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Seawater carbonate chemistry and PI-curve parameters, non-photochemical quenc...
Shallow coastal marine ecosystems are exposed to intensive warming events in the last decade, threatening keystone macroalgal species such as the bladder wrack (Fucus... -
Seawater carbonate chemistry and estuarine dissolved organic carbon export
Relative to their surface area, estuaries make a disproportionately large contribution of dissolved organic carbon (DOC) to the global carbon cycle, but it is unknown how this... -
Seawater carbonate chemistry and net community calcification (NCC) and net co...
There is a long history of examining the impacts of nutrient pollution and pH on coral reefs. However, little is known about how these two stressors interact and influence coral... -
Seawater carbonate chemistry and calcification of Halimeda cuneata, photosynt...
The ultimate effect that ocean acidification (OA) and warming will have on the physiology of calcifying algae is still largely uncertain. Responses depend on the complex... -
Seawater carbonate chemistry and primary and bacterial production in Antarcti...
Polar waters may be highly impacted by ocean acidification (OA) due to increased solubility of CO2 at colder water temperatures. Three experiments examining the influence of OA... -
Gross primary production, respiration, and net calcification in coral reef se...
Rates of gross primary production (GPP), respiration (R), and net calcification (Gnet) in coral reef sediments are expected to change in response to global warming (and the... -
Antagonistic effects of ocean acidification and rising sea surface temperatur...
Increasing atmospheric CO2 is raising sea surface temperature (SST) and increasing seawater CO2 concentrations, resulting in a lower oceanic pH (ocean acidification; OA), which... -
Temperature dependence of CO2-enhanced primary production in the European Arc...
The Arctic Ocean is warming at two to three times the global rate and is perceived to be a bellwether for ocean acidification. Increased CO2 concentrations are expected to have... -
Two intertidal, non-calcifying macroalgae (Palmaria palmata and Saccharina la...
Ocean acidification, the result of increased dissolution of carbon dioxide (CO2) in seawater, is a leading subject of current research. The effects of acidification on... -
Response of the microbial food web to gradients of organic matter and grazing...
Zooplankton treatment: HZ: zooplankton added, LZ: Zooplankton removedCarbon treatment: 0C: No glucose addition, 0.5: 0.5 x Redfield. 1: 1xRedfield, 2: 2xRedfield, 3: 3XRedfield -
Chlorophyll, net oxygen production and respiration rates measured on water bo...
For the determination of primary production surface water samples are filled into Winkler bottles. The sampling station is located directly in front of the institute. Samples... -
Phytoplankton primary production at Koenigshafen, List/Sylt, in 2014
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Phytoplankton primary production at Koenigshafen, List/Sylt, in 2013
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Phytoplankton primary production at Koenigshafen, List/Sylt, in 2012
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Phytoplankton primary production at Koenigshafen, List/Sylt, in 2011
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Phytoplankton primary production at Koenigshafen, List/Sylt, in 2010
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Phytoplankton primary production at Koenigshafen, List/Sylt, in 2009
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Phytoplankton primary production at Koenigshafen, List/Sylt, in 2008
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Phytoplankton primary production at Koenigshafen, List/Sylt, in 2007
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Phytoplankton primary production at Koenigshafen, List/Sylt, in 2006
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