Download URLhttps://www.bco-dmo.org/dataset/782742/data/download
Media Type text/tab-separated-values
Created November 22, 2019
Modified July 14, 2020
State Final no updates expected

Acquisition Description

Sediment samples were stored at 4°C prior to analysis. Proteinaceous material was extracted and quantified with Qubit fluorescent reagent (Life Technologies), following Estes et al. (2016) as modified from Ehrenreich and Widdel (1994).

Assay was quantified using bovine serum albumin standard (Bio-Rad).

See Estes el al. 2019, for complete methods.

Processing Description

BCO-DMO Data Manager Processing Notes:
* exported data in xlsx file “Estes protein data.xlsx” to csv file
* added a conventional header with dataset name, PI name, version date
* modified parameter names to conform with BCO-DMO naming conventions
* blank values in this dataset are displayed as “nd” for “no data.”  nd is the default missing data identifier in the BCO-DMO system.
* latitude and longitude in degrees decimal minutes converted to decimal degrees then rounded to 5 decimal places.
* protein and prot_stdev rounded to two decimal places
* date format converted to ISO 8601 format yyyy-mm-dd


The gravity corer allows researchers to sample sediment layers at the bottom of lakes or oceans. The coring device is deployed from the ship and gravity carries it to the seafloor. (http://www.whoi.edu/instruments/viewInstrument.do?id=1079).

The JOIDES Resolution's Advanced Piston Corer (APC) is used in soft ooze and sediments. The APC is a hydraulically actuated piston corer designed to recover relatively undisturbed samples from very soft to firm sediments.

More information is available from IODP (PDF).

The piston corer is a type of bottom sediment sampling device. A long, heavy tube is plunged into the seafloor to extract samples of mud sediment. A piston corer uses a "free fall" of the coring rig to achieve a greater initial force on impact than gravity coring. A sliding piston inside the core barrel reduces inside wall friction with the sediment and helps to evacuate displaced water from the top of the corer. A piston corer is capable of extracting core samples up to 90 feet in length.
The Multi Corer is a benthic coring device used to collect multiple, simultaneous, undisturbed sediment/water samples from the seafloor. Multiple coring tubes with varying sampling capacity depending on tube dimensions are mounted in a frame designed to sample the deep ocean seafloor. For more information, see Barnett et al. (1984) in Oceanologica Acta, 7, pp. 399-408.


location [site]
Sample origin
Sampling site identification.
expedition [cruise_id]
Cruise name
cruise designation; name
site [site]
Site number
Sampling site identification.
latitude [latitude]


latitude, in decimal degrees, North is positive, negative denotes South; Reported in some datasets as degrees, minutes

longitude [longitude]


longitude, in decimal degrees, East is positive, negative denotes West; Reported in some datsets as degrees, minutes

water_depth [depth]
Water depth

Observation/sample depth below the sea surface. Units often reported as: meters, feet.

When used in a JGOFS/GLOBEC dataset the depth is a best estimate; usually but not always calculated from pressure; calculated either from CTD pressure using Fofonoff and Millard (1982; UNESCO Tech Paper #44) algorithm adjusted for 1980 equation of state for seawater (EOS80) or simply equivalent to nominal depth as recorded during sampling if CTD pressure was unavailable.

core_type [sample_type]
Coring device used
text description of type of sample collected (rock, bio, fluid, etc)
Sample depth (meters below seafloor)

Meters below seafloor (mbsf); convention used for depths below the seabed in geology, oceanography, petrology and ocean drilling; often used in reporting measurements made from sediment cores.

protein [proteins]
Content of proteinaceous material

Protein concentration


prot_stdev [proteins]

Standard deviation of the content of proteinaceous material (triplicate analyses).

Protein concentration


date [date]

date sample collection in ISO 8601 format yyyy-mm-dd

date; generally reported in GMT as YYYYMMDD (year; month; day); also as MMDD (month; day); EqPac dates are local Hawaii time. ISO_Date format is YYYY-MM-DD (http://www.iso.org/iso/home/standards/iso8601.htm)

Dataset Maintainers

Emily R. EstesTexas A&M University (TAMU)
Colleen M. HanselTexas A&M University (TAMU)
Amber YorkWoods Hole Oceanographic Institution (WHOI)
Amber YorkWoods Hole Oceanographic Institution (WHOI)
Amber YorkWoods Hole Oceanographic Institution (WHOI BCO-DMO)

BCO-DMO Project Info

Project Title Elucidating the extent and composition of mineral-hosted carbon in the deep biosphere
Acronym Org C Sed I
Created October 16, 2019
Modified October 16, 2019
Project Description

Abstract from the C-DEBI project page:

Minerals have recently been identified as a primary host for organic carbon (OC) within marine sediments. This strong physical and chemical carbon-mineral association is believed to reduce, and in some cases completely eliminate, the bioavailablilty of this carbon for microbial life. The paucity of information regarding the nature of this carbon-mineral association and the composition of the hosted carbon, however, precludes our ability to predict the ultimate fate of this OC and its involvement in deep subsurface life. Here, we addressed this knowledge gap by using a suite of bulk and spatially-resolved geochemical and mineralogical techniques to characterize OC-mineral associations within the deep subsurface. We characterized sediment samples collected on the 2014 North Atlantic long coring expedition (KN223) in the western subtropical North Atlantic that included three geochemically distinct long cores to a depth of 24-30 m and spanned OC-limited oxic to anoxic sediments. We find measurable and relevant OC concentrations throughout the sediment cores, that decreases linearly over ~25 meters burial depth, from ~0.15 to 0.075 mol OC/kg solid. OC within the sediments is compositionally complex on both a macro- and micro-scale, spanning a gradient of lability even at depth. Proteins are observed throughout the sediment depth profiles, where they appear to constitute a substantial fraction of the TOC. Correspondingly, a low C:N ratio is observed, consistent with proteinaceous carbon within the sediments. In sum, these findings point to a substantial mineral-hosted OC reservoir within the deep subsurface that may fuel the deep biosphere and select for protein-based heterotrophy.

Data Project Maintainers
Colleen M. HanselWoods Hole Oceanographic Institution (WHOI)Principal Investigator
Gariela FarfanWoods Hole Oceanographic Institution (WHOI)Co-Principal Investigator
Emily R. EstesWoods Hole Oceanographic Institution (WHOI)Co-Principal Investigator

BCO-DMO Project Info

Project Title Geochemical controls on organic carbon quantity and quality in the deep subsurface
Acronym Org C Sed II
Created October 15, 2019
Modified October 16, 2019
Project Description

Abstract from the C-DEBI project page:

Sediment underlying ocean gyres receives minimal input of fresh organic matter yet sustains a small but active heterotrophic microbial community. The concentration and composition of the organic carbon (OC) available to this deep biosphere however is unknown. We analyzed the content and composition of OC in pelagic sediment in order to identify mechanism(s) that dictate the balance between OC preservation and utilization by microorganisms. Sediment cores from the North Atlantic gyre (KN223), South Pacific Gyre (Knox02-RR), and Peru Basin (IODP site 1231) allowed for a global comparison and a test of how sediment lithology and redox state affect OC preservation. OC was present in low concentrations in all samples (0.01—0.61%), at depths up to 112 meters below seafloor and estimated sediment ages of up to 50 million years. Synchrotron-based near edge X-ray absorption fine structure (NEXAFS) spectroscopy was conducted on over 100 samples, one of the first applications of NEXAFS to sedimentary environments. NEXAFS revealed an OC reservoir dominated by amide and carboxylic functionalities in a scaffolding of O-alkyl and aliphatic carbons. Detection of extractable, extracellular proteins supports this composition and suggests that sedimentary OC is protein-derived. This composition was common across all sites and depths, implicating physical rather than chemical mechanisms in OC preservation on long timescales. This study thereby points to physical access rather than energy or metabolic potential as a key constraint on subsurface heterotrophic life.

Data Project Maintainers
Emily R. EstesWoods Hole Oceanographic Institution (WHOI)Principal Investigator