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            <gco:CharacterString>Cite this dataset as: Baumann, H., Nye, J., Murray, C. S., Schwemmer, T., Molina, A. I., Cross, E. L. (2020) CO2, temperature, and oxygen effects on Atlantic silverside metabolic rates. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2020-11-10 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.827774.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>CO2, temperature, and oxygen effects on Menidia menidia metabolic rates Dataset Description: &amp;lt;p&amp;gt;This dataset includes metabolic rates of Atlantic silverside (&amp;lt;em&amp;gt;Menidia menidia&amp;lt;/em&amp;gt;) embryos and larvae reared in six separate experiments in 2016 and 2017. Four experiments used factorial combinations of CO₂ and temperature, and two experiments used combinations of CO₂ and oxygen.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Sampling and analytical procedures:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Detailed experimental methods are provided for experimental design and water chemistry in Murray and Baumann (2018) and Cross et al. (2019), and for respirometry methods in Schwemmer et al. (2020). In summary, spawning-ripe adult &amp;lt;em&amp;gt;Menidia menidia&amp;lt;/em&amp;gt; were collected from Mumford Cove (41°19’25” N, 72°1’7” W), Groton, CT, in late spring and early summer of 2016 and 2017 and transported to the Rankin seawater laboratory at University of Connecticut’s Avery Point Campus. Adults were strip-spawned, and fertilized eggs were randomly distributed into 20-L rearing containers, which were placed into each treatment tank within 2h post-fertilization. All experimental methods were approved and conducted according to University of Connecticut Institutional Animal Care and Use Committee protocol #A14-032. Of six factorial experiments conducted in 2016 and 2017, experiments 1-4 quantified CO₂ × temperature effects and experiments 5-6 quantified CO₂ × oxygen effects. Experiment 1 used 400 and 2200 uatm as target pCO₂ levels, crossed with two temperatures: 17°C and 24°C. Experiments 2 and 3 factorially crossed three pCO₂ levels (400, 2200, and 4200 uatm) with three temperatures (17°C, 20°C, and 24°C). Experiment 4 used the same three target pCO₂ levels crossed with 24°C and 28°C. Experiments 5 and 6 exposed &amp;lt;em&amp;gt;M. menidia&amp;lt;/em&amp;gt; early life stages to three levels of pCO₂ (400, 2200, and 4200 uatm) crossed factorially with three target levels of oxygen partial pressure (pO₂): normoxic (23 kPa), suboxic (12 kPa) and hypoxic (7.5 or 9 kPa). The pCO₂ levels were calculated based on measured pH, temperature, salinity, and total alkalinity (A&amp;lt;sub&amp;gt;T&amp;lt;/sub&amp;gt;). A&amp;lt;sub&amp;gt;T&amp;lt;/sub&amp;gt; samples were collected three times per experiment and measured using an endpoint titration. Based on these measurements, the pCO₂ (uatm) was calculated in CO2SYS (V2.1). In the CO₂ × temperature experiments, oxygen was maintained at ~100% air saturation (&amp;amp;gt;20 kPa). For experiments 1 and 4 this was achieved with continuous bubbling and validated daily for each tank with a handheld probe. For experiments 2, 3, 5, and 6, dissolved oxygen (DO, mg L⁻¹) measurements were automatically taken twice hourly in each tank by a DO probe connected to a LabView program, which adjusted bubbling of CO₂-stripped air or nitrogen gas to maintain target oxygen levels.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Closed respirometry measurements were conducted on embryos randomly sampled from each treatment 1-3 days prior to hatch and larvae sampled on the day of hatching. Oxygen consumption rates were measured by two 24-channel SensorDish readers (SDR) and glass well plates equipped with an optical oxygen sensor spot in each well. Each 0.5-mL well received a single embryo or larva, and at least one well contained only treatment water to measure background microbial respiration. Well plates were sealed and placed in temperature-controlled water baths and dissolved oxygen (DO, mg L⁻¹) was recorded every fifteen seconds by the SDR software until DO had decreased by 3 mg L⁻¹ in at least one of the wells, for 15-60 minutes. In the case of the suboxic and hypoxic treatments from experiments 5 and 6, however, the trials lasted five minutes regardless of the DO differential, given the already low oxygen in the treatment water. At the end of each measurement period, embryos and larvae were checked for injury or death, and any other factors that might have affected oxygen consumption rates were noted.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Known Problems:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Embryos were not sampled in Experiment 2 due to logistical issues. Some fish IDs might be missing because the individual died or escaped, and was therefore not included in the dataset although it had already been assigned a number before respirometry.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/650183.rdf" xlink:title="OCE-1536336" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1536336 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1536336</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/650191.rdf" xlink:title="OCE-1536165" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1536165 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1536165</gmx:Anchor>
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Coastal marine ecosystems provide a number of important services and resources for humans, and at the same time, coastal waters are subject to environmental stressors such as increases in ocean acidification and reductions in dissolved oxygen. The effects of these stressors on coastal marine organisms remain poorly understood because most research to date has examined the sensitivity of species to one factor, but not to more than one in combination. This project will determine how a model fish species, the Atlantic silverside, will respond to observed and predicted levels of dissolved carbon dioxide (CO2) and oxygen (O2). Shorter-term experiments will measure embryo and larval survival, growth, and metabolism, and determine whether parents experiencing stressful conditions produce more robust offspring. Longer-term experiments will study the consequences of ocean acidification over the entire life span by quantifying the effects of high-CO2 conditions on the ratio of males to females, lifetime growth, and reproductive investment. These studies will provide a more comprehensive view of how multiple stressors may impact populations of Atlantic silversides and potentially other important forage fish species. This collaborative project will support and train three graduate students at the University of Connecticut and the Stony Brook University (NY), two institutions that attract students from minority groups. It will also provide a variety of opportunities for undergraduates to participate in research and the public to learn about the study, through summer research projects, incorporation in the &quot;Women in Science and Engineering&quot; program, and interactive displays of environmental data from monitoring buoys. The two early-career investigators are committed to increasing ocean literacy and awareness of NSF-funded research through public talks and presentations.&lt;/p&gt;
&lt;p&gt;This project responds to the recognized need for multi-stressor assessments of species sensitivities to anthropogenic environmental change. It will combine environmental monitoring with advanced experimental approaches to characterize early and whole life consequences of acidification and hypoxia in the Atlantic silverside (Menidia menidia), a valued model species and important forage fish along most of the US east coast. Experiments will employ a newly constructed, computer-controlled fish rearing system to allow independent and combined manipulation of seawater pCO2 and dissolved oxygen (DO) content and the application of static and fluctuating pCO2 and DO levels that were chosen to represent contemporary and potential future scenarios in productive coastal habitats. First CO2, DO, and CO2 × DO dependent reaction norms will be quantified for fitness-relevant early life history (ELH) traits including pre- and post-hatch survival, time to hatch, post-hatch growth, by rearing offspring collected from wild adults from fertilization to 20 days post hatch (dph) using a full factorial design of 3 CO2 × 3 DO levels. Second, the effects of tidal and diel CO2 × DO fluctuations of different amplitudes on silverside ELH traits will be quantified. To address knowledge gaps regarding the CO2-sensitivity in this species, laboratory manipulations of adult spawner environments and reciprocal offspring exposure experiments will elucidate the role of transgenerational plasticity as a potential short-term mechanism to cope with changing environments. To better understand the mechanisms of fish early life CO2-sensitivity, the effects of temperature × CO2 on pre- and post-hatch metabolism will be robustly quantified. The final objective is to rear silversides from fertilization to maturity under different CO2 levels and assess potential CO2-effects on sex ratio and whole life growth and fecundity.&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;Related references:&lt;/strong&gt;&lt;br /&gt;
Gobler, C.J. and Baumann, H. (2016) Hypoxia and acidification in ocean ecosystems: Coupled dynamics and effects on marine life. Biology Letters 12:20150976. doi:&lt;a href=&quot;http://dx.doi.org/10.1098/rsbl.2015.0976&quot; target=&quot;_blank&quot;&gt;10.1098/rsbl.2015.0976&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;Baumann, H. (2016) Combined effects of ocean acidification, warming, and hypoxia on marine organisms. Limnology and Oceanography e-Lectures 6:1-43. doi:&lt;a href=&quot;http://dx.doi.org/10.1002/loe2.10002&quot; target=&quot;_blank&quot;&gt;10.1002/loe2.10002&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;Depasquale, E., Baumann, H., and Gobler, C.J. (2015) Variation in early life stage vulnerability among Northwest Atlantic estuarine forage fish to ocean acidification and low oxygen Marine Ecology Progress Series 523: 145–156.doi:&lt;a href=&quot;http://dx.doi.org/10.3354/meps11142&quot; target=&quot;_blank&quot;&gt;10.3354/meps11142&lt;/a&gt;&lt;/p&gt;</gco:CharacterString>
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                <gco:CharacterString>&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Sampling and analytical procedures:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Detailed experimental methods are provided for experimental design and water chemistry in Murray and Baumann (2018) and Cross et al. (2019), and for respirometry methods in Schwemmer et al. (2020). In summary, spawning-ripe adult &amp;lt;em&amp;gt;Menidia menidia&amp;lt;/em&amp;gt; were collected from Mumford Cove (41°19’25” N, 72°1’7” W), Groton, CT, in late spring and early summer of 2016 and 2017 and transported to the Rankin seawater laboratory at University of Connecticut’s Avery Point Campus. Adults were strip-spawned, and fertilized eggs were randomly distributed into 20-L rearing containers, which were placed into each treatment tank within 2h post-fertilization. All experimental methods were approved and conducted according to University of Connecticut Institutional Animal Care and Use Committee protocol #A14-032. Of six factorial experiments conducted in 2016 and 2017, experiments 1-4 quantified CO₂ × temperature effects and experiments 5-6 quantified CO₂ × oxygen effects. Experiment 1 used 400 and 2200 uatm as target pCO₂ levels, crossed with two temperatures: 17°C and 24°C. Experiments 2 and 3 factorially crossed three pCO₂ levels (400, 2200, and 4200 uatm) with three temperatures (17°C, 20°C, and 24°C). Experiment 4 used the same three target pCO₂ levels crossed with 24°C and 28°C. Experiments 5 and 6 exposed &amp;lt;em&amp;gt;M. menidia&amp;lt;/em&amp;gt; early life stages to three levels of pCO₂ (400, 2200, and 4200 uatm) crossed factorially with three target levels of oxygen partial pressure (pO₂): normoxic (23 kPa), suboxic (12 kPa) and hypoxic (7.5 or 9 kPa). The pCO₂ levels were calculated based on measured pH, temperature, salinity, and total alkalinity (A&amp;lt;sub&amp;gt;T&amp;lt;/sub&amp;gt;). A&amp;lt;sub&amp;gt;T&amp;lt;/sub&amp;gt; samples were collected three times per experiment and measured using an endpoint titration. Based on these measurements, the pCO₂ (uatm) was calculated in CO2SYS (V2.1). In the CO₂ × temperature experiments, oxygen was maintained at ~100% air saturation (&amp;amp;gt;20 kPa). For experiments 1 and 4 this was achieved with continuous bubbling and validated daily for each tank with a handheld probe. For experiments 2, 3, 5, and 6, dissolved oxygen (DO, mg L⁻¹) measurements were automatically taken twice hourly in each tank by a DO probe connected to a LabView program, which adjusted bubbling of CO₂-stripped air or nitrogen gas to maintain target oxygen levels.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Closed respirometry measurements were conducted on embryos randomly sampled from each treatment 1-3 days prior to hatch and larvae sampled on the day of hatching. Oxygen consumption rates were measured by two 24-channel SensorDish readers (SDR) and glass well plates equipped with an optical oxygen sensor spot in each well. Each 0.5-mL well received a single embryo or larva, and at least one well contained only treatment water to measure background microbial respiration. Well plates were sealed and placed in temperature-controlled water baths and dissolved oxygen (DO, mg L⁻¹) was recorded every fifteen seconds by the SDR software until DO had decreased by 3 mg L⁻¹ in at least one of the wells, for 15-60 minutes. In the case of the suboxic and hypoxic treatments from experiments 5 and 6, however, the trials lasted five minutes regardless of the DO differential, given the already low oxygen in the treatment water. At the end of each measurement period, embryos and larvae were checked for injury or death, and any other factors that might have affected oxygen consumption rates were noted.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Known Problems:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Embryos were not sampled in Experiment 2 due to logistical issues. Some fish IDs might be missing because the individual died or escaped, and was therefore not included in the dataset although it had already been assigned a number before respirometry.&amp;lt;/p&amp;gt;</gco:CharacterString>
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                <gco:CharacterString>&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Data Processing:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Routine metabolic rates were calculated in R statistical software (v4.0.0; R Core Team, 2020). Because temperature influences oxygen solubility and metabolic rates of fish, we measured temperature simultaneously with DO throughout the measurement period and only used data for periods of time in which the temperature changed by less than ~0.03°C min⁻¹. A linear model was fit to the DO values with respect to time for each well. The slope (mg O₂ L⁻¹ s⁻¹) of the linear model was used to calculate oxygen consumption rate (RO₂; umol O₂ h⁻¹) with the following formula: RO₂=slope/(0.032×3600×0.0005), where 0.032 is the molar mass of O₂ (mg mol⁻¹), 3600 converts seconds to hours, and 0.0005 L is the well volume. The mean RO2 from control wells was subtracted from each fish-containing well of the same treatment to account for microbial respiration and obtain fish RO2. Size differences in embryos were negligible and quantifying embryo mass was impractical, so RO2 was not normalized to mass and is reported as whole-embryo routine metabolic rate (RMR). Larval total length (TL, mm) was measured in images (Image J) taken by digital camera (TrueChrome Metrics, Tucsen Photonics Co., Fuzhou, Fujian, China) connected to a stereo microscope (Nikon Eclipse E200). TL was then converted to dry weight (DW, mg) using the relationship ln(DW)=2.997×ln(TL)-6.703 (H. Baumann, personal communication, June 23, 2017). DW was then used to calculate the larval mass-specific RMR (umol mg⁻¹ h⁻¹) as RMR=RO2/DW.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;BCO-DMO processing:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
- converted dates to format YYYY-MM-DD;&amp;lt;br /&amp;gt;
- rounded values of&amp;amp;nbsp;embryo_RMR and larva_RMR to 6 decimal places.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmi:MI_Instrument>
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Intellical PHC281 pH Electrode with HQ11D Handheld pH/ORP Meter, Hach®, Loveland, CO, USA. 
Hach® pHD digital electrode. 
  Instrument Name: pH Sensor Instrument Short Name:pH Sensor   Instrument Description: An instrument that measures the hydrogen ion activity in solutions.

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