Depth profiles of lipid biomarkers from R/V Kilo Moana KM1314 in the North Pacific Ocean (Seattle to Honolulu, Line P, Station ALOHA), Aug-Sept 2013

Website: https://www.bco-dmo.org/dataset/997800
Version: 1
Version Date: 2026-04-30

Project
» Significance of nitrification in shaping planktonic biodiversity in the ocean (Nitrification and Marine Planktonic Biodiversity)

Program
» Dimensions of Biodiversity (Dimensions of Biodiversity)
ContributorsAffiliationRole
Qin, WeiUniversity of Illinois Urbana-Champaign (UIUC)Principal Investigator
Shen, HuiUniversity of Illinois Urbana-Champaign (UIUC)Contact, Technician
Soenen, KarenWoods Hole Oceanographic Institution (WHOI BCO-DMO)BCO-DMO Data Manager

Abstract
This dataset contains in situ temperature (°C), TEX86-derived temperature (°C), and isoprenoid concentrations (ng L−1) measured from 0 to 300 m depth at Stations 5, 8, and 13 in the Northeastern Pacific Ocean during the R/V Kilo Moana cruise KM1314 in August 2013. Samples were collected to characterize vertical variations in archaeal lipid biomarkers and evaluate the relationship between TEX86 paleotemperature estimates and ambient water column temperature. In situ temperatures were obtained from CTD measurements, TEX86 values were calculated from the relative abundances of GDGT-1, GDGT-2, GDGT-3, and the crenarchaeol regioisomer, and TEX86-derived temperatures were reconstructed using a published calibration equation. These data were generated to assess how environmental gradients influence archaeal lipid distributions and the accuracy of TEX86 temperature reconstructions in the upper ocean.


Coverage

Spatial Extent: N:50 E:-134.68034444 S:30 W:-150
Temporal Extent: 2013-08-14 - 2013-08-29

Methods & Sampling

Samples were collected onboard the R/V Kilo Moana between 8/7 and 9/5 2013. At Stations 5, 8, and 13, seawater samples (1 L per depth) were collected by Niskin bottles attached at CTD ,and then filtered onto 0.22 μm Durapore membrane filters (Millipore Co.) for archaeal lipid extraction.


Data Processing Description

 Isoprenoidal GDGTs (glycerol dibiphytanyl glycerol tetraethers) were subsequently extracted from the filters. Lipid extracts were analyzed by atmospheric pressure chemical ionization on an Agilent 1100 Series liquid chromatograph coupled to an Agilent ion trap mass spectrometer. Detailed methodologies for archaeal lipid extraction and analysis are described in Qin et al. (2015). TEX86 values were calculated based on the relative abundances of GDGT-1, GDGT-2, GDGT-3, and crenarchaeol regioisomer (Cren’), using their respective peak areas according to the following equation in Qin et al. 2015.


[ table of contents | back to top ]

Related Publications

...retrieving the citation from: /osprey_data_entry/citation-formatter/488/10.1073%252Fpnas.150156811/520 as text/x-bibliography; style=apa https://doi.org/10.1073/pnas.150156811
Methods

[ table of contents | back to top ]

Related Datasets

IsDerivedFrom
Devol, A., Moffett, J. W., Ingalls, A. E., Armbrust, E., Stahl, D. A. (2014) Bottle data from R/V Kilo Moana KM1314 in the The North Pacific Ocean (Seattle to Honolulu, including Line P, Station ALOHA), Aug - Sept 2013 (Nitrification and Marine Planktonic Biodiversity project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 2014-11-14) Version Date 2014-11-14 http://lod.bco-dmo.org/id/dataset/539724 [view at BCO-DMO]
Devol, A., Moffett, J. W., Ingalls, A. E., Armbrust, E., Stahl, D. A. (2014) CTD data from R/V Kilo Moana KM1314 in the The North Pacific Ocean (Seattle to Honolulu, including Line P, Station ALOHA), Aug - Sept 2013 (Nitrification and Marine Planktonic Biodiversity project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 2014-11-24) Version Date 2014-11-24 http://lod.bco-dmo.org/id/dataset/539810 [view at BCO-DMO]
IsRelatedTo
Stahl, D. A., Devol, A., Moffett, J. W., Ingalls, A. E., Armbrust, E. (2017) Ammonia oxidation rate profiles from R/V Kilo Moana KM1314 in the North Pacific Ocean (Seattle to Honolulu, Line P, Station ALOHA), Aug-Sept 2013 (Nitrification and Planktonic Biodiversity project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). Version Date 2017-01-04 http://lod.bco-dmo.org/id/dataset/672310 [view at BCO-DMO]

[ table of contents | back to top ]

Parameters

ParameterDescriptionUnits
Datetime_of_sampling

Date and time of sampling in UTC time zone

unitless
Latitude

Latitude of sampling location

decimal degrees
Longitude

Longitude of sampling location

decimal degrees
Station_ID

Station identification

unitless
Depth_m

Depth of sampling

meters (m)
insitu_T_degC

in situ temperature at depth of sampling

degrees Celsius (°C)
TEX86_derived_temperature_degC

TEX86 values were calculated based on the relative abundances of GDGT-1, GDGT-2, GDGT-3, and the crenarchaeol regioisomer. TEX₈₆-derived temperatures were reconstructed using the calibration equation in https://doi.org/10.1073/pnas.1501568112.

degrees Celsius (°C)
Isoprenoid_ng_per_L

Concentration of Isoprenoid

nano gram per liter (ng/L)


[ table of contents | back to top ]

Instruments

Dataset-specific Instrument Name
CTD SBE 911plus
Generic Instrument Name
CTD Sea-Bird SBE 911plus
Generic Instrument Description
The Sea-Bird SBE 911 plus is a type of CTD instrument package for continuous measurement of conductivity, temperature and pressure. The SBE 911 plus includes the SBE 9plus Underwater Unit and the SBE 11plus Deck Unit (for real-time readout using conductive wire) for deployment from a vessel. The combination of the SBE 9 plus and SBE 11 plus is called a SBE 911 plus. The SBE 9 plus uses Sea-Bird's standard modular temperature and conductivity sensors (SBE 3 plus and SBE 4). The SBE 9 plus CTD can be configured with up to eight auxiliary sensors to measure other parameters including dissolved oxygen, pH, turbidity, fluorescence, light (PAR), light transmission, etc.). more information from Sea-Bird Electronics

Dataset-specific Instrument Name
Agilent 1100 Series liquid chromatograph
Generic Instrument Name
High-Performance Liquid Chromatograph
Dataset-specific Description
Agilent 1100 Series liquid chromatograph coupled to an Agilent ion trap mass spectrometer
Generic Instrument Description
A High-performance liquid chromatograph (HPLC) is a type of liquid chromatography used to separate compounds that are dissolved in solution. HPLC instruments consist of a reservoir of the mobile phase, a pump, an injector, a separation column, and a detector. Compounds are separated by high pressure pumping of the sample mixture onto a column packed with microspheres coated with the stationary phase. The different components in the mixture pass through the column at different rates due to differences in their partitioning behavior between the mobile liquid phase and the stationary phase.

Dataset-specific Instrument Name
Agilent ion trap mass spectrometer
Generic Instrument Name
Mass Spectrometer
Dataset-specific Description
Agilent 1100 Series liquid chromatograph coupled to an Agilent ion trap mass spectrometer
Generic Instrument Description
General term for instruments used to measure the mass-to-charge ratio of ions; generally used to find the composition of a sample by generating a mass spectrum representing the masses of sample components.

Dataset-specific Instrument Name
Niskin Bottle
Generic Instrument Name
Niskin bottle
Generic Instrument Description
A Niskin bottle (a next generation water sampler based on the Nansen bottle) is a cylindrical, non-metallic water collection device with stoppers at both ends. The bottles can be attached individually on a hydrowire or deployed in 12, 24, or 36 bottle Rosette systems mounted on a frame and combined with a CTD. Niskin bottles are used to collect discrete water samples for a range of measurements including pigments, nutrients, plankton, etc.


[ table of contents | back to top ]

Deployments

KM1314

Website
Platform
R/V Kilo Moana
Start Date
2013-08-07
End Date
2013-09-05


[ table of contents | back to top ]

Project Information

Significance of nitrification in shaping planktonic biodiversity in the ocean (Nitrification and Marine Planktonic Biodiversity)


Microorganisms sustain the biogeochemical cycling of nitrogen, one of the most important nutrient cycles on earth. A key step in this cycle, the oxidation of ammonia to nitrite by autotrophic microorganisms, was for a century thought mediated by a few restricted bacterial genera. Significant ammonia oxidation, perhaps most, is now attributed to a previously enigmatic group of Archaea - the ammonia-oxidizing archaea (AOA) - of high abundance in both marine and terrestrial environments. The investigators prior physiological and environmental analyses, the foundation for this proposal, have shown that AOA are active within the marine photic zone and that their competitive fitness in the marine environment is at least in part attributable to an extremely high affinity for ammonia, growing at near maximum growth rates at concentrations of ammonia that would not sustain known bacterial ammonia oxidizers, and an unusual copper-based respiratory system that may render them more competitive in iron limited environments. The compelling inference from these prior analyses is that AOA alter and possibly control the forms of fixed nitrogen available to other microbial assemblages within the photic zone by converting ammonia, a nearly universally available form of nitrogen, into nitrite, a form only available to nitrite oxidizing bacteria and some phytoplankton. If correct, this has a significant impact on biodiversity.

The PIs will use the most recent technological advances in protein and high throughput sequencing to evaluate the significance of nitrification in shaping biodiversity (genomic and metagenomics), activity (transcriptome, proteome and stable isotope probing), and in controlling availability of an important trace element (copper). In turn, by resolving the environmental and biotic variables that influence the diversity, distribution and activity of AOA, they will advance general understanding of their taxonomy. More directly, functional knowledge of the contribution of AOA to regenerated nitrate will improve estimates of new ocean production ("biological pump") based on nitrate assimilation, which in the past has mostly neglected the importance of nitrification as a major source of nitrate. Together these studies will transform understanding of the marine nitrogen cycle, estimates of new production, and will ultimately provide a better understanding of the impact of human activity on this critical nutrient cycle.

The nitrogen cycle has been profoundly affected by anthropogenic inputs of reactive nitrogen into terrestrial, marine, and atmospheric systems having, or predicted to have, major impacts on marine biological production, increased N20 emissions, nitrogen pollution, and eutrophication. Likewise, there is a poor understanding of the relationship between nitrogen cycling and productivity in marine ecosystems. Marine systems are increasingly affected by ocean acidification and by atmospheric inputs of reactive nitrogen. Since both changes greatly alter nitrogen available to microorganisms, the characterization of the response of these environmentally relevant AOA is of tremendous relevance to understanding the affect of acidification and anthropogenic nitrogen inputs on major ocean processes.

The proposed project encompasses and integrates the three dimensions (functional genetic, and taxonomic) of biodiversity. First, the project is framed by function: microbial control of one of the most important nutrient cycles on earth, the nitrogen-cycle. Second, it is motivated by recent genetic analyses that associate activities of a novel clade of Archaea (provisionally assigned to a new kingdom within the Archaea, the Thaumarchaeota) with control of ammonia oxidation in the ocean. Third, it is built upon a compelling synthesis of physiological and environmental data that lead to its central hypothesis that by altering and possibly controlling the form of nitrogen, the AOA also alter biodiversity and ecological function in one of the most productive environments on earth. It identifies a specific taxonomic imperative. The tremendous genetic diversity among the globally abundant AOA catalogued almost exclusively by gene sequencing surveys and therefore lacking formal description makes it essential to resolve membership into ecologically relevant groups or clades as a prelude to developing a formal taxonomy. The investigators have assembled a group of researchers with specific expertise in each of dimension and uniquely qualified to address the research objectives outlined in an integrative way.



[ table of contents | back to top ]

Program Information

Dimensions of Biodiversity (Dimensions of Biodiversity)


Coverage: global


(adapted from the NSF Synopsis of Program)
Dimensions of Biodiversity is a program solicitation from the NSF Directorate for Biological Sciences. FY 2010 was year one of the program.  [MORE from NSF]

The NSF Dimensions of Biodiversity program seeks to characterize biodiversity on Earth by using integrative, innovative approaches to fill rapidly the most substantial gaps in our understanding. The program will take a broad view of biodiversity, and in its initial phase will focus on the integration of genetic, taxonomic, and functional dimensions of biodiversity. Project investigators are encouraged to integrate these three dimensions to understand the interactions and feedbacks among them. While this focus complements several core NSF programs, it differs by requiring that multiple dimensions of biodiversity be addressed simultaneously, to understand the roles of biodiversity in critical ecological and evolutionary processes.



[ table of contents | back to top ]

Funding

Funding SourceAward
NSF Division of Ocean Sciences (NSF OCE)

[ table of contents | back to top ]