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
  • 18S (SSU) rRNA gene  (1)
  • Carbon isotopes  (1)
Document type
Keywords
Years
  • 1
    Publication Date: 2022-10-26
    Description: © The Author(s), 2022]. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Suter, E. A., Pachiadaki, M., Taylor, G. T., & Edgcomb, V. P. Eukaryotic parasites are integral to a productive microbial food web in oxygen-depleted waters. Frontiers in Microbiology, 12, (2022): 764605, https://doi.org/10.3389/fmicb.2021.764605.
    Description: Oxygen-depleted water columns (ODWCs) host a diverse community of eukaryotic protists that change dramatically in composition over the oxic-anoxic gradient. In the permanently anoxic Cariaco Basin, peaks in eukaryotic diversity occurred in layers where dark microbial activity (chemoautotrophy and heterotrophy) were highest, suggesting a link between prokaryotic activity and trophic associations with protists. Using 18S rRNA gene sequencing, parasites and especially the obligate parasitic clade, Syndiniales, appear to be particularly abundant, suggesting parasitism is an important, but overlooked interaction in ODWC food webs. Syndiniales were also associated with certain prokaryotic groups that are often found in ODWCs, including Marinimicrobia and Marine Group II archaea, evocative of feedbacks between parasitic infection events, release of organic matter, and prokaryotic assimilative activity. In a network analysis that included all three domains of life, bacterial and archaeal taxa were putative bottleneck and hub species, while a large proportion of edges were connected to eukaryotic nodes. Inclusion of parasites resulted in a more complex network with longer path lengths between members. Together, these results suggest that protists, and especially protistan parasites, play an important role in maintaining microbial food web complexity, particularly in ODWCs, where protist diversity and microbial productivity are high, but energy resources are limited relative to euphotic waters.
    Description: This work was supported by the National Science Foundation (NSF) grants (OCE-1336082 to VE and OCE-1335436 and OCE-1259110 to GT). The Cyverse infrastructure and resources are supported by the NSF under Award Numbers DBI-0735191, DBI-1265383, and DBI-1743442 (www.cyverse.org). Support was also provided by the Faculty Scholarship and Academic Advancement Committee at Molloy College.
    Keywords: 18S (SSU) rRNA gene ; Oxygen-depleted environment ; Oxygen minimum zone (OMZ) ; Protist ; Syndiniales ; Parasite ; Eukaryotes ; Network analysis
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2022-10-26
    Description: Author Posting. © American Geophysical Union, 2020. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research- Biogeosciences 125(2), (2020): e2019JG005276, doi:10.1029/2019JG005276.
    Description: A chemoautotrophy maximum is present in many anoxic basins at the sulfidic layer's upper boundary, but the factors controlling this feature are poorly understood. In 13 of 31 cruises to the Cariaco Basin, particulate organic carbon (POC) was enriched in 13C (δ13CPOC as high as −16‰) within the oxic/sulfidic transition compared to photic zone values (−23 to −26‰). During “heavy” cruises, fluxes of O2 and [NO3− + NO2−] to the oxic/sulfidic interface were significantly lower than during “light” cruises. Cruises with isotopically heavy POC were more common between 2013 and 2015 when suspended particles below the photic zone tended to be nitrogen rich compared to later cruises. Within the chemoautotrophic layer, nitrogen‐rich particles (molar ratio C/N〈 10) were more likely to be 13C‐enriched than nitrogen‐poor particles, implying that these inventories were dominated by living cells and fresh detritus rather than laterally transported or extensively decomposed detritus. During heavy cruises, 13C enrichments persisted to 1,300 m, providing the first evidence of downward transport of chemoautotrophically produced POC. Dissolved inorganic carbon assimilation during heavy cruises (n = 3) was faster and occurred deeper than during light cruises (n = 2). Metagenomics data from the chemoautotrophic layer during two cruises support prevalence of microorganisms carrying RuBisCO form II genes, which encode a carbon fixation enzyme that discriminates less against heavy isotopes than most other carbon fixation enzymes, and metatranscriptomics data indicate that higher expression of form II RuBisCO genes during the heavy cruises at depths where essential reactants coexist are responsible for the isotopically heavier POC.
    Description: We thank the captain and crew of the B/O Hermano Gines and the staff of Estación de Investigaciones Marinas, Fundación de la Salle de Ciencias Naturales, Margarita Island, Venezuela, for their field and laboratory assistance. We are also indebted to the many students, colleagues, and technicians who have participated in this project, in particular, L. Medina Faull for contour plots, E. Tappa (USC) for POC and δ13CPOC data measured in Robert Thunell's lab, and K. Fanning and K. Buck and W. Abbott (USF) for nutrient data. Digna‐Rueda‐Roa, Laura Lorenzoni, and Matt Biddle assisted greatly in getting the data into a format suitable for submission to the BCO‐DMO database. We are also grateful to two anonymous reviewers for their insightful comments. This research was supported by grants from NSF (OCE‐1259110 awarded to M. I. S. and G. T. T.; OCE‐1258991 to R. C. T.; OCE‐0326268, OCE‐0963028, OCE‐1259043, and OCE‐1649626 to F. M. K.; and OCE‐1336082 and OCE‐1335436 awarded to V. P. E. and G. T. T., respectively), from Venezuela's FONACIT (2000001702 and 2011000353 to Y. A.), and a WHOI subaward A101259 to M. G. P. Biological and Chemical Oceanography Data Management Office Metadata landing page for the Cariaco Time series Niskin bottle data is/https://www.bco‐dmo.org/dataset/3093. For the data from our biogeochemistry cruises the BCO‐DMO Metadata landing page is https://ww.bco‐dmo.org/dataset/3120 and for the Time series CTD data is https://www.bco‐dmo.org/dataset/3092. δ13CDIC data are presented in Table S1. Metagenome and metatranscriptome data are available from SRA (accession number PRJNA544741). δ13CPOC data are available at https://doi.org/10.6084/m9.figshare.8214470.v1.
    Description: 2020-07-30
    Keywords: Cariaco Basin ; Chemoautotrophy ; Metagenomics ; Carbon isotopes
    Repository Name: Woods Hole Open Access Server
    Type: Article
    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...