Dataset: Lost City hydrothermal fluids sequence data
View Data: Data not available yet
Data Citation:
Brazelton, W. (2023) Lost City hydrothermal fluids sequence data from R/V Atlantis AT42-01 in the Lost City hydrothermal field from September to October 2018 (Lost City Limits to Life project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2023-06-27 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/897962 [access date]
Terms of Use
This dataset is licensed under Creative Commons Attribution 4.0.
If you wish to use this dataset, it is highly recommended that you contact the original principal investigators (PI). Should the relevant PI be unavailable, please contact BCO-DMO (info@bco-dmo.org) for additional guidance. For general guidance please see the BCO-DMO Terms of Use document.
Spatial Extent: N:30.2708 E:30.2708 S:-42.1246 W:30.0054
Temporal Extent: 2018-09-08 - 2018-10-01
Principal Investigator:
William Brazelton (University of Utah)
Contact:
William Brazelton (University of Utah)
BCO-DMO Data Manager:
Sawyer Newman (Woods Hole Oceanographic Institution, WHOI BCO-DMO)
Version:
1
Version Date:
2023-06-27
Restricted:
No
Validated:
No
Current State:
Preliminary and in progress
Lost City hydrothermal fluids sequence data from R/V Atlantis AT42-01 in the Lost City hydrothermal field from September to October 2018 (Lost City Limits to Life project)
Abstract:
Hydrothermal fluid samples were collected from actively venting chimneys at the Lost City hydrothermal field using ROV Jason during the 2018 Lost City expedition aboard R/V Atlantis (AT42-01). This study includes 39 samples of hydrothermal fluids that were dedicated to DNA and RNA sequencing, including analyses of amplicon sequence variants (ASVs), metagenomes, and metatranscriptomes. The present study included hydrothermal fluid samples from seven chimney locations: Camel Humps, Sombrero, Marker 3, Marker C, Calypso, Marker 2, and Marker 8. Several fluid samples collected from the Beehive chimney, where the highest fluid temperatures have been measured, yielded only low-quality DNA sequences and are not included in this study. The Sombrero site was sampled on two different ROV Jason dives, and samples from the separate dives are labeled as Sombrero1 or Sombrero2 when appropriate. Fluid samples collected from Markers C, 2, 3, and 8 were included in an early microbial diversity study (Brazelton et al., 2006), but microbial diversity data from the other chimneys are reported here for the first time. The fluid samples ranged from those that were barely distinguishable from ambient seawater (~11 ºC, pH 8) to warm and highly alkaline hydrothermal fluids (~80 ºC, pH 10). Direct counts of visible cells showed little variability among fluids, with densities approximately 2-8 × 104 mL-1 in all samples, although the two samples with the highest temperatures had the least number of cells.