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  • 2020-2023  (2)
  • 2020-2022  (1)
  • 2021  (3)
  • 2021  (3)
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  • 1
    Publication Date: 2021-12-08
    Description: The simulation of deep-sea conditions in laboratories is technically challenging but necessary for experiments that aim at a deeper understanding of physiological mechanisms or host-symbiont interactions of deep-sea organisms. In a proof-of-concept study, we designed a recirculating system for long-term culture (〉2 years) of deep-sea mussels Gigantidas childressi (previously Bathymodiolus childressi). Mussels were automatically (and safely) supplied with a maximum stable level of ~60 µM methane in seawater using a novel methane-air mixing system. Experimental animals also received daily doses of live microalgae. Condition indices of cultured G. childressi remained high over years, and low shell thickness growth could be detected, which is indicative of positive energy budgets. Using stable isotope data, we demonstrate that G. childressi in our culture system gained energy, both, from digestion of methane oxidizing endosymbionts and from digesting particulate food (microalgae). Limitations of the system, as well as opportunities for future experimental approaches involving deep-sea mussels are discussed.
    Type: Article , NonPeerReviewed
    Format: text
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  • 2
    Publication Date: 2022-01-10
    Description: Benthic foraminifera are unicellular eukaryotes that inhabit sediments of aquatic environments. Several foraminifera of the order Rotaliida are known to store and use nitrate for denitrification, a unique energy metabolism among eukaryotes. The rotaliid Globobulimina spp. has been shown to encode an incomplete denitrification pathway of bacterial origins. However, the prevalence of denitrification genes in foraminifera remains unknown and the missing denitrification pathway components are elusive. Analysing transcriptomes and metagenomes of ten foraminifera species from the Peruvian oxygen minimum zone, we show that denitrification genes are highly conserved in foraminifera. We infer of the last common ancestor of denitrifying foraminifera, which enables us to predict further denitrifying species. Additionally, an examination of the foraminifera microbiota reveals evidence for a stable interaction with Desulfobacteracea , which harbour genes that complement the foraminifera denitrification pathway. Our results provide evidence that foraminiferal denitrification is complemented by the foraminifera microbiome. The interaction of Foraminifera with their resident bacteria is at the basis of foraminifera adaptation to anaerobic environments that manifested in ecological success within oxygen depleted habitats.
    Type: Article , NonPeerReviewed
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  • 3
    Publication Date: 2022-12-22
    Type: Report , NonPeerReviewed
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