Biology subjects

de Kluijver, A.

Publications and source records attributed to de Kluijver, A..

3 recordsLinked to original sources

bioRxiv2024

Dissolved organic matter fluxes and fatty acid composition from shallow-water and deep-water demo- and hexactinellid sponges from New Zealand

Sponges are an important component of shallow- and deep-water ecosystems enhancing eukaryotic biodiversity via diverse endo- and epibiota and by providing three dimensional habitats for benthic invertebrates and fishes. Sponge biodiversity is particularly high in the waters around New Zealand (Southwest Pacific), where we collected two shallow- and two deep-water sponge species (Tedania sp., Suberea meandrina, Farrea raoulensis, Artemisina sp.) for ex-situ incubation experiments to detect whether these sponges may process dissolved organic matter. We assessed the biochemical and phospholipid-derived fatty acids (PLFAs) and measured dissolved organic carbon (DOC) and total dissolved nitrogen (TDN) fluxes. Changes in fluorescent dissolved organic matter (FDOM) over time were analyzed and the results were linked to the bacterial communities of the sponge holobiont. Dried sponge tissue consisted of 17.5 {+/-} 3.75% organic (org.) C and of 4.34 {+/-} 1.02% total nitrogen (TN) with a natural stable isotope composition of -19.0 {+/-}0.25{per thousand} for {delta}13org. C and of 10.2 {+/-}2.43{per thousand} for {delta}15TN. None of the DOC fluxes was significant and only the release of TDN by Tedania sp. was significantly different from 0 mol TDN g org. C-1 d-1. We detected the presence of four fluorophores in the FDOM pool: 2 tryptophan- and protein-like fluorophores (C1, C2), 1 humic-like fluorophore (C3), and 1 tyrosine-like fluorophore (C4). The maximum fluorescence intensity Fmax of C1 decreased significantly in S. meandrina incubations, whereas Fmax of C2 grew in the same incubations. Fmax of C3 increased in Tedania sp. incubations, in which Fmax of C4 decreased. In comparison, Fmax of C4 in S. meandrina rose. The PLFA composition of sponge tissue was dominated by long-chain fatty acids, saturated fatty acids, and monosaturated fatty acids and most PLFAs were sponge- and bacteria-specific. The bacterial community of the demosponges Artemisina sp., S. meandrina and Tedania sp. consisted mostly of Proteobacteria and Chloroflexota, whereas the dominating bacteria phylum of the hexactinellid F. raoulensis was Proteobacteria. We proposed that the holobionts of S. meandrina and Tedania sp. contain bacteria that are involved in the transformation and degradation of DOM. In S. meandrina, Chloroflexota and Poribacteria may degrade tryptophan-like fluorophores to a chemically modified tryptophan-like and protein-like fluorophore, while producing a tyrosine-like fluorophore. In Tedania sp., Chloroflexota may contribute to the release of significant amounts of TDN by producing humic-like fluorophores, while degrading tyrosine-like fluorophores. Farrea raoulensis may not take up DOM due to a lack of Poribacteria and Chloroflexota or may use colloidal instead of truly dissolved DOC.

ecology↗

bioRxiv2024

Nutrient fluxes, oxygen consumption and fatty acid composition from deep-water demo- and hexactinellid sponges from New Zealand

Sponges are an important component of deep-water ecosystems enhancing eukaryotic biodiversity by hosting diverse endo- and epibiota and providing three dimensional habitats for benthic invertebrates and fishes. As holobionts they are important hosts of microorganisms which are involved in carbon and nitrogen cycling. While increasing exploration of deep-water habitats results in new sponge species being discovered, little is known about their physiology and role in nutrient fluxes. Around New Zealand (Southwest Pacific), the sponge biodiversity is particularly high, and we selected six deep-sea sponge clusters (Saccocalyx, Suberites, Tedania, Halichondria/ Dendoricella, Sceptrulophora, Lissodendoryx) for in-situ and ex-situ experiments. We investigated the biochemical composition of the sponges, measured oxygen consumption and inorganic nutrient fluxes, as well as bacterial and phospholipid-derived fatty acid (PLFA) compositions. Our aim was to assess differences in fluxes and fatty acid composition among sponge clusters and linking their bacterial communities to nitrogen cycling processes. All sponges excreted nitrite and ammonia. Nitrate and phosphate excretion were independent of phylum affiliation (Demospongiae, Hexactinellida). Nitrate was excreted by the Halichondria/ Dendoricella and Lissodendoryx clusters, whereas the Suberites, Tedania, and Sceptrulophora clusters consumed it. Phosphate was excreted by Sceptrulophora and Halichondria/ Dendoricella clusters and consumed by all other clusters. Silicon was consumed by all sponge clusters, except for Saccocalyx and Halichondria/ Dendoricella clusters. Oxygen consumption rates ranged from 0.17 to 3.56{+/-}0.60 mmol O2 g C d-1. The PLFA composition was very sponge-cluster dependent and consisted mostly of long-chain fatty acids. Most PLFAs were sponge-specific, followed by bacteria-specific PLFAs, and others. All sponge clusters, except for Suberites, were low-microbial abundance (LMA) sponges whose bacterial community composition was dominated by Proteobacteria, Bacteroidota, Planctomycetota, and Nitrospinota. The Suberites cluster consisted of high-microbial abundance (HMA) sponges with Proteobacteria, Chloroflexota, Acidobacteriota, and Actinobacteriota as dominant bacteria. Based on the inorganic nitrogen flux measurements, we identified three types of nitrogen cycling in the sponges: In type 1, sponges (Dendoricella spp. indet., Lissodendoryx cluster) respired aerobically and ammonificated organic matter (OM) to ammonium, fixed N2 to ammonium, and nitrified aerobically heterotrophically produced ammonium to nitrate and nitrite. In type 2, sponges (Halichondria sp., Sceptrulophora, Suberites, Tedania clusters) respired OM aerobically and ammonificated it to ammonium. They also reduced nitrate anaerobically to ammonium via dissimilatory nitrate reduction to ammonium. In type 3, ammonium was microbially nitrified to nitrite and afterwards to nitrate presumably by ammonium-oxidizing Bacteria and/ or Archaea.

ecology↗

bioRxiv2020

Bacterial precursors and unsaturated long-chain fatty acids are biomarkers of North-Atlantic demosponges

Sponges produce distinct fatty acids (FAs) that (potentially) can be used as chemotaxonomic and ecological biomarkers to study endosymbiont-host interactions and the functional ecology of sponges. Here, we present FA profiles of five common habitat-building deep-sea sponges (class Demospongiae, order Tetractinellida), which are classified as high microbial abundance (HMA) species. Geodia hentscheli, G. parva, G. atlantica, G. barretti, and Stelletta rhaphidiophora were collected from boreal and Arctic sponge grounds in the North-Atlantic Ocean. Bacterial FAs dominated in all five species and particularly isomeric mixtures of mid-chain branched FAs (MBFAs, 8- and 9-Me-C16:0 and 10 and 11-Me-C18:0) were found in high abundance (together [≥] 20% of total FAs) aside more common bacterial markers. In addition, the sponges produced long-chain linear, mid- and a(i)-branched unsaturated FAs (LCFAs) with a chain length of 24-28 C atoms and had predominantly the typical {Delta}5,9 unsaturation, although also {Delta}9,19 and (yet undescribed) {Delta}11,21 unsaturations were identified. G. parva and S. rhaphidiophora each produced distinct LCFAs, while G. atlantica, G. barretti, and G. hentscheli produced similar LCFAs, but in different ratios. The different bacterial precursors varied in carbon isotopic composition ({delta}13C), with MBFAs being more enriched compared to other bacterial (linear and a(i)-branched) FAs. We propose biosynthetic pathways for different LCFAs from their bacterial precursors, that are consistent with small isotopic differences found in LCFAs. Indeed, FA profiles of deep-sea sponges can serve as chemotaxonomic markers and support the conception that sponges acquire building blocks from their endosymbiotic bacteria.

biochemistry↗