Working Group on Net Community Production & Respiration Kendra - - PowerPoint PPT Presentation

working group on net community production respiration
SMART_READER_LITE
LIVE PREVIEW

Working Group on Net Community Production & Respiration Kendra - - PowerPoint PPT Presentation

Working Group on Net Community Production & Respiration Kendra Daly, USF Jason Lenes, USF Michael Murrell, EPA Brian Roberts, LUMCON John Walsh, USF Gary Hitchcock, UM Estuaries Shelf Oligotrophic DEFINITIONS GPP = Gross primary


slide-1
SLIDE 1

Working Group on Net Community Production & Respiration

Kendra Daly, USF Jason Lenes, USF Michael Murrell, EPA Brian Roberts, LUMCON John Walsh, USF Gary Hitchcock, UM

slide-2
SLIDE 2

Estuaries Shelf Oligotrophic

slide-3
SLIDE 3

DEFINITIONS

GPP = Gross primary production (all autotrophs) Rcom = community respiration (autotrophs + heterotrophs) NCP = GPP – Rcom NCP ≈ NPP – Rheterotrophs If NCP < 0, heterotrophic metabolic state allochthonous C source CO2 source If NCP > 0, autotrophic metabolic state

autochthonous C source

CO2 sink

slide-4
SLIDE 4

Rcom σ R GPP = ∫ Net Com Prod + ∫ Rcom

pycnocline

NCP NCP Stratified Shelf & Open Gulf Estuary depth CO2 CO2

slide-5
SLIDE 5

Estuaries: Open Water O2 Method

Δ O2 = (GPP – R) + Advection + (Air Sea Exchange)

slide-6
SLIDE 6

Estuary Comparison: open water method National Estuarine Research Reserve (Caffrey, 2003, 2004) Eastern Gulf of Mexico estuaries:  Limited seasonality in GPP, Rcom  SE estuaries are heterotrophic almost year-round  Southernmost estuaries have higher Rcom than temperate waters  Location (marsh, mangroves) and freshwater input (FWI) are determinants of metabolism heterotrophy

slide-7
SLIDE 7

Russell, M.J., and P. A. Montagna. 2007. Spatial and Temporal Variability and Drivers of Net Ecosystem Metabolism in Western Gulf of Mexico Estuaries.

Western Gulf of Mexico: Texas estuaries heterotrophy autotrophy Estuarine gradient in precipitation, freshwater inflows High GPP rates, balanced by high Rcom Spatial variability measured for correspondence of GPP, R Win Spr Sum Fall

slide-8
SLIDE 8

Gulf of Mexico Shelf Mississippi River: SW Pass Plume and Atchafalaya River Green et al., 2006

slide-9
SLIDE 9

Combined biological & physical models : Inverse and physical model:  Heterotrophic in winter (entire plume)  Spring to summer: autotrophic, progresses from SW Pass to west  Summer: NEM autotrophic with highest rates near SW Pass

Breed et al. 2004; Green et al., 2008

 Bacteria dominate plankton R in winter.

slide-10
SLIDE 10

 NCP from inorganic C mass balance model of plume  NCP maximum at salinity of 18 – 27  NCP rates of 1 – 9 g C m-2 d-1; global maxima for river plumes  Higher rates in spring-summer

Murrell et al. 2013

Guo et al. (2012)

slide-11
SLIDE 11

Murrell et al. (2013) Highest GPP, Rcom at < 30 m spring, summer Rcom in surface > bottom waters Rcom decreases east to west LA Shelf heterotrophic in west, offshore waters likely fueled by Miss River Org-C

slide-12
SLIDE 12

F2A C6C F5 C3 C9

F transect C transect

F1

Brian Roberts: LUMCON  Variable seasonal patterns

  • f Rcom, NCP

 Maximum Rcom near rAR mouth, in surface waters, declines offshore  Rcom proportional to DIN uptake

mmol O2 m-3 d-1

Atchafalaya River, 30% of MARS flow

  • B. Roberts - LUMCON
slide-13
SLIDE 13

West Florida Shelf: HABSIM Schematic of Carbon Flows

slide-14
SLIDE 14

West Florida Shelf (NCP, Rcom) Wanninkhof et al. (2007)

Hitchcock et al (2000)

West Florida Shelf (NCP, R) Karenia brevis - Hitchcock et al (2010; submit.) Spring 2007 FSLE Declining plankton ‘bloom’

18O2 GPP ≈ Rcom

2006 Bloom indicates

  • K. brevis autotrophic

No ‘seasonal’ progression

  • f auto to heterotrophic

Dense populations may be net heterotrophic

slide-15
SLIDE 15

Open Gulf Waters: Few NCP observations, low Rcom

Pomeroy et al., 1995

Pomeroy ‘95 Biddanda Benner 1997

 Few observations in oligotrophic GOM  Rcom in surface are relatively low  Current debate on metabolic state of oligotrophic waters

slide-16
SLIDE 16

Group Summary:

 GOM estuaries are predominantly heterotrophic, CO2 source to atmosphere (Cai, 2010)  Mississippi River Plume best characterized of all regions; intermediate salinity waters are autotrophic

 GOM Shelf and oligotrophic waters under-sampled

 Quantify NCP linkage to riverine nutrient and carbon sources, N fixation in open Gulf