Ocean Acidification Lab

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Diamonique Harris Dr. Amanda Glazier Biology 3244 Lab May 30, 2018 Ocean Acidification Introduction : Ocean acidification refers to a reduction in the pH of the ocean over an extended period of time, caused primarily by uptake of carbon dioxide from the atmosphere. (NOAA) The pH of the water lowers when the atmospheric CO 2 dissolves and equilibrates in surface waters, forming carbonic acid (H 2 CO 3 ), which disassociates to bicarbonate ions (HCO 3 - ) and hydrogen ions (H + ). At the same time the H + ions are reacting with carbonate ions (CO 3 2- ) to form additional HCO 3 - , reducing the available carbonate ions (CO 3 2- ) that some organisms use to produce calcium carbonate skeletons. If the concentration of H + increases in a solution, it’s pH decreases and the solution will become more acidic, which is why the process is called ocean acidification (Dr. Jay Lecture 4). Prior to the industrial revolution the carbon cycle was approximately in balance (Dr. Jay Lecture 4), as in the amount of CO s being output into the atmosphere was the same amount being absorbed by the ocean. Over the years surface waters have decreased by 0.1 pH unit and are now expected to decline an additional 0.3-0.4 pH unit in about 70 years. Ocean acidification affects marine organisms that secrete calcium carbonate shells or skeletons such as corals, mollusks, and echinoderms. The ocean absorbs about 30 percent of CO 2 that is released into the atmosphere. (NOAA) Resulting in a direct correlation between an increase in CO 2 and an increase in the level of the ocean which decreases the oxygen available.
Corals have a more soluble form of calcium carbonate in their shells called aragonite, whereas, Donax has a less soluble form, called calcite. It is expected that ocean acidification will not only have a negative effect on marine calcifiers but have a greater effect on organisms that secrete aragonite. The purpose of this experiment is to test the effects of ocean acidification on skeletons of corals and shells of the beam clam Donax sp. Null Hypothesis (H 0 ) : There is no change in the shell mass through several days of treatment Alternative Hypothesis (H 1 ): There is a loss of mass indicating shells are dissolving (initial mass – wet mass 23) Methods : The experiment began with four beakers. Two labeled ambient pH and two labeled treatment pH, one of each for control and the other for clam. 20 clamshells being placed into seawater to soak for 10 minutes and the weights were recorded. The four beakers were filled as the following: Ambient pH control jar: 100 mL seawater Treatment pH control jar: 100 mL low pH water Ambient pH clam jar: 100 mL seawater Treatment pH clam jar: 100 mL low pH water 20 clamshells soaking . The clamshells were then placed 10 into each of the “clam” jars. An API kit was used in order to determine the pH, calcium concentration and Kh levels of the samples. The samples then sat
to dry for 5 days and then the pH, calcium concentration, and Kh levels were recorded for each samples. Finally, the clamshells were placed back into seawater solution to soak again and their final weights were recorded. Results : Table 1: Test subject masses. Clam – ambient Clam – treatment Initial mass (g) 0.232 0.40 Wet mass (g) May 21 0.216 0.338 Dry mass (g) May 23 0.209 0.361 Wet mass (g) May 23 0.209 0.37 Table 2: Masses of clams over a 5day period. Clam - ambient Clam - treatment Initial mass to wet mass May 21 0.232 – 0.216 = 0.016 0.40 – 0.338 = 0.062 Initial mass to dry mass may 23 0.232 – 0.209 = 0.023 0.40 – 0.361 = 0.039 Initial mass to wet mass may 23 0.232 – 0.209 = 0.023 0.40 – 0.37 = 0.03 Wet mass May 21 to dry mass May 23 0.216 – 0.209 = 0.007 0.338 – 0.361 = - 0.023 Wet mass May 21 to wet mass May 23 0.216 – 0.209 = 0.007 0.338 – 0.37 = - 0.032 Table 3: Water chemistry parameters for seawater control. pH – ambient pH – treatment Calcium – ambient Calcium – treatment KH – ambient KH - treatment Start 7.35 6.55 600 ppm – 30 drops 580 – 29 drops 14 drops – 250.6 ppm 16 drops – 286.4 ppm 1.5 hours later 7.45 6.67 540 ppm 500 – 25 drops 14 drops – 250.6 16 drops – 286.4 5 days later 7.94 7.69 520 ppm 440 ppm 14 drops 12 drops – 214.8 ppm Net change 0.59 1.14 -80 -140 0 -71.6 Table 4: Water chemistry parameters for clam treatment. pH – ambient pH – treatment Calcium – ambient Calcium – treatment KH – ambient KH - treatment Start 7.46 6.62 460 ppm 520 – 26 drops 14 drops – 250.6 ppm 14 drops – 250.6 ppm 1.5 hours later 7.47 6.58 560 ppm -28 drops 560 – 28 drops 14 drops – 250.6 ppm 16 drops -286.4
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5 days later 7.92 7.71 520 ppm-26 drops 420 – 21 drops 11 drops- 196.9 ppm 11 drops – 196.9 ppm Net change 0.46 1.09 60 -100 -53.7 -53.7 Table 5: Class Data: Clam mass
Table 6: Class Data: Net Changes in Seawater Parameters: a) b)
c) d) e) f) g)
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Graphs: A) 1 2 0 0.2 0.4 0.6 0.8 1 1.2 Control pH vs Clam pH Control Clam pH B) 1 2 -60 -40 -20 0 20 40 60 Control Calcium vs Clam Calcium Control Clam Calcium C) 1 2 -70 -60 -50 -40 -30 -20 -10 0 Control Kh vs Clam Kh Control Clam Kh
The data above was collected over a period of 5 days. Table 1 shows the mass results of the experiment of our individual group. It displays that the final mass of the clams was less than the initial mass in both the ambient and treatment clams. Table 2, is a breakdown of masses over the 5 day period comparing ambient clams to those in the treatment solution. Tables 3 and 4, are the values of pH, calcium, and Kh for ambient and treatment clams in both seawater solution as the control and the experimental clam treatment solution. In both solutions, the ph increased over the course of 5 days, however, both the calcium and Kh decreased over the course of the 5 days. Table 5, is the class data for the clam ambient and clam treatment masses over the course 5 days. Table 6, shows the class data for the net change in seawater parameters for ph, calcium, and Kh, and the average. Table 6a-6f, display t-Test for the following: a-b) Calcium ambient vs calcium treatment within the two setups (seawater, clam) c-d) KH ambient vs KH treatment within the two setups (seawater, clam) e) Calcium treatment between the two setups (clam vs seawater). f) KH treatment between the two setups (clam vs seawater). g) Between appropriate net change ambient mass and treatment mass. Finally graphs A-C, are of calcium, pH, and Kh for both seawater and clam. Graph A, shows that the clam has an effect on the pH, as the pH was almost double. Graph B, shows that the clam cause the calcium levels to decrease compared to the seawater where the calcium increases. Lastly, graph C, shows that the Kh decreases in both seawater and clam, however in clam the Kh decreases by almost double the amount of seawater.
Discussion: The purpose of this experiment was to test the effects of ocean acidification on skeletons of corals and shells. After several days of testing it was found that the clamshells gained mass over time in seawater, whereas, in clam solution the clam loss mass. In addition, it was measured that the pH of the clam treatment was lower than the pH of the clam ambient and the same for the seawater ambient and treatment. However, the difference in pH between seawater ambient and treatment versus clam ambient and treatment is that the clam ambient and treatment are slightly higher than the seawaters. Following after, it was found that the calcium concentration in both the seawater ambient and treatment decreased over the 5-day period. Whereas, the clam ambient and treatment solutions initially increased within the first 1.5 hours and then proceeded to decrease at the 5 th day. Finally, the Kh for each solution was found, the Kh for seawater ambient remain unchanged over the course of the 5 days. On the contrary, the Kh for seawater treatment and clam ambient both remain unchanged after 1.5 hours and then decreased by the 5 th day. For the clam treatment the Kh initially increased after 1.5 hours but then decreased by the 5 th day. Next, there were several t-Test ran in order to determine the p values for both seawater and clam, ambient and treatment. The p value for the net change in clam ambient and clam treatment mass was 0.31843554, which is above 0.05 indicating there is not enough evidence to reject the null hypothesis. Failing to reject the null hypothesis, means that there is not a significant change in clam mass within a few days, however it is still possible that over a course of several days or even weeks, there could be a significant change in mass.
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Although the result of the experiment did not give a complete accurate account as to what happens to clams during ocean acidification, it gives a general idea. Scientist predict that with that the levels of ocean acidification increasing, they can predict what the pH will be in 2100. With that prediction scientist formulated an experiment with pteropods, the pteropods were placed in seawater with the pH and carbonate levels projected for the year 2100 (PMEL). Studies showed that over the course of 45 days, the pteropod’s shell dissolved (PMEL) showing that as the ocean acidification increases the endangerment of calcium carbonate skeleton organisms increases. On the other hand, there are few species that can benefit from the higher concentration of CO 2 within the ocean such as photosynthetic algae and seagrasses because they require CO 2 just like plants on land (PMEL). References : Albright, A., Masona, B., Miller, M., and Langdon, C. 2010. Ocean acidification compromises recruitment success of the threatened Caribbean coral Acropora palmata. PNAS 107 (47): 20400-20404. Lunden, Dr. Jay. “Lecture 4 Global Ocean Change.” 21 May. 2018. Biology 3244 – Experimental Marine Biology, Temple University. Microsoft PowerPoint presentation. https://templeu.instructure.com/courses/40000/files/1924410?module_item_id=404689 Raven, J. Caldeira, K., Elderfield, H., Hoeg-Guldberg, O. and others. 2005. Ocean acidification due to increasing atmospheric carbon dioxide. Policy document 12/05. The Royal Society , London. Accessed at www.royalsoc.ac.uk on June 9, 2009. US Department of Commerce, and National Oceanic and Atmospheric Administration, “What Is Ocean Acidification?” NOAA’s National Ocean Service, Aug. 2012, https://oceanservice.noaa.gov/facts/acidification.html US Department of Commerce, and National Oceanic and Atmospheric Administration-PMEL, “What Is Ocean Acidification?” Ocean Carbon Storage, www.pmel.noaa.gov/co2/story/What+is+Ocean+Acidification%3F