GLORIA

GEOMAR Library Ocean Research Information Access

Ihre E-Mail wurde erfolgreich gesendet. Bitte prüfen Sie Ihren Maileingang.

Leider ist ein Fehler beim E-Mail-Versand aufgetreten. Bitte versuchen Sie es erneut.

Vorgang fortführen?

Exportieren
  • 1
    In: Biogeosciences, Copernicus GmbH, Vol. 15, No. 20 ( 2018-10-26), p. 6315-6328
    Kurzfassung: Abstract. Manganese geochemistry in deep-sea sediments is known to vary greatly over the first few centimeters, which overlaps the in-sediment depth habitats of several benthic foraminiferal species. Here we investigated manganese incorporation in benthic foraminiferal shell carbonate across a six-station depth transect in the Gulf of Lions, NW Mediterranean, to unravel the impacts of foraminiferal ecology and Mn pore water geochemistry. Over this transect water depth increases from 350 to 1987 m, while temperature (∼13 ∘C) and salinity (∼38.5) remained relatively constant. Manganese concentrations in the tests of living (rose bengal stained) benthic foraminiferal specimens of Hoeglundina elegans, Melonis barleeanus, Uvigerina mediterranea, and Uvigerina peregrina were measured using laser ablation inductively coupled mass spectrometry (laser ablation ICP-MS). Pore water manganese concentrations show a decrease from shallow to deeper waters, which corresponds to a generally decreasing organic-matter flux with water depth. Differences in organic-matter loading at the sediment–water interface affects oxygen penetration depth into the sediment and hence Mn pore water profiles. Mn ∕ Ca values for the investigated foraminiferal species reflect pore water geochemistry and species-specific microhabitat in the sediment. The observed degree of variability within a single species is in line with known ranges in depth habitat and gradients in redox conditions. Both the Mn ∕ Ca ratio and interspecific variability hence reflect past Mn cycling and related early diagenetic processes within the sediment, making this a potential tool for bottom-water oxygenation and organic-matter fluxes. Dynamics of both in-sediment foraminiferal depth habitats and Mn cycling, however, limit the application of such a proxy to settings with relatively stable environmental conditions.
    Materialart: Online-Ressource
    ISSN: 1726-4189
    Sprache: Englisch
    Verlag: Copernicus GmbH
    Publikationsdatum: 2018
    ZDB Id: 2158181-2
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 2
    In: Biogeosciences, Copernicus GmbH, Vol. 16, No. 10 ( 2019-05-20), p. 2115-2130
    Kurzfassung: Abstract. Shell chemistry of foraminiferal carbonate proves to be useful in reconstructing past ocean conditions. A new addition to the proxy toolbox is the ratio of sulfur (S) to calcium (Ca) in foraminiferal shells, reflecting the ratio of SO42- to CO32- in seawater. When comparing species, the amount of SO42- incorporated, and therefore the S∕Ca of the shell, increases with increasing magnesium (Mg) content. The uptake of SO42- in foraminiferal calcite is likely connected to carbon uptake, while the incorporation of Mg is more likely related to Ca uptake since this element substitutes for Ca in the crystal lattice. The relation between S and Mg incorporation in foraminiferal calcite therefore offers the opportunity to investigate the timing of processes involved in Ca and carbon uptake. To understand how foraminiferal S∕Ca is related to Mg∕Ca, we analyzed the concentration and within-shell distribution of S∕Ca of three benthic species with different shell chemistry: Ammonia tepida, Bulimina marginata and Amphistegina lessonii. Furthermore, we investigated the link between Mg∕Ca and S∕Ca across species and the potential influence of temperature on foraminiferal S∕Ca. We observed that S∕Ca is positively correlated with Mg∕Ca on a microscale within specimens, as well as between and within species. In contrast, when shell Mg∕Ca increases with temperature, foraminiferal S∕Ca values remain similar. We evaluate our findings in the light of previously proposed biomineralization models and abiological processes involved during calcite precipitation. Although all kinds of processes, including crystal lattice distortion and element speciation at the site of calcification, may contribute to changes in either the amount of S or Mg that is ultimately incorporated in foraminiferal calcite, these processes do not explain the covariation between Mg∕Ca and S∕Ca values within specimens and between species. We observe that groups of foraminifera with different calcification pathways, e.g., hyaline versus porcelaneous species, show characteristic values for S∕Ca and Mg∕Ca, which might be linked to a different calcium and carbon uptake mechanism in porcelaneous and hyaline foraminifera. Whereas Mg incorporation might be controlled by Ca dilution at the site of calcification due to Ca pumping, S is linked to carbonate ion concentration via proton pumping. The fact that we observe a covariation of S and Mg within specimens and between species suggests that proton pumping and Ca pumping are intrinsically coupled across multiple scales.
    Materialart: Online-Ressource
    ISSN: 1726-4189
    Sprache: Englisch
    Verlag: Copernicus GmbH
    Publikationsdatum: 2019
    ZDB Id: 2158181-2
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 3
    In: Nature, Springer Science and Business Media LLC, Vol. 441, No. 7093 ( 2006-6), p. 610-613
    Materialart: Online-Ressource
    ISSN: 0028-0836 , 1476-4687
    RVK:
    RVK:
    RVK:
    Sprache: Englisch
    Verlag: Springer Science and Business Media LLC
    Publikationsdatum: 2006
    ZDB Id: 120714-3
    ZDB Id: 1413423-8
    SSG: 11
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 4
    Online-Ressource
    Online-Ressource
    Copernicus GmbH ; 2018
    In:  Biogeosciences Vol. 15, No. 7 ( 2018-04-16), p. 2205-2218
    In: Biogeosciences, Copernicus GmbH, Vol. 15, No. 7 ( 2018-04-16), p. 2205-2218
    Kurzfassung: Abstract. Accurate reconstructions of seawater salinity could provide valuable constraints for studying past ocean circulation, the hydrological cycle and sea level change. Controlled growth experiments and field studies have shown the potential of foraminiferal Na ∕ Ca as a direct salinity proxy. Incorporation of minor and trace elements in foraminiferal shell carbonate varies, however, greatly between species and hence extrapolating calibrations to other species needs validation by additional (culturing) studies. Salinity is also known to impact other foraminiferal carbonate-based proxies, such as Mg ∕ Ca for temperature and Sr ∕ Ca for sea water carbonate chemistry. Better constraints on the role of salinity on these proxies will therefore improve their reliability. Using a controlled growth experiment spanning a salinity range of 20 units and analysis of element composition on single chambers using laser ablation-Q-ICP-MS, we show here that Na ∕ Ca correlates positively with salinity in two benthic foraminiferal species (Ammonia tepida and Amphistegina lessonii). The Na ∕ Ca values differ between the two species, with an approximately 2-fold higher Na ∕ Ca in A. lessonii than in A. tepida, coinciding with an offset in their Mg content (∼ 35 mmol mol−2 versus ∼ 2.5 mmol mol−1 for A. lessonii and A. tepida, respectively). Despite the offset in average Na ∕ Ca values, the slopes of the Na ∕ Ca–salinity regressions are similar between these two species (0.077 versus 0.064 mmol mol−1 change per salinity unit). In addition, Mg ∕ Ca and Sr ∕ Ca are positively correlated with salinity in cultured A. tepida but show no correlation with salinity for A. lessonii. Electron microprobe mapping of incorporated Na and Mg of the cultured specimens shows that within chamber walls of A. lessonii, Na ∕ Ca and Mg ∕ Ca occur in elevated bands in close proximity to the primary organic lining. Between species, Mg banding is relatively similar, even though Mg content is 10 times lower and that variation within the chamber wall is much less pronounced in A. tepida. In addition, Na banding is much less prominent in this species than it is in A. lessonii. Inter-species differences in element banding reported here are hypothesized to be caused by differences in biomineralization controls responsible for element uptake.
    Materialart: Online-Ressource
    ISSN: 1726-4189
    Sprache: Englisch
    Verlag: Copernicus GmbH
    Publikationsdatum: 2018
    ZDB Id: 2158181-2
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 5
    Online-Ressource
    Online-Ressource
    Elsevier BV ; 2016
    In:  Journal of Experimental Marine Biology and Ecology Vol. 481 ( 2016-08), p. 9-14
    In: Journal of Experimental Marine Biology and Ecology, Elsevier BV, Vol. 481 ( 2016-08), p. 9-14
    Materialart: Online-Ressource
    ISSN: 0022-0981
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2016
    ZDB Id: 410283-6
    ZDB Id: 1483103-X
    SSG: 12
    SSG: 7,20
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 6
    In: Functional Ecology, Wiley, Vol. 36, No. 9 ( 2022-09), p. 2188-2199
    Kurzfassung: Ansammlungen von Tiefseeschwämmen (sog. Schwammböden) sind Hotspots der Biodiversität und Biomasse in der Tiefsee, ähnlich wie Oasen in der Wüste. Es bleibt weitgehend ungeklärt, wie Schwammböden in diesem nahrungsarmen Ökosystem überleben können. Hier entschlüsseln wir, wie Schwämme und deren zugehörige Fauna dort überleben können, indem wir ihre Nahrungsquellen und Wechselwirkungen innerhalb des Nahrungsnetzes identifizieren. Dafür haben wir die Isotopenzusammensetzung der Fauna und potentiellen Nahrungsquellen analysiert, was Rückschlüsse auf die Zusammensetzung ihrer Nahrung zulässt. Schwämme zeigten eine andere Isotopenzusammensetzung als von Filtrieren erwartet, abhängig von der Anzahl an Mikroben in ihrem Gewebe. Unsere Studie zeigt, dass Schwämme mit einer hohen Anzahl an Mikroorganismen, bei denen Mikroben bis zu 60 % der Schwammbiomasse ausmachen können, am Fuß des Nahrungsnetzes stehen. Dies deutet darauf hin, dass sie in der Lage sind, im Wasser gelöste Nährstoffe zu nutzen, die für Tiere im Allgemeinen unzugänglich sind. Im Kontrast dazu hatten Schwämme deren Anzahl an Mikroben zwei bis vier Größenordnungen niedriger sind, eine Isotopenzusammensetzung, die einem Raubtier an der Spitze des Nahrungsnetzes ähnelt. Dies scheint das Ergebnis sehr effizienter Recyclingwege zu sein, welche weiterhin unbekannt sind. Zusätzliche spezifische Isotopenanalysen, bei denen wir die Isotopenzusammensetzung der einzelnen Aminosäuren analysierten, zeigte eine realistischere Position von Schwämmen im Nahrungsnetz und ordneten Schwämme mit geringer Anzahl an Mikroben den Filtrierern zu, was ihrer zu erwartenden Ernährungsweise entspricht. Darüber hinaus konnten wir zeigen, dass die zugehörige Fauna sich auch von Schwämmen ernährte. Dies zeigt, dass Tiefseeschwammböden nicht dem klassischen Tiefseenahrungsnetz entsprechen und Schwämme eine zusätzliche Basis durch das Einbringen von Ressourcen in das Nahrungsnetz darstellen. Dadurch sind Schwämme der Schlüssel zur Erhaltung von lebendigen Tiefseeökosystemen wie Schwammböden und wahrscheinlich auch in vielen anderen Ökosystemen in denen sie vorkommen (z. B. Kaltwasserkorallenriffe), und könnten so Auswirkungen auf das globale Meeresökosystem sowie biogeochemische Kreisläufe haben.
    Materialart: Online-Ressource
    ISSN: 0269-8463 , 1365-2435
    URL: Issue
    Sprache: Englisch
    Verlag: Wiley
    Publikationsdatum: 2022
    ZDB Id: 2020307-X
    ZDB Id: 619313-4
    SSG: 12
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 7
    In: Nature, Springer Science and Business Media LLC, Vol. 450, No. 7173 ( 2007-12), p. 1218-1221
    Materialart: Online-Ressource
    ISSN: 0028-0836 , 1476-4687
    RVK:
    RVK:
    RVK:
    Sprache: Englisch
    Verlag: Springer Science and Business Media LLC
    Publikationsdatum: 2007
    ZDB Id: 120714-3
    ZDB Id: 1413423-8
    SSG: 11
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 8
    In: Applied and Environmental Microbiology, American Society for Microbiology, Vol. 77, No. 16 ( 2011-08-15), p. 5643-5654
    Kurzfassung: Sphagnum peatlands are important ecosystems in the methane cycle. Methane-oxidizing bacteria in these ecosystems serve as a methane filter and limit methane emissions. Yet little is known about the diversity and identity of the methanotrophs present in and on Sphagnum mosses of peatlands, and only a few isolates are known. The methanotrophic community in Sphagnum mosses, originating from a Dutch peat bog, was investigated using a pmoA microarray. A high biodiversity of both gamma- and alphaproteobacterial methanotrophs was found. With Sphagnum mosses as the inoculum, alpha- and gammaproteobacterial acidophilic methanotrophs were isolated using established and newly designed media. The 16S rRNA, pmoA , pxmA , and mmoX gene sequences showed that the alphaproteobacterial isolates belonged to the Methylocystis and Methylosinus genera. The Methylosinus species isolated are the first acid-tolerant members of this genus. Of the acidophilic gammaproteobacterial strains isolated, strain M5 was affiliated with the Methylomonas genus, and the other strain, M200, may represent a novel genus, most closely related to the genera Methylosoma and Methylovulum . So far, no acidophilic or acid-tolerant methanotrophs in the Gammaproteobacteria class are known. All strains showed the typical features of either type I or II methanotrophs and are, to the best of our knowledge, the first isolated (acidophilic or acid-tolerant) methanotrophs from Sphagnum mosses.
    Materialart: Online-Ressource
    ISSN: 0099-2240 , 1098-5336
    RVK:
    Sprache: Englisch
    Verlag: American Society for Microbiology
    Publikationsdatum: 2011
    ZDB Id: 223011-2
    ZDB Id: 1478346-0
    SSG: 12
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 9
    In: ICES Journal of Marine Science, Oxford University Press (OUP), Vol. 77, No. 3 ( 2020-05-01), p. 1167-1177
    Kurzfassung: Man-made structures in the North Sea are known to act as artificial reefs by providing a habitat for sessile epifauna in a predominantly soft sediment environment. This epifauna is hypothesized to cast a so-called “shadow” over the soft sediment ecosystem by altering the nutrient composition in the overlying water column. In addition, the structure itself could alter currents and thereby influence the deposition and erosion of the sediments in the wake of the platform. This study aims to assess the long-term effects of a gas platform in the southern North Sea on the surrounding benthic community by both morphological and molecular identification of benthic species. The species composition and a set of abiotic factors of the sediment around a gas platform were assessed along four transects. Differences for the abiotic factors were found in the closer vicinity of the platform in the direction corresponding to the predominant currents. The number of benthic fauna families found in the molecular approach were on average three times higher than for the morphological approach. Both approaches showed that small differences occurred primarily due to changes in sedimentary organic matter content. Differences in species composition were more pronounced between transects rather than between distances from the platform.
    Materialart: Online-Ressource
    ISSN: 1054-3139 , 1095-9289
    Sprache: Englisch
    Verlag: Oxford University Press (OUP)
    Publikationsdatum: 2020
    ZDB Id: 2463178-4
    ZDB Id: 1468003-8
    ZDB Id: 29056-7
    SSG: 12
    SSG: 21,3
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 10
    In: New Phytologist, Wiley, Vol. 217, No. 1 ( 2018-01), p. 453-466
    Kurzfassung: Dinitrogen fixation by Nostoc azollae residing in specialized leaf pockets supports prolific growth of the floating fern Azolla filiculoides . To evaluate contributions by further microorganisms, the A. filiculoides microbiome and nitrogen metabolism in bacteria persistently associated with Azolla ferns were characterized. A metagenomic approach was taken complemented by detection of N 2 O released and nitrogen isotope determinations of fern biomass. Ribosomal RNA genes in sequenced DNA of natural ferns, their enriched leaf pockets and water filtrate from the surrounding ditch established that bacteria of A. filiculoides differed entirely from surrounding water and revealed species of the order Rhizobiales. Analyses of seven cultivated Azolla species confirmed persistent association with Rhizobiales. Two distinct nearly full‐length Rhizobiales genomes were identified in leaf‐pocket‐enriched samples from ditch grown A .  filiculoides . Their annotation revealed genes for denitrification but not N 2 ‐fixation. 15 N 2 incorporation was active in ferns with N. azollae but not in ferns without. N 2 O was not detectably released from surface‐sterilized ferns with the Rhizobiales. N 2 ‐fixing N. azollae , we conclude, dominated the microbiome of Azolla ferns. The persistent but less abundant heterotrophic Rhizobiales bacteria possibly contributed to lowering O 2 levels in leaf pockets but did not release detectable amounts of the strong greenhouse gas N 2 O.
    Materialart: Online-Ressource
    ISSN: 0028-646X , 1469-8137
    URL: Issue
    Sprache: Englisch
    Verlag: Wiley
    Publikationsdatum: 2018
    ZDB Id: 208885-X
    ZDB Id: 1472194-6
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
Schließen ⊗
Diese Webseite nutzt Cookies und das Analyse-Tool Matomo. Weitere Informationen finden Sie hier...