession of
bacterioplanktonbacterioplankton
ICMICM
Temporal dynamics of bacterial Temporal dynamics of bacterial groups and populationsgroups and populations
ICMICM
Four sites 70 km appartFour sites 70 km appart
One sample for seasonOne sample for season
Comparison of bacterial composition Comparison of bacterial composition
by DGGEby DGGE
How representative is the Blanes site?How representative is the Blanes site?
CO
Blanes-Jul
Blanes-Nov
Masnou-Jul
Barcelona-Jul
Masnou-Nov
Blanes-Jan
Blanes-Apr
Masnou-Apr
Barcelona-Apr
Harbour-Jan
Masnou-Jan
Barcelona-Jan
Barcelona-Nov
CC
Harbour-Apr
Harbour-Jul
Harbour-Nov
1.0
Summer
Winter
Spring
ICMICM
PML/SOC seasonal sampling site
Time series station since 1988(Roger Harris and PML Zooplankton group)
Measurements: (weekly throughout the year)
•Environmental: Chl a, Temp, Salinity, Optics, POC, PON
•Biological: Phytoplankton, Zooplankton, Bacteria, Viruses
•Processes: Primary production (FRRF), Calanus egg production, L4 location:
Western English ChannelPML/SOCPML/SOC
-) Why bacteria ?-) Why bacteria ?A) Why bacterial diversity ? A) Why bacterial diversity ? B) Why biogeochemical function ?B) Why biogeochemical function ?
• • why the C cyclewhy the C cycle• • why the S cyclewhy the S cycle
C) Why study the linkage ?C) Why study the linkage ?D) The key: Single-Cell methodsD) The key: Single-Cell methodsE) Project organizationE) Project organizationF) Project partnershipF) Project partnership
• • The sampling sitesThe sampling sites• • A few of the first resultsA few of the first results
MPIMMMPIMM
Horseradish-peroxidase-labeled FISH probes and catalyzed reporter deposition (CARD)
(tyramide signal amplification, TSA)
HRP
protein
fluorescently labeled tyramide
Signal AmplificationPermeabilization
HRP
HRP HRP
Hybridization
MPIMMMPIMM
Sediment
Surface
water
Exposure time:
10 seconds 1 second
10 seconds 1 second
conventional FISH
FISH & signal amplification
MPIMMMPIMM
G2 EuryarchaeaDAPI-staining
Euryarchaeota in coastal North Sea surface waters
Coastal North Sea, % detection by FISH
Month
03 05 07 09 11 01
Probe detection rate [% of total cells]
0
10
20
30
40
50
G2-Euryarchaeota
MPIMMMPIMM
And still, other unplanned BASICS returns...And still, other unplanned BASICS returns...
• • Development and optimization of molecular tools Development and optimization of molecular tools (useful with other microorganisms and in other (useful with other microorganisms and in other ecosystemsecosystems
• • Better knowledge of the spatial and temporal scales of Better knowledge of the spatial and temporal scales of bacterial biodiversity changesbacterial biodiversity changes
• • Applicability of the “key species” concept to bacteriaApplicability of the “key species” concept to bacteria• • Autoecology of bacteriaAutoecology of bacteria• • Indicator bacterial species of ecosystem perturbationsIndicator bacterial species of ecosystem perturbations• • Biotechnological exploitation of effort made at the Biotechnological exploitation of effort made at the
“pure science” (knowledge for its own sake) level“pure science” (knowledge for its own sake) level•• ......
Single-cell approachesSingle-cell approaches
linkagelinkageBacterial diversityBacterial diversity
Bacterial biogeochemical Bacterial biogeochemical functionfunction
BaBacterial cterial sisingle-ngle-ccell ell approaches to the approaches to the relationship between relationship between diversity and function diversity and function in the in the SSeaea
www.icm.csic.es/bio/projects/basicswww.icm.csic.es/bio/projects/basics