a novel approach to estimating active carbon flux using ...€¦ · _`abcd efghij klmn = q o + q p...

1
Oceans play a critical role in global carbon cycling. The process known as the biological carbon pump involves the synthesis of organic matter by phytoplankton at the ocean’s surface and its subsequent transport to the deep ocean via: 1. Passive carbon transport via gravitational settling of organic particles, and 2. Active carbon transport via vertical migrations of zooplankton and micronekton feeding in the epipelagic at night and residing in the mesopelagic during the day. Methodology • Depth stratified (0-100 and 550- 650 m) diel sampling using three different trawl types off the southwest coast of Oahu, Hawaii (Fig. 1) • Size dependent equations obtained from the literature for respiration, mortality, excretion and gut flux to be used in biomass/production size dependent model (Box 1). A Novel Approach to Estimating Active Carbon Flux Using the Biomass Size Spectra Lian Kwong 1 ([email protected]), Brian Hunt 1,2 ([email protected]) and Evgeny Pakhomov 1,3 ([email protected]) Department of Earth, Ocean and Atmospheric Sciences UBC 1 , Hakai Institute 2 , Institute for the Oceans and Fisheries UBC 3 , BC, Canada Total micronekton migrant biomass: • Based on the biomass size spectra model: 7796.5 mgC m -2 • Based on catch: 543.5 mgC m -2 (7% of biomass spectra estimate) Active carbon transport: • Based on the biomass size spectra model: 105 mgC m -2 day -1 • Based on catch: 17.6 mgC m -2 day -1 (17% of biomass spectra estimate) Conclusions • The biomass spectra approach provides a promising tool for predicting active carbon flux, particularly at the community level. • In combination with the use of multiple gears, the biomass spectra may potentially reduce net sampling bias associated with avoidance by larger micronekton. • Previous estimates of active carbon flux may have underestimated the contribution of zooplankton and micronekton to global carbon cycling by up to an order of magnitude. • While time at depth can be estimated using global acoustic data sets, gut flux requires further investigation to decrease model uncertainty. • Combining this model with acoustic methods may improve predictions of regional and global active carbon fluxes. Main Objectives 1. Develop biomass size spectra for the day and night in the mesopelagic zone and for the night in the epipelagic zone 2. Estimate total migratory micronekton biomass 3. Develop a biomass/production size dependent model based on the biomass spectra theory to quantify active carbon Fig 1. Sampling locations by trawl type on the southwest coast of Oahu, Hawaii. Trawl Mouth (m 2 ) Mesh (mm) Cobb 140 10 HUFT 4 3 IKMT 3 5 Fig 4. Biomass size spectra expressed as the log-transformed relationship between average abundance (individuals m -2 ) of against carbon weight (mg) for organisms ranging from 20 to 100 mm in length. Box 1. Biomass/production size dependent modelling. References: 1. Blanco et al. 1994. Scientia Marina 58(1-2):17- 29. 2. Ikeda. 1985. Mar. Biol. 85:1-11. 3. Pakhomov et al. 1996. Mar. Ecol. Prog. Ser.134(1-3):1-14. 4. Peterson and Wroblewski. 1984. Can. J. Fish. Aquat. Sci. 41:1117-1120. 5. Steinberg et al. 2000. DSR 1 47(1):137-158. Acknowledgements: This project is funded by an NSERC Discovery grant for Dr. Evgeny A. Pakhomov and an Australian Research Council (ARC) grant. Fig 4. Locations of past studies assessing active carbon flux. It should be noted that the depth of export is not portrayed in this figure. Current estimates of active carbon transport focus primarily on individual species/ groups or certain fluxes. Whole communities and all four fluxes (respiration [R], excretion [E], gut flux [G] and mortality[M]) are not often considered. Table 1. Results of the sensitivity analysis as percent change in the carbon flux rate from the epipelagic to mesopelagic for perturbation in individual parameters. Results b = Slope of the biomass size spectra W Ni = Nominal size class (carbon (CW Ni ) or dry (DW Ni ) weight) representing each size bin W i = Lower limit of the size class N WNi = Abundance of individuals in a given nominal size class N(w) B(CW Ni ) = Abundance of individuals by carbon or dry weight = Biomass in a given nominal size class T = Environmental temperature ( o C) RO CWNi = Respiratory rate of oxygen uptake for a given nominal size class RQ = Respiratory quotient (0.97) R(CW Ni ) = Respiratory carbon equivalent for a given nominal size class ISF Ni = Index of stomach fullness GPT Ni = Gut passage time for a given nominal size class G(CW Ni ) = Gut flux for a given nominal size class E(CW Ni ) = Excretion rate for a given nominal size class TD = Time at depth (hours) CR HM(DW Ni ) = Carbon weight to dry weight ratio for data set = Hourly mortality rate for a given nominal size class M(DWNi) = Mortality rate for a given nominal size class ! = Total community respiration " = Total community gut flux # = Total community excretion $ = Total community mortality Biomass Size Spectra 1 Standing Stock Abundance Respiration 2 !"#$ %& '( = 0.5254 + 0.8354 ∗ !"45 67 + 0.0601: #(45 67 ) = #$ %& '( ∗ #= ∗ > ?@ @@.A B C D = E(F & '( ∗ #(45 67 )) 6 7G? Excretion 3 H(45 67 )=# 67 ∗ 0.31 I D = E(F & '( ∗ H(45 67 )) 6 7G? Mortality 5 JK(L5 67 )= M5.26 ∗ 10 NO PQR N? S ∗ L5 67 NT.@U 24 ℎWXYZ K(45 67 ) = [(45 67 ) ∗ JK(L5 67 ) ∗ :L ∗ 4# \ D = E K(L5 67 ) 6 7G? Gut Flux 4 ](45 67 ) = 45 67 ∗ 0.15 ∗ ^_`a '( bc def '( gb h ?TT i D = F & '( ∗ ](45 67 ) 6 7G? F & '( = F(l)Pl 7 7 m? nopqrs tuvwxy z{|} = C D +\ D +I D +i D 5 67 =5 7 ^ 2 ~m? −1 (2 − 1)(Ä + 1) h ? ~ Parameter Perturbation -40% -20% -10% -5% 5% 10% 20% 40% Index of stomach fullness 17 9 4 2 -2 -4 -9 -17 Gut passage time -29 -11 -5 -2 2 4 7 12 Gut flux 17 9 4 2 -2 -4 -9 -17 Respiratory oxygen 16 8 4 2 -2 -4 -8 -16 Respiratory carbon 16 8 4 2 -2 -4 -8 -16 Daily mortality 6 3 2 1 -1 -2 -3 -6 Mortality 6 3 2 1 -1 -2 -3 -6 Excretion 4 2 1 0 0 -1 -2 -4

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Page 1: A Novel Approach to Estimating Active Carbon Flux Using ...€¦ · _`abcd efghij klmn = Q o + Q p + q Q + Q r 5 67 =5 7 V N stu ID (NID)(v^D) X u s b = Slope of the biomass size

Oceans play a critical role in global carbon cycling. The process known as the biological carbon pump involves the synthesis of organic matter by phytoplankton at the ocean’s surface and its subsequent transport to the deep ocean via:

1. Passive carbon transport via gravitational settling of organic particles, and

2. Active carbon transport via vertical migrations of zooplankton and micronekton feeding in the epipelagic at night and residing in the mesopelagic during the day.

Methodology• Depth stratifi ed (0-100 and 550-

650 m) diel sampling using three different trawl types off the southwest coast of Oahu, Hawaii (Fig. 1)

• Size dependent equations obtained from the literature for respiration, mortality, excretion and gut fl ux to be used in biomass/production size dependent model (Box 1).

A Novel Approach to Estimating Active Carbon Flux Using the Biomass Size Spectra

Lian Kwong1 ([email protected]), Brian Hunt1,2 ([email protected]) and Evgeny Pakhomov1,3 ([email protected])Department of Earth, Ocean and Atmospheric Sciences UBC1, Hakai Institute2, Institute for the Oceans and Fisheries UBC3, BC, Canada

Total micronekton migrant biomass:• Based on the biomass size spectra model: 7796.5 mgC m-2

• Based on catch: 543.5 mgC m-2 (7% of biomass spectra estimate)Active carbon transport:

• Based on the biomass size spectra model: 105 mgC m-2 day-1 • Based on catch: 17.6 mgC m-2 day-1 (17% of biomass spectra estimate)

Conclusions• The biomass spectra approach provides a promising tool for predicting active carbon

fl ux, particularly at the community level. • In combination with the use of multiple gears, the biomass spectra may potentially

reduce net sampling bias associated with avoidance by larger micronekton.• Previous estimates of active carbon fl ux may have underestimated the contribution of

zooplankton and micronekton to global carbon cycling by up to an order of magnitude. • While time at depth can be estimated using global acoustic data sets, gut fl ux

requires further investigation to decrease model uncertainty. • Combining this model with acoustic methods may improve predictions of regional and

global active carbon fl uxes.

Main Objectives1. Develop biomass size spectra for the day and night in the mesopelagic zone and for the night in the epipelagic zone

2. Estimate total migratory micronekton biomass 3. Develop a biomass/production size dependent model based on the biomass spectra theory to quantify active carbon

Fig 1. Sampling locations by trawl type on the southwest coast of Oahu, Hawaii.

Trawl Mouth (m2) Mesh (mm)Cobb 140 10HUFT 4 3IKMT 3 5

Fig 4. Biomass size spectra expressed as the log-transformed relationship between average abundance (individuals m-2) of against carbon weight (mg) for organisms ranging from 20 to 100 mm in length.

Box 1. Biomass/production size dependent modelling.

References: 1. Blanco et al. 1994. Scientia Marina 58(1-2):17-29. 2. Ikeda. 1985. Mar. Biol. 85:1-11. 3. Pakhomov et al. 1996. Mar. Ecol. Prog. Ser.134(1-3):1-14. 4. Peterson and Wroblewski. 1984. Can. J. Fish. Aquat. Sci. 41:1117-1120. 5. Steinberg et al. 2000. DSR 1 47(1):137-158.

Acknowledgements: This project is funded by an NSERC Discovery grant for Dr. Evgeny A. Pakhomov and an Australian Research Council (ARC) grant.

Fig 4. Locations of past studies assessing active carbon fl ux. It should be noted that the depth of export is not portrayed in this fi gure.

Current estimates of active carbon transport focus primarily on individual species/groups or certain fl uxes. Whole communities and all four fl uxes (respiration [R], excretion [E], gut fl ux [G] and mortality[M]) are not often considered.

Table 1. Results of the sensitivity analysis as percent change in the carbon fl ux rate from the epipelagic to mesopelagic for perturbation in individual parameters.

Results

Bio

mas

s Si

ze S

pect

ra

Stan

ding

Sto

ck A

bund

ance

Size

Dep

ende

nt R

ates

Respira

tion

!"#$%&

'(=0.5254+0.8354

∗!"45

67+0.0601:

#(4567)=#$%&

'(∗#=∗>12 22.4?

#@=A

(B&

'(∗#( 4567))

6 7CD

Excretion

E(4567)=# 6

7∗0.31

E@=A

(B&

'(∗E( 4567))

6 7CD

Mortality

( F5

67)=G2.196∗10I

J ℎID L∗:F

∗F567I

M.NO

PQ=A

(B&

'(∗P( F567)))

6 7CD

∗4#

GutFlux

R(4567)=STU 6

7∗10 V1 WX

R@=Y A

B&

'(∗R( 4567)

6 7CD

Z∗0.15

B&'(= ∫

B(\

)]\

7 7 ^D

_`abcdef

ghij

klmn=oQ

+pQ+qQ+rQ

567=5

7V

NstuID

( NID)( v^D)Xu s

b = Slope of the biomass size spectra WNi = Nominal size class (carbon (CWNi) or dry

(DWNi) weight) representing each size bin Wi = Lower limit of the size class NWNi = Abundance of individuals in a given

nominal size class N(w)

B(CWNi)

= Abundance of individuals by carbon or dry weight

= Biomass in a given nominal size class T = Environmental temperature (oC)

ROCWNi = Respiratory rate of oxygen uptake for a given nominal size class

RQ = Respiratory quotient (0.97) R(CWNi) = Respiratory carbon equivalent for a given

nominal size class ISFNi = Index of stomach fullness GPTNi = Gut passage time for a given nominal size

class G(CWNi) = Gut flux for a given nominal size class E(CWNi) = Excretion rate for a given nominal size

class TD = Time at depth (hours) CR

HM(DWNi)

= Carbon weight to dry weight ratio for data set

= Hourly mortality rate for a given nominal size class

M(DWNi) = Mortality rate for a given nominal size class ! = Total community respiration " = Total community gut flux # = Total community excretion $ = Total community mortality

Biomass Size Spectra1

Standing Stock Abundance

Respiration2

!"#$%&'( = 0.5254 + 0.8354 ∗ !"4567 + 0.0601:

#(4567) = #$%&'( ∗ #= ∗ > ?@@@.A

B

CD =E(F&'( ∗ #(4567))6

7G?

Excretion3

H(4567) = #67 ∗ 0.31

ID =E(F&'( ∗ H(4567))6

7G?

Mortality5

JK(L567) =M5.26 ∗ 10NOPQRN?S ∗ L567

NT.@U

24ℎWXYZ

K(4567) = [(4567) ∗ JK(L567) ∗ :L ∗ 4#

\D =EK(L567)6

7G?

Gut Flux4

](4567) = 4567 ∗ 0.15 ∗^_`a'(∗

bcdef'(

gbh

?TT

iD = ∑ F&'( ∗ ](4567)6

7G?

Standing Stock AbundanceF&'( = ∫ F(l)Pl7

7m?

nopqrstuvwxyz{|} = CD +\D + ID +iD

Biomass Size Spectra

567 = 57 ^2~m? − 1

(2 − 1)(Ä + 1)h

?~ Parameter

Perturbation -40% -20% -10% -5% 5% 10% 20% 40%

Index of stomach fullness 17 9 4 2 -2 -4 -9 -17 Gut passage time -29 -11 -5 -2 2 4 7 12

Gut flux 17 9 4 2 -2 -4 -9 -17 Respiratory oxygen 16 8 4 2 -2 -4 -8 -16 Respiratory carbon 16 8 4 2 -2 -4 -8 -16

Daily mortality 6 3 2 1 -1 -2 -3 -6 Mortality 6 3 2 1 -1 -2 -3 -6 Excretion 4 2 1 0 0 -1 -2 -4