Background:
Since the beginning of the industrial revolution, about one third of the CO2 released by human activities has been absorbed by the world’s ocean which plays a key role in moderating climate change. Without the ocean absorbing CO2, the CO2 in the atmosphere would be much higher, potentially increasing the effects of global climate change.
The burning of fossil fuels for energy production, manufacturing, and transportation has driven the level of carbon dioxide in the atmosphere to levels 30% greater than prior to the industrial revolution. Higher atmospheric levels of carbon dioxide have resulted in increasing amounts of carbon dioxide dissolving in the ocean leading to the reduction in pH or increase in acidity of the ocean. It should be noted that the ocean is not acidic (pH < 7) however the trend in declining pH has been observed and is referred to as “ocean acidification”. When carbon dioxide (CO2) dissolves in seawater, it creates carbonic acid (H2CO3), which releases bicarbonate ions (HCO31-) and hydrogen (H+) ions into the water. The hydrogen ions make the seawater more acidic (lowering its pH) and promoting the dissolution of CaCO3.In addition, some of the hydrogen ions (H+)react with carbonate ions (CO32-) already in the seawater to create more bicarbonate (Figure 1). This process reduces the amount of carbonate (an important mineral for building shells) dissolved in the seawater.
Figure 1. The process of ocean acidification.
Thus, the impacts of ocean acidification and lower carbonate ion concentrations on marine ecosystems include reduced growth of organisms that form calcareous skeletons or shells, such as corals, pteropods (swimming snails) and bivalves (such as oysters, clams and mussels). This results in reducing the rate at which marine animals can build new skeletons and shells while simultaneously increasing the rate of dissolution of existing shells.
In this lab, we will focus on coral reefs with their enormous biodiversity, productivity and susceptibility to human impact We can’s investigate the rate at which coral reefs are being built in the context of this lab. We can however investigate the impact of elevated CO2 on the dissolution of existing reefs. The vast bulk of a coral reef is composed of CaCO3 in coral skeletons and the shells of a vast array of animals inhabiting the reef and we can simply expose a composite sample of a reefs skeletons and shells to increased CO2 (decreased pH). We can obtain a representative sample of coral skeletons and animal shells in an unlikely place, parrotfish poop. Check out the link Parrotfish poop.
Check out the poop.
The beach sand we will use today was collected from the beaches of the Florida Keys by previous SMCM students. Place a small sample (single layer of grains) in a weigh boat and observe it under a dissecting microscope. List the organisms that you can identify. This web site will help. Coral beach sand.
Experimental Procedure Week 1
Set up the microcosms:
Prepare acidified seawater
When all of your samples have been prepared, double check your labels and store them on the shelves at the back of the lab until next time.
Questions
While you wait your turn to process your samples, answer the questions on todays work sheet and submit it in the assignments tab on BB
Provide your answers in blue font color below each question.
This must be submitted before you leave lab today
Experimental Procedure Week 2
Determine the weight of the remaining coral and shell material in each treatment pH
Caution: take great care, at every step below, to prevent sand loss.
Experimental Procedure Week 3
Final weighing an visualization of your data
(To Be Completed Today--Your ticket out the door!)
Procedures:
Percent Change (%) =
Part B. Addressing your hypothesis (Final Report)
Consider the hypothesis you created during the first week of the Ocean Acidification Lab. You now have access to the entire class data set. Using this complete data set, visualize the data needed to address your hypothesis. You will need to consider how best to visualize the data and be able to discuss why your hypothesis was upheld or not. You may need to do some more research and seek help from your instructor to TA on how to accomplish this task. You can also complete some simple statistical analyses as well, that your instructor or TA could help you with. Remember “Hypothesis testing from the stats lab? . If not take the time to take the time to work with your TA or instructor.
Your rubric and expectations are below. Let me know if you have questions.
Expectations of final report
You are to turn in a typed document, which includes all of the components of a scientific paper. You may want to reread the lab manual for lab 1 This document is to be formatted like a formal lab report, with Introduction, Methods, Results and Discussion.
Introduction |
1. Includes the background information that you acquired in the first week. This information should lead to your hypothesis. 2. States hypothesis that is based on knowledge of what you know about ocean acidification |
15 |
Methods |
Logical description of methods, that includes all steps taken to collect ALL the data. Also, description of replicates (each lab team did the exact same experiment and collected the same data. why did you do that?) Be sure to include everything we did over the three week long research project, that includes, weighing, seawater, pH...drying...etc...! |
15 |
Results |
Describes what happened in words and uses tables and/or graph type which highlights relationships between the data points or other relevant aspects of the data. To ilustrate the text. The results of hypothesis testing statistics |
15 |
Discussion |
-Lead section with the most exciting or interesting result |
15 |
Background Info |
Completed on first day of lab (already turned in) |
15 |
Walter I. Hatch
wihatch@smcm.edu
October 01, 2017