Award Abstract # 1521610
OCE-PRF Track 2 (International) - Plasticity of Inorganic Carbon Use in Marine Calcifying Macroalgae Across a Latitudinal Gradient and Consequences of Global Change

NSF Org: OCE
Division Of Ocean Sciences
Recipient:
Initial Amendment Date: July 22, 2015
Latest Amendment Date: July 22, 2015
Award Number: 1521610
Award Instrument: Fellowship Award
Program Manager: Elizabeth Rom
elrom@nsf.gov
 (703)292-7709
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: August 1, 2015
End Date: January 31, 2018 (Estimated)
Total Intended Award Amount: $194,000.00
Total Awarded Amount to Date: $194,000.00
Funds Obligated to Date: FY 2015 = $194,000.00
History of Investigator:
Recipient Sponsored Research Office: Hofmann Laurie C
28195 Bremen
 GM
Sponsor Congressional District:
Primary Place of Performance: Max Planck Institute for Marine Microbiology
Bremen
 GM  28359
Primary Place of Performance
Congressional District:
07
Unique Entity Identifier (UEI):
Parent UEI:
NSF Program(s): IRFP-Inter Res Fellowship Prog
Primary Program Source: 01001516DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 1650, 5936, 7137, 8205
Program Element Code(s): 595600
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Crustose coralline algae (CCA) are calcifying algae that are important to coastal stability, beach formation, and coral reef structure. There is growing concern that these organisms are sensitive to global climate change, which will have important consequences for coastal and reef stability. Despite their significance and sensitivity, their basic photosynthetic and calcification mechanisms are not well understood. In this project, the fellow will establish a better understanding of these mechanisms by studying CCA specimens along a latitudinal gradient in the Northeast Atlantic. The research will be conducted at the Max Planck Institute for Marine Microbiology in Bremen, Germany within the Microsensor Research Group led by Dr. Dirk de Beer. The activities and results of this project will be shared on a Blog and Facebook page to enhance public awareness of the project. Furthermore, the fellow will facilitate development of a Virtual CCA Research Group to foster communication among scientists world-wide working with CCA which will elevate the impacts of this project to a global scale.

Both field sampling and laboratory experiments are used to pursue the goals of the project, which are: 1) to determine the environmental factors influencing the stable carbon isotope signatures of Lithothamnion spp. along a latitudinal gradient, 2) to determine the plasticity of dissolved inorganic carbon (DIC) uptake mechanisms in response to light and temperature and 3) to determine how photosynthesis and calcification are linked to DIC uptake mechanisms. The latitudinal gradient consists of eight sampling locations in the North Atlantic from Svalbard to Cape Verde in the east and from Florida to the Caribbean in the west. The stable carbon isotope signatures of collected samples are measured to determine the plasticity of DIC uptake along the latitudinal gradient in relation to environmental conditions measured at long-term monitoring stations. In the lab, microsensors are used to measure pH, oxygen and calcium fluxes within the diffusive boundary layer (DBL) at the surface of the algae. Because DIC uptake depends heavily on the DBL, microsensors provide a unique method for determining the effects of temperature and light on photosynthesis and calcification within the microenvironment at the interface between the external seawater and the algal surface. Successful completion of the project will provide the first study on latitudinal patterns and the flexibility of DIC uptake mechanisms in a calcifying macroalga and will improve the scientific knowledge of the relationship between DIC uptake, photosynthesis and calcification under changing environmental conditions and across biogeographical ranges.

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

Rhodoliths are free-living calcareous red algae with a global distribution from the Artic to the tropics and the widest depth range of any marine algae. As ecosystem engineers, they form extensive beds in shallow marine environments that provide important habitats and nurseries for marine organisms and contribute to carbonate sediment accumulation. There is growing concern that these organisms are sensitive to rising carbon dioxide levels, yet little is known about their physiology. Therefore, the main goal of this project was to establish a better understanding of how rhodoliths obtain the carbon they need for photosynthesis and calcification, and how these mechanisms are affected by different environmental conditions. I found that the carbon uptake mechanisms of rhodoliths in the northeast Atlantic are flexible and depend on environmental conditions, mainly dissolved inorganic carbon concentrations in the seawater. Arctic rhodoliths have unique physiological mechanisms that facilitate calcification and reduce the loss of inorganic carbon during long periods of darkness. Some rhodoliths are even able to take up organic carbon and nitrogen to supplement their energy demands. High carbon dioxide levels did not have a strong effect on photosynthesis, and the algae were able to maintain a chemical microenvironment on their surface conducive to calcification. The results of this project show that rhodoliths are robust organisms that optimize the use of available dissolved inorganic and organic compounds through flexible physiological mechanisms. This is an important first step in understanding the physiology of rhodoliths and why they have such an extensive biogeographical distribution. Additionally, the results suggest that some rhodoliths may be less sensitive to high carbon dioxide levels than previously thought. Results from this project and other researchers working on coralline algae will be published in a special issue on coralline algae in the open access journal Frontiers in Marine Science.

The broader impacts of the project include the establishment of the Coralline Algae Network. The network is a platform on the Research Gate website where researchers and students around the world that are interested in coralline algae can ask questions, share results, discuss failures, and establish new collaborations. The project website, blog, facebook page and public talks increased awareness about the world wide importance of rhodolith beds. Additionally, the research conducted during this project resulted in the L'Oreal Germany For Women in Science award that established financial support for female researchers needing child care during field trips and travel for conferences. The project had a strong international network, including bachelor and masters students from Germany, Serbia, Spain, Latvia and the USA. A collaboration was also established with partners from Brazil, where resources for marine research are limited, to provide them with access to new technology and methods for investigating rhodolith beds in the north and south Atlantic. Future projects stemming from this project are planned, including investigating whether rhodoliths can be used as biofilters for fish aquaculture, physiological investigations of south Atlantic rhodoliths, and a diversity assessment of Cuban coralline algae, where little is known about the species present.

 

 


Last Modified: 03/09/2018
Modified by: Laurie C Hofmann

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