INTERACTING EFFECTS OF PHYSICAL DISTURBANCE AND …vm277wt9615/... · This study tested the effects...
Transcript of INTERACTING EFFECTS OF PHYSICAL DISTURBANCE AND …vm277wt9615/... · This study tested the effects...
1"
INTERACTING EFFECTS OF PHYSICAL
DISTURBANCE AND OCEAN
ACIDIFICATION STRESS ON THE
CALIFORNIA MUSSELS, MYTILUS
CALIFORNIANUS
Andrew B Hines
Hopkins Marine Station
May 2014
2"
Interacting effects of physical disturbance and ocean acidification stress on the California mussel, Mytilus californianus
An Honors Thesis Submitted to
the Department of Biology in partial fulfillment of the Honors Program
STANFORD UNIVERSITY
Andrew Hines May 2013
3"
Acknowledgments Two years is a long time to work on an undergraduate thesis, and as the time
passed, it became increasingly easy to rationalize giving up, falling back on personal
hardship as an excuse to turn in, switch off, and hide. But for the grace and support of my
advisor, Fio Micheli, I would have never had the strength to finish this document. Every
word is a product of that support, of Fio’s tireless care and intelligent comments, keeping
me going through a two-year period that saw me finish this thesis and regain the joys of
being a scientist. Fio, together with the stats acumen of Jim Watanabe, the fieldwork of
Cheryl Butner, and the comments of Steve Palumbi, have made my time at Hopkins a
growing experience. I owe a debt of gratitude (an in one case, pastries) to all those who
have aided me in this endeavor, but it is with the utmost gratitude that I thank Fio, Steve,
Jim, and Cheryl.
To my friends Ana Guerra, Chelsea Wood and Jen Cole, whose stories and beers
and theories-on-the development-of-vampirism-in-reality are some of my fondest
memories, I offer thanks. I will miss our late-night conversations and early-morning
dives/dances. I would also like to thank Francesco Ferretti, Ashley Greenley, Kristy
Kroeker, Sarah Lummis, Steve Litvin, and Paul Leary; Fiolab has been as a family to me,
teaching me more than any classroom.
I would also like to acknowledge the wonderful staff of Hopkins Marine Station;
Doreen Zelles, Freya Sommer, John Lee, Chris Patton, Joe Wible, Don Kohrs, and of
course, Judy Thompson, who keep our little world spinning.
4"
Abstract One of the main impacts of human carbon dioxide emission is the decline of
oceanic pH. The concomitant reduction in carbonate ion concentration has proven
deleterious to range of calcareous marine species, many of which are also subject to
habitat loss and disturbance due to human exploitation of the coast. Here, I examined the
interaction of pH and dislodgement stress on the California mussel, Mytilus
californianus. First, pH was found to be the dominant stress affecting growth; however,
due to pseudoreplication, a second experimental run was conducted, which suggested that
pH and disturbance act synergistically to reduce growth rates. Further analysis
determined that pH and disturbance did not significantly differ between experiments, but
that potential compensatory effect had been acting in the tanks: increased pCO2 in tank
water may have allowed mussels to offset the metabolic demand of hypercapnia and
byssogenesis. These results highlight the difficulty of simulating the intertidal
environment in a controlled fashion and the necessity of continued study of compound
stress effects for the management of coastal resources under climate change.
5"
Table of Contents Introduction ....................................................................................................................... 6
Materials and Methods ..................................................................................................... 8
Tank setup ....................................................................................................................... 9
Analysis ........................................................................................................................... 9
Results .............................................................................................................................. 11
Discussion ......................................................................................................................... 12
Magnitude of treatment levels ....................................................................................... 12
Implications and Future work ....................................................................................... 14
References ........................................................................................................................ 16
Tables ................................................................................................................................ 19
Figures .............................................................................................................................. 20
6"
Introduction Recent research has shown that human activities are driving large-scale rapid
change in the oceans through multiple co-occurring stressors (Pachauri 2007, Halpern et
al. 2008, Rockström 2009). Rising atmospheric CO2 results in the oceanic uptake of CO2
(Doney 2010). This carbonate pump is governed by the following equations,
CO2(aq) + H2O ↔ H2CO3 ↔ H+ + HCO3- ↔ H+ + CO3
2- (1)
Ca2+ + 2HCO3- ↔ CaCO3 + CO2 + H20 (2)
An increase in atmospheric CO2 results in elevated oceanic bicarbonate ion concentration
(HCO3-) and hydrogen ions (H+) and a decrease in the concentration of carbonate ion
(CO32-) (Gattuso & Buddemeier 2000). Thus, influx of CO2 into seawater drives a shift in
the inorganic carbon equilibrium, from a CaCO3 precipitating environment, towards a
carbonate ion (CO32-) limited one (Zondervan et al. 2001).
The overall effect of this process is termed Ocean acidification, and has been
shown to affect marine species both positively and negatively, via several mechanisms
(adapted from Kroeker et al. 2010): (1) increased pCO2 and HCO3-, (2) decreased pH,
and (3) decreased CO32- concentration. An increase in pCO2 and HCO3
- concentrations is
expected to benefit some marine autrotrophs by allowing increased photosynthetic
efficiency (Hurd et al. 2009). Decreased pH is expected to induce hypercapnia in marine
heterotrophs, which in turn results in metabolic depression (Langenbuch & Pörtner
2004). The regulation of extracellular pH is an energetically intensive process, and OA-
induced hypercapnia may force energetic trade-offs between growth and homeostatic
maintenance (Pörtner et al. 2004). Finally, CO32- is required to form the calcium
carbonate (CaCO3) shells used by many marine species. In a carbonate ion limited
environment, calcification rates will likely decrease while the rate of dissolution of
calcium carbonate increases (Kleypas et al. 1999, Gattuso & Buddemeier 2000, Orr et al.
2005).
However, the responses of marine calcifiers to hypercapnic conditions are
intensely variable (Ries et al. 2009, Kroeker et al. 2010). Some species respond by
reducing growth rates while others, such as the blue mussel, Mytilus edulis thrive even in
acidic (hypercapnic) conditions (Kroeker 2010). Multiple hypotheses accounting for this
7"
variation in biological response have been proposed, but they all treat ocean acidification
(OA) as the dominant stressor. The resilience of Mytiloids to hypercapnia is due to their
metabolism and feeding ecology (Thomsen et al. 2010, Melzner et al. 2011) thus,
introducing disturbance as an additional component of stress creates a more realistic
stress regime, which targets mussel’s energy allocation mechanisms rather than their
shells alone. While lowered pH can be an important factor in the calcification rates of
marine mollusks (Gazeau et al. 2007), it is not the sole factor in the intertidal
environment.
Crain et al. [2008] found that stressors such as lowered pH and dislodgement can
be additive, synergistic, or antagonistic in combination. These categories, originally
described by Folt et al. [1999] are defined as follows: two stressors with negative
impacts, “A” and “B” are applied to an organism, and result in reduced amounts “a” and
“b”, respectively. This negative response is a reduction from the normal value being
measured, e.g. growth rate, and can be characterized as additive (response = a + b),
antagonistic (response < a + b), or synergistic (response > a + b) (Folt et al. 1999, Crain
et al. 2008). This classification provides a useful system for determining the forcing
stresses in an organism’s environment, and which are dominant. Given that the individual
effects of both acidification and trampling have been observed in marine intertidal
ecosystems (Thomsen et al. 2010, Melzner et al. 2011, Brosnan & Crumrine 1994), it is
important that we understand how they act together. Trampling mussels can remove
individuals from the substrate, and reattachment after dislodgment is an energetically
intensive process (Brosnan & Crumrine 1994). The combined impact of lowered pH on
calcification, and the energetic demand of byssogenesis, could result in altered energy
allocation, reduced growth rates, and decreased survival of individuals (Wood et al. 2008,
Kroeker et al. 2010). Furthermore, if lowered pH and dislodgement were found to
simultaneously depress the metabolic rate of a mussel, resulting in a reduced growth rate
(when compared to the effect of only pH, or only disturbance), they may be additive.
However, if the effect of pH alone overshadows that of dislodgement and pH combined,
pH stress would be the dominant force in mussel growth dynamics.
8"
This study tested the effects of physical dislodgement and acidification on
mussels. Dislodgment (from trampling and wave action) and ocean acidification have
tremendous impacts on coastal ecosystems singularly (Brosnan & Crumrine 1994,
Halpern et al. 2008), but are experienced by coastal organisms as discrete stressors.
California’s shores experience heavy traffic and, over the next 40 years, are projected to
experience a reduction in pH and CaCO3 to an average of 7.82 ± 0.04, and 1.26 ± 0.12,
respectively (Gruber et al. 2012) By subjecting the California mussel, Mytilus
californianus to both of these anthropogenic stressors, I attempted to gain a better
understanding of possible synergisms in nature, of which there is little information
(Darling & Coté 2008, Crain et al. 2008). I focused on two main questions, (1) how do
pH and dislodgement affect shell growth separately, and (2) when combined, are the
stressors additive, or is there a dominant mechanism that determines M. californianus
growth? I hypothesized that pH and disturbance treatments would have an additive
effect, reducing the somatic growth rate of mussels due to the energetic demands of
homeostasis.
Materials and Methods M. californianus is commonly found on the west coast of North America,
occurring in rocky intertidal zones from Mexico to Alaska. Hopkins Marine Station of
Monterey Bay lies near the southern edge of the range, and provided a large closed-
access population of mussels for this study. 200 mussels were haphazardly sampled from
one of the northern beds near China point (36°37’18’N, 121º54’19”W), during late July-
early August 2012 (Supplement A). Within the bed, mussels were selected for similar
length. Each mussel was cleaned of epibionts, measured for initial length and width using
digital calipers (Supplement B) n=160, !! = 31mm SDL= 3.9mm, !! = 15mm,
SDW=1.9mm), then tagged. Using a random number generator, mussels were assigned to
one of 4 treatment bins, 20 mussels to a bin. An additional group of mussels was assigned
to mesh bags staked in the sampled plots to create an external control. All subjects were
kept in a fasting state during the experiment, with no food administered other than the
particulates generated in the tanks. As tanks were a common resource, with multiple
experiments and species sharing space, subjects were housed in modified open-top
9"
Tupperware containers (10x10x8cm, with grit-tape bottoms). Two mesh bags of 20
individuals were staked in the intertidal using zip ties and steel bolts, but were
subsequently found ripped open, with all mussels missing, on 10 August.
The entire experiment was replicated across two samples of mussels, for a total of
8 treatment bins, two of each pH and disturbance combination (Figure 8). After a one-
week acclimation period, experimental treatments began, and were administered weekly
(Supplement C). Disturbance treatments involved complete removal of an individual’s
byssus complex via wrenching from the substrate (plastic Tupperware tub with grit-tape),
while pH treatments were constant in the tanks. Measurements of mussel growth were
taken monthly (Supplement B and C) and required the exposure of each treatment group
to air for 30 minutes to 1 hour, during which time length and width was measured for
each individual. Immediately post-measurement, mussels were returned to their
treatments.
Tank setup
All experiments were conducted in the Aquaria complex of Hopkins Marine Station. Two
separate pH tanks were constructed (Figure 9) and filled with seawater from Monterey
Bay Aquarium to a depth of 8cm. Tank water temperature and dissolved oxygen were
measured continuously during the experiment using an AADI 4500a sensor. Tank pH
was measured as ion voltages using Honeywell durafet sensor, then converted to pH
using the following equation (calibrated 8/10/12 and 8/12/12 respectively by HMS staff):
!": !"!"#$%&' !!!! − !! (3)
where !"!"#$%&' !is the measured value, and ! and ! are probes-specific corrections.
Experimental pH values were set by the pH of incurrent water from the Monterey Bay
Aquarium (pH = 7.75 ± 0.05), and the approximated ambient pH of Monterey Bay (pH =
7.95).
Analysis
To determine the effect of pH-Disturbance treatment combinations, I compared the post-
treatment surface areas of each mussel to its pre-treatment value. As a baseline for
comparison, the Undisturbed and High pH (UH) treatment group was chosen. If pH and
10"
Disturbance had a negative effect on growth rate, the UH treatment should exhibit the
highest growth. Surface area measurements were taken monthly, and included removal
of subjects from treatment tubs, and recording of length and width. For a three-
dimensional shell, measurements of the longitudinal axis (length) and latitudinal axis
(width) were used to approximated the surface area of a mussel as the combined surface
area of two simple ellipses:
!"#$%&'!!"#$! !.!. = !2!"# (4)
Where ! is the latitudinal axis, and ! is the longitudinal axis. Lacking a third dimension,
and given the mathematical complexity of calculating the surface area of an ellipsoid, the
above method was deemed sufficient.
The effect of pH and disturbance was calculated as the incremental growth
response ratio !:
! = (!!!!!)!!
! (5)
Where !! is the final surface area, and !! is the initial (pre-treatment) surface area. The
response ratio quantified the incremental change resulting from experimental
manipulations. A positive response ratio indicated the treatment had a positive effect on
growth, while a negative value indicated a negative effect; a value of zero indicated no
effect.
Initial comparison of the variance in growth ratios was conducted using twin 2-
way Factorial ANOVAs, (Model I), with pH and Disturbance as fixed, orthogonal
factors, one for each experimental run. Variation in the growth rate among treatment
combinations across samples was tested with a 4-way Model II ANCOVA, with pH and
Disturbance as orthogonal fixed factors, initial surface area as a covariate, and sample
group as a random factor nested within pH and disturbance, after tests for normality and
homogeneity of variance. Due to the random nature of the sample groups, I used a Model
II (Mixed) effects model to calculate the overall mean effect for each stressor variable. A
mixed model accounted for the variation in treatment response due to the different
sample groups, as they were nested within tanks, while still allowing me to determine the
experimental variation due to my treatments. Mixed effects models account for this
variation by calculating the between group variance of the nested factor !"!"!"#$ and
weighting the significance of each experimental variable according to that term.
11"
Results The observed variation in growth rates of M. californianus exposed to low pH and
dislodgement did not support the hypotheses that these stressors have a negative impact
on mussels, nor did it provide conclusive evidence that ocean acidification and physical
dislodgment are synergistic or additive stressors. During the first trial (sample 1), growth
variation of experimentally manipulated mussels differed significantly among treatments
(Table 1). Analysis of variance of sample group 1 found only pH to be a significant factor
(2-way factorial ANOVA; pH: F(1,73)=5.75, P<0.01). Growth was greatest in the
Disturbed and Low pH group (Figure 1), suggestive of a synergistic effect of the two
stressors. Mussels in the Undisturbed treatments (undisturbed-low pH, UL, and
undisturbed-high pH, UH) and in the Disturbed and High pH treatment (DH) were found
to have a mean growth ratio significantly less than the Disturbed-low pH (DL) treatment,
but were not significantly different from each other. To determine if the positive effect of
pH in Sample group 1 was a treatment effect, and not an artifact of pseudo-replication of
pH tanks, a second experimental run was conducted (Figure 1, Sample 2). Sample Group
2 exhibited markedly different responses to the treatments compared to sample 1, with
the highest mean growth occurring in the UL treatment; lowest mean growth occurred in
the High pH treatments (UH and DH). However, growth rates were not significantly
different among these treatments. The interaction of pH and Disturbance was found to be
significant (Table 2); however, in contrast with sample 1, growth was lower when both
treatments were applied together, suggestive of an antagonistic effect (Figure 1).
The opposing trends found in each experimental run indicated that additional
confounding factors were affecting the growth of mussels. To account for those
confounding factors, Sample group was added to the model as a random, nested factor
(within pH and Disturbance treatments), with initial surface area included as a covariate.
However, because the effect of initial size was found not to be significant (3-way
ANCOVA F(1,4)=0.43, P=0.55), this factor was removed. ANOVA indicated that only
the nested term of sample group was significant (4-factor Model II ANCOVA;
F(4/156)=6.23, P<0.001; Table 3. When the two experiment runs were combined, the
effects of treatments were no longer significant. Due to the opposite effects of treatments
in the two experimental runs, interaction plots of treatments and growth rates were
12"
generated to determine whether treatments had a positive or negative overall effect,
within each sample group. Decreased pH was found to have a positive effect on growth
(Figure 2). The effect of Disturbance was both positive (sample 2) and negative (sample
1), and indicated an additional interaction (Figure 3). The interaction of pH and
Disturbance was found to have a positive effect in sample 1, and a negative effect in
sample 2; mussels in UH treatments grew less than mussels in DH treatments, while
mussels in DL treatments grew less than those in UL treatments (Figure 4). In addition,
the difference in mean growth ratio of DH and DL mussels in sample group 2 was five
times that of sample group 1.
Discussion My results do not offer conclusive evidence of a positive or negative effect of pH
or Disturbance. Furthermore, due to the highly variable treatment responses and the
resulting non-significance of each factor, it is impossible to determine whether or not pH
or Disturbance act synergistically, additively, or antagonistically. Thus, while low pH
appears to have an overall positive effect on mussel growth, further experiments are
needed to assess the significance of this effect and whether it interacts with dislodgement
disturbance. However, the variation of effects prompted by just two stressors illuminates
the complex nature of modeling forces in the intertidal. The results of this experiment are
limited due to pseudoreplication (only one ambient and one low pH tank were available).
Magnitude of treatment levels
The response of growth ratio to low pH appeared to be positive, and thus contradictory to
the established literature on ocean acidification, which contends that reduced pH shifts
the oceans from CaCO3 deposition to dissolution (Zondervan et al. 2001). Given the non-
significance of pH in my analysis, increased growth of mussels in the UL and DL
treatments suggests that the reduction in pH may have resulted in a separate,
compensatory reaction. While not directly measured, it is possible the increased CO2
concentration in the waters boosted algal growth (Ries et al. 2009, Kroeker et al. 2010)
providing an uncontrolled source of nutrients to offset the metabolic strain of
13"
hypercapnia. An increase in pyhtoplanktonic photosynthesis could buffer the negative
effect of ocean acidification on calcification (Ries et al. 2009, Kroeker et al. 2010).
However, growth in the High pH tanks was only marginally different from the Low,
indicating an even simpler explanation: pH treatments were biologically within M.
californianus tolerances. In particular, the pH values used in this experiment differed by
0.2 points, and were not constant (Figure 5).
Mytilus edulis, a close relative of M. californianus, was found to be unaffected by
pH as low as 7.4 (Berge et al. 2006). In designing my experiment, I referred to the work
of Michaelidis et al. [2005] who described declines in growth and metabolic activity
under hypercapnic conditions. During periods of hypercapnia, mussel shell growth was
reduced due to an increase in homeostatic energy expenditure (Thomsen & Melzner
2010, Matsuhiro & Miyashita 2004). In response to hypercapnia, energy expenditure
rose 58% above control level (Michaelidis et al. 2005, Thomsen et al. 2010). Thomsen et
al hypothesized that decreased shell growth was a consequence of higher energy demand
and existing energy re-allocation in a lowered pH system. The mussels must expend
more energy in ion regulation, and overcome essential nitrogen limitation brought on by
increased protein turnover. If the pH stress overcomes the mussels’ capacity to restore
somatic tissue, increased energy must be put into maintenance of existing tissue, resulting
in lower shell growth rate.
However, this work differed greatly from previous studies by measuring the
change in surface area rather than shell thickness or shell weight, both of which are
thought to be a more likely to respond to pH stress than overall reduction of growth rate
(Bamber 1990). In fact such mechanisms could still have been occurring in my
experiment, as a reduction in respiration rates (as measured by Michaelidis et al. [2005])
could imply a decrease in the interpallial pCO2, and therefore an increased ability to fix
CaCO3 (Gazeau et al. 2007). Thus, even mussels exposed to lowered pH could maintain
growth rate, if they reduced overall metabolic rate. This compensatory effect is
compounded if the mussels are able to feed, which would allow them to maintain their
metabolic rate and continue to grow (Thompsen & Melzner 2007). Even if the pH was
well below the norm, as long as they’re feeding, the mussels can maintain homeostasis
and continue to grow, as demonstrated by Thompsen & Melzner [2007].
14"
The compensatory effect of feeding, combined further obfuscates the effect of
disturbance. Disturbance treatments used in this study were determined from the work of
Brosnin & Crumrine [1994], who analyzed the effect of trampling and physical damage
on intertidal communities. I simulated the effect of human trampling and wave action on
mussels as a wrenching force that removed the mussels from the substrate, and destroyed
the plaque of the byssus complex. I reasoned that byssogenesis would be prioritized in
the intertidal, but neglected any size or age-based variation in byssal strength. To
maintain balance in my analysis, I avoided further damage to the shells, focusing only on
the energetics of byssogenesis while neglecting to standardize the force applied to the
mussels during treatment.
Experiments by Babbarro et al. [2007] suggest an additional metabolic strategy
available to Mytiloids in the management of byssogenesus, strategies that invalidate my
singular measurements of growth. Babarro and his colleagues found that fasting adult
mussels were able to maintain byssus secretion and attachment strength via the “transfer
of energy between soft tissues and byssus under stress,” resulting in rapid reattachment
and mobility. Since the secretion and strength of byssus threads is known to respond to
environmental flow rate (Lee 1990, Babbarro et al. 2007), and the water of the tanks
circulated without significant force, byssus destruction presented no real stress. Thus, the
manner and frequency of disturbance meted out in my treatments is also a poor estimate
of the conditions found in the intertidal. If the mussels could feed on particulates in the
tanks, and byssus secretion in a slow-flowing tank is not metabolically taxing, weekly
disturbances that left the shell intact could not compare to the millennia of waves and
storms survived by the mussel’s evolutionary precursors.
Implications and Future work
While non-significant on their own, the results of these experiments provide useful
preliminary data for future work on interacting stress effects. In particular, further work
should include a careful selection of stressors, both obvious, like water temperature
(Rodolfo-Metalpa et al. 2011), and nuanced, such as water flow-rate (Babarro et al.
2007) as well as greater depth of measurement. The molecular and physiological aspects
of stress responses offer important insights into organismal coping strategies, like those
15"
of Mytilus edulis (Melzner et al. 2010), and cannot be approximated with a single
measurement. Finally, the results of this experiment highlight the importance of
determining realistic stress parameters; my experiments were inconclusive due to
marginal levels of pH and disturbance, which proved inconsistent as stressors. Both
realistic and extreme values should be considered; recent experiments by Gruber et al.
[2012] have concluded that the California Current System is rapidly approaching pH and
aragonite (a form of CaCO3) saturation levels “well outside the natural range,” with
“frequent or even persistent under-saturation conditions.” The true effect of OA cannot
be accurately modeled without multiple pH levels that span the natural and worst-case
IPCC scenarios. In addition, while boosted algal growth may have sustained the mussels
in this experiment, the evidence is mounting that OA will have a negative impact on
global phytoplankton populations (Boyce et al. 2010, Hofmann et al. 2011). Marine
phytoplankton is the basis for the oceanic food web, and can provide a buffer against the
stress of life in the oceans. Without that buffer, mussels are fighting a losing battle; as go
the phytoplankton, so goes everyone else.
16"
References 1. Babarro, et al., Secretion of byssal threads and attachment strength of Mytilus
galloprovincialis: the influence of size and food availability, J. Mar. Bio. Assoc.
UK, 88.04 (2008)
2. Bamber, R. N., The effects of acidic seawater on 3 species of lamellibranch
mollusc, J. Exp. Mar. Biol. Ecol., 143 (1990)
3. Berge, et al., Effects of increased sea water concentrations of CO2 on growth of
the bivalve Mytilus edulis L, Chemosphere, 62 (2006)
4. Boyce, D. G., et al. Global phytoplankton decline over the past century.
Nature 466 (2012)
5. Brosnan, D, Crumrine, L., Effects of human trampling on marine rocky shore
communities, J. Exp. Mar. Bio. Ecol., 177, (1994)
6. Crain, C. Kroeker, K. & Halpern, B. Interactive and cumulative effects of
multiple human stressors in marine systems, Ecol. Lett, 11, (2008)
7. Darling, S. & Coté, I. Quantifying the evidence for ecological synergies, Ecol.
Lett. 11, (2008)
8. Doney, S.C. et al., Ocean acidification: the other CO2 problem, Annu. Rev. Mar.
Sci., 1, (2009)
9. Doney, S.C., The Growing Human Footprint on Coastal and Open-Ocean
Biogeochemistry, Science, 328, (2010)
10. Folt, C.L., et al. Synergism and antagonism among multiple stressors. Limnol.
Oceanogr., 44, (1999)
11. Turley, C.M. et al., Novel microcosm system for investigating the effects of
elevated carbon dioxide and temperature on intertidal organisms, Aqua Bio, 3,
(2008) DOI:10.3354/ab00061
12. Gazeau, F. et al. Impact of elevated CO 2 on shellfish calcification. Geophysical
Research Letters, 34, (2007).
13. Gattuso J.P. & Buddemeier R.W., Ocean biogeochemistry: Calcification and
CO2. Nature, 407 (2000)
14. Gruber, Nicolas, et al., Rapid progression of ocean acidification in the California
Current System." Science 337 (2012)
17"
15. Halpern, B. et al., A Global Map of Human Impact on Marine Ecosystems,
Science, 319, (2008) DOI: 10.1126/science.1149345
16. Hoegh-Guldberg, O. & Bruno, J., The Impact of Climate Change on the World’s
Marine Ecosystems, Science, 328, (2010) DOI: 10.1126/science.1189930
17. Hoegh-Guldberg, O. et al., Coral reefs under rapid climate change and ocean
acidification, Science, 318, (2007) DOI: 10.1126/science.1152509
18. Hofmann et al., Declining ocean chlorophyll under unabated anthropogenic
CO2 emissions, Environ. Res. Lett 6 (2011) doi:10.1088/1748-9326/6/3/034035
19. Hurd C.L., et al. (2009). Testing the effects of ocean acidification on algal
metabolism: Considerations for experimental designs. J. Phyc., 45 (2009)
20. Kleypas J.A., et al. Geochemical consequences of increased atmospheric CO2 on
coral reefs. Science 284 (1999)
21. Kroeker, K. J. et al., Meta-analysis reveals negative yet variable effects of ocean
acidification on marine organisms, Eco. Lett., (2010). DOI: 10.1111/j.1461-
0248.2010.01518.x.
22. Langenbuch M. & Pörtner H.O. High sensitivity to chronically elevated CO2
levels in a eurybathic marine sipunculid. Aquatic Toxicology, 7 (2004).
23. Lee C.Y., Shirley S.L. and Owen M.D., The rate and strength of byssal
reattachment by blue mussels (Mytilus edulis L.), Can. J. Zoo., 68, (1990)
24. Matsushiro A., Miyashita T., Evolution of hard-tissue mineralization: comparison
of the inner skeletal system and the outer shell system, J. Bone. Miner. Metab. 22
(2004) 25. Michaelidis B. et al., Effects of long-term moderate hypercapnia on acid–base balance and growth
rate in marine mussels Mytilus galloprovincialis, Mar Ecol Prog Ser 293 (2005)
26. Melzner F, et al., Food Supply and Seawater pCO2 Impact Calcification and
Internal Shell Dissolution in the Blue Mussel Mytilus edulis, PLoS ONE 6 (2011)
27. Orr J.C., et al., Anthropogenic ocean acidification over the twenty-first century
and its impact on calcifying organisms. Nature, 437 (2005)
28. Pachauri, R., Climate Change 2007: Synthesis Report, IPCC Secretariat, Geneva,
(2007)
29. Thomsen, J. & Melzner, F., Calcifying invertebrates succeed in a naturally CO2
enriched coastal habitat but are threatened by high levels of future acidification,
18"
Biogeosci. Dis. 7 (2010)
30. R Core Team, R: A language and environment for statistical computing. R
Foundation for Statistical Computing, Vienna,Austria. (2014), URL
http://www.R-project.org/.
31. Ries, J. B., Cohen, a. L., & McCorkle, D. C., Marine calcifiers exhibit mixed
responses to CO2-induced ocean acidification, Geology 37 (2009)
DOI:10.1130/G30210A
32. Rockstrom, J. et al., A safe operating space for humanity, Nature, 461, (2009).
URL: http://dx.doi.org/10.1038/461472a
33. Rodolfo-Metalpa, R. et al. Coral and mollusc resistance to ocean acidification
adversely affected by warming. Nature Climate Change 1.6 (2011)
34. Wood H.L., Spicer J.I. & Widdicombe S., Ocean acidification may increase
calcification rates, but at a cost. Proc. Roy. Soc. B. 275, (2008)
35. Wootton, T.J et al. Dynamic patterns and ecological impacts of declining ocean
pH in a high-resolution multi-year dataset Proc. Nat. Acad. Sci. 105 (2008)
36. Zondervan, Ingrid, et al., Decreasing marine biogenic calcification: A negative
feedback on rising atmospheric pCO2, Glo. Biogeochem. Cyc. 15.2 (2001)
19"
Tables
Table 1: 2-way Factorial ANOVA, group 1 Source df SS MS F value P pH_1 1 0.001750 0.0017496 5.746 0.0191 Disturbance_1 1 1 0.000224 0.0002240 0.736 0.3938 Interaction (P:D) 1 0.000520 0.0005201 1.708 0.1953 Within 73 0.022227 0.0003045
Table 2: 2-way Factorial ANOVA, group 2 Source df SS MS F value P pH_2 1 0.00355 0.003552 7.739 0.5418 Disturbance_2 1 0.00003 0.000034 0.075 0.9455
Interaction (P:D) 1 0.00462 0.004624 10.077 0.0022 Within 76 0.03488 0.000459 Table 3: 3 way Mixed Model ANOVA, groups 1&2 Source df SS MS F value P Initial Surface Area 1 0.00103 0.00103 0.43130 0.54589
pH 1 0.00509 0.00509 2.13293 0.21795
Disturbance 1 4.67E-05 4.67E-05 0.01966 0.89554
Interaction (P:D) 1 0.00102 0.00102 0.42740 0.54895
Sample group S(P:D) 4 0.00955 0.00239 6.23206 0.00012
Within 149 0.05710 0.00038 Total 156
20"
Figures
0
0.01
0.02
0.03
0.04
0.05
0.06
0.07
UL UH DH DL UL UH DH DL
Sample 1 Sample 2
Gro
wth
Rat
io
Treatment and Experimental Groups
Incremental Growth ratio in M. californianus
Figure 1: Mean Incremental Growth Ratio across all treatments and sample groups, with calculated Error bars (mean ± 1 SE). Treatment combinations are color-coded by Disturbance level and pH combination: blue for the Undisturbed/Low (UL); red for Undisturbed/High (UH); green for Disturbed/Low (DH); purple for Disturbed/Low (DL). Experimental runs identified by sample group number, e.g. 1 = sample group 1, 1st experiment. Y-axis is the Incremental growth rate, a dimensionless ratio given by equation 5.
21"
0.025
0.030
0.035
0.040
0.045
0.050
∆Growth ratio by pH treatment
pH level
Mea
n G
row
th ra
tio
High Low
Figure 2: Interaction plot of the change in Mean growth ratio across pH Treatments, with error bars (mean ± 1 SE). Experimental runs indicated by line type, e.g. hashed line is Sample 1, while the, solid line is Sample 2. Here, the lines indicate the difference in growth ratio between pH treatments for each sample run, while slope indicates the magnitude of the change, e.g. the positive slope indicates a higher growth ratio in the Low pH treatments of both samples 1 and 2. However, mussels of sample 2 had higher mean growth ratios (than sample 1) for both treatments, and exhibited a greater magnitude of positive response to pH than those of sample 1.
22"
0.025
0.030
0.035
0.040
0.045
∆Growth ratio by Disturbance treatment
Disturbance level
Me
an
Gro
wth
ra
tio
Disturbed Undisturbed
Figure 3: Interaction plot of change in Mean Growth ratio across Disturbance treatments, error bars (mean ± 1 SE). Experimental runs indicated by line type, here the hashed line is Sample 1, and the solid line is Sample 2. The interaction plot visualizes broad trends across treatments, and is useful in primary comparisons among treatments, and in the determination of numerical treatment effects. Here, the Disturbed treatment had a positive effect on growth ratio in Sample 2, but a negative effect in Sample 1; however, the magnitude of the positive effect on growth seen in sample 2 is less than the magnitude of the negative effect observed in sample 1.
23"
0.02
0.03
0.04
0.05
0.06
Sample group 1
pH level
Mea
n G
row
th ra
tio
High Low
0.02
0.03
0.04
0.05
0.06
Sample group 2
pH level
Mea
n G
row
th ra
tio
High Low
Effects of pH and Disturbance on Growth ratio
Figure 4: Interaction plot of the change in Mean Growth ratio across pH levels, by Disturbance treatment (Sample runs 1 & 2) with error bars (mean ± 1 SE). Disturbed treatments indicated by hashed line; undisturbed treatments given by solid line. Here, the effect of pH and Disturbance resulted positive growth in sample 1, as well as positive and marginally negative growth in sample 2. In sample 1, growth ratio was higher (meaning greater net growth) in the disturbed and low pH treatments, though both disturbance/pH combinations resulted in growth. In contrast, sample 2 exhibited a greater growth ratio increase in low pH and undisturbed treatments, while disturbed treatments across pH levels were not significantly different.
24"
Figure 5: pH variation during the experiment. Ambient pH is in blue, low pH is in red. Due to the type of pH manipulation (the incurrent water was acidic, and raised to the ambient level via bubbling) the variation in High (ambient) pH is negligible, while the pH of MBA water fluctuated semi-monthly.
25"
High pH Undisturbed
Sample group 1 Undisturbed
Sample group 2 Disturbed
Sample group 1 Disturbed
Sample group 2
Low pH
Undisturbed Sample group 1
Undisturbed Sample group 2
Disturbed Sample group 1
Disturbed Sample group 2
Figure 6: Diagram of the Experimental Setup. Large boxes are pH tanks, color-coded boxes represent factorial treatment combinations and replicate experiments.
26"
Figure 9: pH tank construction. Water flow is set to two liters per minute, through two spigots; one spigot sends the water through 30m of drip irrigation tubing, which is submerged in the reservoir tank of the water from the other system forming a simple heat exchanger. The other spigot sends the water to a 1.2 X 0.8 X 1.6 meter reservoir where an air pump connected to a soaker hose bubbles air into the tank. The surface water from this tank then gravity feeds into a 1.2 X 0.7 X 1 meter reservoir; the water is pumped at 3.8 liters per minute to the top of a column 2.4m tall by 0.27m diameter filled with BioSpheres. This column drains back into the same reservoir. The surface water from this reservoir then gravity feeds to the experiment trough.
27"
Supplement A: Sampling Dates Group 1: originally sampled 16/7/12, finish 17/9/12 Group 2: originally sampled 10/8/12, finish 14/9/12 Group 3: originally sampled 17/8/12, finish 21/9/12
removed from experiment due to loss of subjects B. Measurement Protocol Before recording any measurements, 3 mussels were measured to calibrate the calipers. Length
Align the less-curved side of mussel parallel to the calipers, and slowly close the calipers until they just touch the mussel. This measurement attempts to capture the distance from umbo to edge of the mussel, and requires that the umbo touch the base of the calipers (i.e. instead of measuring from the hinge, measure from one-side of the hinge, to get the absolute length.
Width
Position the mussel such that the overall curve of the shell us upward (away from you). Clear the shell of debris and position the lower arm of the caliper on the leading edge of the shell. Close the calipers until the top arm touches the shell, to get absolute width.
28"
C. Treatment/measurement timeline Date(dd/m/yy) Event Treatments Color code
27/8/12 Disturb Group 1 Disturbed/ High No colors Disturbed/ Low
31/8/12 Disturb Group 2 Disturbed/ High Red/white Disturbed/ Low
3/9/12 Disturb Group 1 Disturbed/ High No colors Disturbed/ Low
7/9/12 Disturb Group 2 Disturbed/ High Red/white Disturbed/ Low
10/9/12 Disturb Group 1 Disturbed/ High No colors Disturbed/ Low
14/9/12 Measure Group 2 Dist./ High Red/white Dist. /Low Undist./ High Undist./ Low
17/9/12 Measure Group 1 Dist./ High No colors Dist./ Low Undist./ High Undist./ Low
21/9/12 Measure Group 3 Both Bags (red bags, pick 20 and measure them)
No colors