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  • 1-(O-deoxyhexose)-3,25-hexacosanediol I, fractional abundance; 1-(O-deoxyhexose)-3,25-hexacosanediol II, fractional abundance; 1-(O-hexose)-3,25,27-octacosanetriol I, fractional abundance; 1-(O-hexose)-3,25,27-octacosanetriol II, fractional abundance; 1-(O-hexose)-3,25-hexacosanediol I, fractional abundance; 1-(O-hexose)-3,25-hexacosanediol II, fractional abundance; 1-(O-hexose)-3,27,29-triacontanetriol I, fractional abundance; 1-(O-hexose)-3,27,29-triacontanetriol II, fractional abundance; 1-(O-hexose)-3,27,29-triacontanetriol III, fractional abundance; 1-(O-hexose)-3,27-octacosanediol I, fractional abundance; 1-(O-hexose)-3,27-octacosanediol II, fractional abundance; 1-(O-hexose)-3,29,31-dotriacontanetriol I, fractional abundance; 1-(O-hexose)-3,29,31-dotriacontanetriol II, fractional abundance; 1-(O-hexose)-3,29-triacontanediol I, fractional abundance; 1-(O-hexose)-3,29-triacontanediol II, fractional abundance; 1-(O-hexose)-3-keto-25,27-octacosanediol I, fractional abundance; 1-(O-hexose)-3-keto-25,27-octacosanediol II, fractional abundance; 1-(O-hexose)-3-keto-25-hexacosanol I, fractional abundance; 1-(O-hexose)-3-keto-25-hexacosanol II, fractional abundance; 1-(O-hexose)-3-keto-27,29-triacontanediol I, fractional abundance; 1-(O-hexose)-3-keto-27,29-triacontanediol II, fractional abundance; 1-(O-hexose)-3-keto-27-octacosanol I, fractional abundance; 1-(O-hexose)-3-keto-27-octacosanol II, fractional abundance; 1-(O-hexose)-3-keto-29,31-dotriacontanediol I, fractional abundance; 1-(O-hexose)-3-keto-29,31-dotriacontanediol II, fractional abundance; 1-(O-hexose)-3-keto-29-triacontanol I, fractional abundance; 1-(O-hexose)-3-keto-29-triacontanol II, fractional abundance; 1-(O-pentose)-3,25-hexacosanediol I, fractional abundance; 1-(O-pentose)-3,25-hexacosanediol II, fractional abundance; 1-(O-pentose)-3,27,29-triacontanetriol I, fractional abundance; 1-(O-pentose)-3,27,29-triacontanetriol II, fractional abundance; 1-(O-pentose)-3,29,31-dotriacontanetriol I, fractional abundance; 1-(O-pentose)-3,29,31-dotriacontanetriol II, fractional abundance; 1-(O-pentose)-3,29-triacontanediol I, fractional abundance; 1-(O-pentose)-3,29-triacontanediol II, fractional abundance; Amundsen Sea; ANT-XXXII/3; AWI_Paleo; DEPTH, sediment/rock; Heterocyst diol index of 26 carbon atoms; Heterocyst diol index of 28 carbon atoms; Heterocyst triol index of 30 carbon atoms; MeBo70; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Paleo-surface water temperature; PIT-3; Polarstern; PS104; PS104_20-2; Sample code/label  (1)
  • Adaman_Sea_coral_reefs; BIOACID; Biological Impacts of Ocean Acidification; Burma Sea, Andaman Sea; Counts; EPOCA; European Project on Ocean Acidification; Event label; Figure; Mediterranean Sea Acidification in a Changing Climate; MedSeA; Sample code/label; Wave number  (1)
Document type
Keywords
Publisher
Years
  • 1
    facet.materialart.
    Unknown
    Raman spectra obtained at different skeletal region of the tropical coral Porites sp. (2015)
    PANGAEA
    In:  Supplement to: Wall, Marlene; Nehrke, Gernot (2012): Reconstructing skeletal fiber arrangement and growth mode in the coral Porites lutea (Cnidaria, Scleractinia): a confocal Raman microscopy study. Biogeosciences, 9(11), 4885-4895, https://doi.org/10.5194/bg-9-4885-2012
    Details
    Publication Date: 2023-02-24
    Description: Confocal Raman microscopy (CRM) mapping was used to investigate the microstructural arrangement and organic matrix distribution within the skeleton of the coral Porites lutea. Relative changes in the crystallographic orientation of crystals within the fibrous fan-system could be mapped, without the need to prepare thin sections, as required if this information is obtained by polarized light microscopy. Simultaneously, incremental growth lines can be visualized without the necessity of etching and hence alteration of sample surface. Using these methods two types of growth lines could be identified: one corresponds to the well-known incremental growth layers, whereas the second type of growth lines resemble denticle finger-like structures (most likely traces of former spines or skeletal surfaces). We hypothesize that these lines represent the outer skeletal surface before another growth cycle of elongation, infilling and thickening of skeletal areas continues. We show that CRM mapping with high spatial resolution can significantly improve our understanding of the micro-structural arrangement and growth patterns in coral skeletons.
    Keywords: Adaman_Sea_coral_reefs; BIOACID; Biological Impacts of Ocean Acidification; Burma Sea, Andaman Sea; Counts; EPOCA; European Project on Ocean Acidification; Event label; Figure; Mediterranean Sea Acidification in a Changing Climate; MedSeA; Sample code/label; Wave number
    Type: Dataset
    Format: text/tab-separated-values, 40431 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 2
    facet.materialart.
    Unknown
    Heterocyst glycolipids and SWT reconstruction of sediment cores 9R and 10R at site PS104_20-2 (2019)
    PANGAEA
    Details
    Publication Date: 2024-02-02
    Keywords: 1-(O-deoxyhexose)-3,25-hexacosanediol I, fractional abundance; 1-(O-deoxyhexose)-3,25-hexacosanediol II, fractional abundance; 1-(O-hexose)-3,25,27-octacosanetriol I, fractional abundance; 1-(O-hexose)-3,25,27-octacosanetriol II, fractional abundance; 1-(O-hexose)-3,25-hexacosanediol I, fractional abundance; 1-(O-hexose)-3,25-hexacosanediol II, fractional abundance; 1-(O-hexose)-3,27,29-triacontanetriol I, fractional abundance; 1-(O-hexose)-3,27,29-triacontanetriol II, fractional abundance; 1-(O-hexose)-3,27,29-triacontanetriol III, fractional abundance; 1-(O-hexose)-3,27-octacosanediol I, fractional abundance; 1-(O-hexose)-3,27-octacosanediol II, fractional abundance; 1-(O-hexose)-3,29,31-dotriacontanetriol I, fractional abundance; 1-(O-hexose)-3,29,31-dotriacontanetriol II, fractional abundance; 1-(O-hexose)-3,29-triacontanediol I, fractional abundance; 1-(O-hexose)-3,29-triacontanediol II, fractional abundance; 1-(O-hexose)-3-keto-25,27-octacosanediol I, fractional abundance; 1-(O-hexose)-3-keto-25,27-octacosanediol II, fractional abundance; 1-(O-hexose)-3-keto-25-hexacosanol I, fractional abundance; 1-(O-hexose)-3-keto-25-hexacosanol II, fractional abundance; 1-(O-hexose)-3-keto-27,29-triacontanediol I, fractional abundance; 1-(O-hexose)-3-keto-27,29-triacontanediol II, fractional abundance; 1-(O-hexose)-3-keto-27-octacosanol I, fractional abundance; 1-(O-hexose)-3-keto-27-octacosanol II, fractional abundance; 1-(O-hexose)-3-keto-29,31-dotriacontanediol I, fractional abundance; 1-(O-hexose)-3-keto-29,31-dotriacontanediol II, fractional abundance; 1-(O-hexose)-3-keto-29-triacontanol I, fractional abundance; 1-(O-hexose)-3-keto-29-triacontanol II, fractional abundance; 1-(O-pentose)-3,25-hexacosanediol I, fractional abundance; 1-(O-pentose)-3,25-hexacosanediol II, fractional abundance; 1-(O-pentose)-3,27,29-triacontanetriol I, fractional abundance; 1-(O-pentose)-3,27,29-triacontanetriol II, fractional abundance; 1-(O-pentose)-3,29,31-dotriacontanetriol I, fractional abundance; 1-(O-pentose)-3,29,31-dotriacontanetriol II, fractional abundance; 1-(O-pentose)-3,29-triacontanediol I, fractional abundance; 1-(O-pentose)-3,29-triacontanediol II, fractional abundance; Amundsen Sea; ANT-XXXII/3; AWI_Paleo; DEPTH, sediment/rock; Heterocyst diol index of 26 carbon atoms; Heterocyst diol index of 28 carbon atoms; Heterocyst triol index of 30 carbon atoms; MeBo70; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Paleo-surface water temperature; PIT-3; Polarstern; PS104; PS104_20-2; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 114 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
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