GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Articles  (3)
  • 1
    Publication Date: 2014-04-15
    Repository Name: EPIC Alfred Wegener Institut
    Type: Inbook , peerRev
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2016-02-27
    Description: In a recent opinion article titled "The Omega Myth", Cyronak et al . provide a series of arguments as to why saturation state should not matter to marine calcifiers. In sections of their article, they highlight several aspects of our published work, and unfortunately appear to misinterpret the foundation for the kinetic–energetic hypothesis we have laid out previously. While we are in full agreement that omega sensitivity is not a substrate limitation issue, we more clearly detail below what a kinetic limitation means and why it is different from a substrate limitation. The kinetic argument we have previously presented highlights how the energetic cost of calcification increases with a decreasing saturation state (or omega). We then highlight several issues with a bicarbonate/proton flux model applied to newly developing marine bivalve larvae, and discuss how a bicarbonate/proton flux and omega-based sensitivity model do not have to be mutually exclusive. Our intent with this comment is to clarify the points raised by Cyronak et al . about our work, and help to move the thinking past dialectic debate towards a more synthetic view on ocean acidification impacts on marine calcifiers.
    Print ISSN: 1054-3139
    Electronic ISSN: 1095-9289
    Topics: Biology , Geosciences , Physics
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2015-10-20
    Description: The ability to reconstruct past ocean currents is essential for determining ocean circulation’s role in global heat transport and climate change. Our understanding of the relationship between circulation and climate in the past allows us to predict the impact of future climate-driven circulation changes. One proposed tracer of past ocean circulation is the neodymium isotope composition ( Nd ) of ancient water masses. However, ambiguities in what governs the Nd distribution in the modern ocean hamper interpretations of this tracer. Here we present Nd values for marine pore fluids, sediments, and the overlying water column for three sites in the North Pacific. We find that ocean bottom water Nd ( Nd BW ) in the northeast Pacific lies between the value expected for the water mass (–3.3) and the measured Nd of sediment pore fluid ( Nd PW ;–1.8). Moreover, Nd PW resembles the Nd of the sediment. Combined, these findings are consistent with recent assessments that sediment pore fluids may be a major source of rare earth elements to the ocean and suggest that the benthic flux of Nd from pore fluids exerts the primary control over the deep ocean distribution of Nd .
    Print ISSN: 0091-7613
    Electronic ISSN: 1943-2682
    Topics: Geosciences
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...