Joana Barcelos e Ramos

Community composition has greater impact on the functioning of marine phytoplankton communities than ocean acidification

Ecosystem functioning is simultaneously affected by changes in community composition and environmental change such as increasing atmospheric carbon dioxide (CO2 ) and subsequent ocean acidification. However, it largely remains uncertain how the effects of these factors compare to each other. Addressing this question, we experimentally tested the hypothesis that initial community composition and elevated CO2 are equally important to the regulation of phytoplankton biomass. We full-factorially exposed three compositionally different marine phytoplankton communities to two different CO2 levels and examined the effects and relative importance (ω(2) ) of the two factors and their interaction on phytoplankton biomass at bloom peak. The results showed that initial community composition had a significantly greater impact than elevated CO2 on phytoplankton biomass, which varied largely among communities. We suggest that the different initial ratios between cyanobacteria, diatoms, and dinoflagellates might be the key for the varying competitive and thus functional outcome among communities. Furthermore, the results showed that depending on initial community composition elevated CO2 selected for larger sized diatoms, which led to increased total phytoplankton biomass. This study highlights the relevance of initial community composition, which strongly drives the functional outcome, when assessing impacts of climate change on ecosystem functioning. In particular, the increase in phytoplankton biomass driven by the gain of larger sized diatoms in response to elevated CO2 potentially has strong implications for nutrient cycling and carbon export in future oceans.

Effects of increasing seawater carbon dioxide concentrations on chain formation of the diatom Asterionellopsis glacialis.

Diatoms can occur as single cells or as chain-forming aggregates. These two strategies affect buoyancy, predator evasion, light absorption and nutrient uptake. Adjacent cells in chains establish connections through various processes that determine strength and flexibility of the bonds, and at distinct cellular locations defining colony structure. Chain length has been found to vary with temperature and nutrient availability as well as being positively correlated with growth rate. However, the potential effect of enhanced carbon dioxide (CO2) concentrations and consequent changes in seawater carbonate chemistry on chain formation is virtually unknown. Here we report on experiments with semi-continuous cultures of the freshly isolated diatom Asterionellopsis glacialis grown under increasing CO2 levels ranging from 320 to 3400 µatm. We show that the number of cells comprising a chain, and therefore chain length, increases with rising CO2 concentrations. We also demonstrate that while cell division rate changes with CO2 concentrations, carbon, nitrogen and phosphorus cellular quotas vary proportionally, evident by unchanged organic matter ratios. Finally, beyond the optimum CO2 concentration for growth, carbon allocation changes from cellular storage to increased exudation of dissolved organic carbon. The observed structural adjustment in colony size could enable growth at high CO2 levels, since longer, spiral-shaped chains are likely to create microclimates with higher pH during the light period. Moreover increased chain length of Asterionellopsis glacialis may influence buoyancy and, consequently, affect competitive fitness as well as sinking rates. This would potentially impact the delicate balance between the microbial loop and export of organic matter, with consequences for atmospheric carbon dioxide.

Nutrient-specific responses of a phytoplankton community: a case study of the North Atlantic Gyre, Azores

 DEPARTAMENTO DE CIÊNCIAS AGRÁRIAS, INSTITUTE OF AGRICULTURAL AND ENVIRONMENTAL RESEARCH AND TECHNOLOGY OF THE AZORES, RUA CAPITÃO D’ÁVILA, SÃO PEDRO, PT-- ANGRA DO HEROÍSMO, AÇORES PORTUGAL, CENTRE FOR COASTAL BIOGEOCHEMISTRY, SCHOOL OF ENVIRONMENT, SCIENCE AND ENGINEERING, SOUTHERN CROSS UNIVERSITY, PO BOX , LISMORE, NSW , AUSTRALIA, DEPARTMENT OF BIOLOGICAL OCEANOGRAPHY, LEIBNIZ INSTITUTE FOR BALTIC SEA RESEARCH, WARNEMÜNDE (IOW), SEESTRASSE , D- ROSTOCK, GERMANY, DEPARTMENT OF BIOLOGICAL OCEANOGRAPHY, OCEANOGRAPHIC INSTITUTE AT THE UNIVERSITY OF SÃO PAULO, PRAÇA DO OCEANOGRÁFICO , SÃO PAULO, SP -, BRAZIL AND