19:I[42426,["/_next/static/immutable/chunks/1xctgzqre-wsy.js","/_next/static/immutable/chunks/06_-wz6pdtp2b.js","/_next/static/immutable/chunks/30e52g49hg40p.js","/_next/static/immutable/chunks/02yq6tul2z-oh.js","/_next/static/immutable/chunks/10bx_ec2vj7n_.js","/_next/static/immutable/chunks/33bfn03fo8xnt.js","/_next/static/immutable/chunks/0tfjf78scu61b.js","/_next/static/immutable/chunks/31xnvej4n1bi9.js"],"default"] 1a:Tbc8,

All methodology was described in Ladd & Sachs, GCA, 2017, doi: 10.1016/j.gca.2017.01.046

Surface water and precipitation δ2H and δ18O values were measured with a Picarro Cavity Ring Down Spectroscopy (CRDS) L2130i Water Isotope Analyzer at the University of Washington measured. Three laboratory standards of known isotopic composition were analyzed after every six samples and were used to normalize results to the Vienna Standard Mean Ocean Water (VSMOW) scale. All samples and standards were injected six times, and the first three measurements were discarded in order to avoid any memory effects from the previous analysis. Leaf and xylem water samples were analyzed by a Thermal Conversion Elemental Analyzer (TC/EA) coupled to a Delta V Isotope Ratio Mass Spectrometer (IRMS; ThermoFisher Scientific, Waltham, MA) at the University of Basel, Switzerland. Each sample and standard was injected six times in sequence. In order to avoid any memory effects from the previous analysis, the first three injections of each sample were discarded.

The δ2H values of individual lipids were measured by GC-IRMS on a Thermo DELTA V PLUS system (ThermoFisher Scientific, Waltham, MA, USA). The GC (Trace Ultra, ThermoFisher Scientific) was equipped with a split-splitless injector operated in splitless mode at 320 deg C, a TRIPLUS autosampler (ThermoFisher Scientific), and a VF-17ms capillary column (60 m X 0.25 mm X 0.25 um, Agilent). For lupeol analyses, the GC was heated from 120 deg C to 260 deg C at 20 deg C/min, then at 1 deg C/min to 300 deg C, at 20 deg C/min to 325 deg C and then held at 325 deg C for 20 min. For n-alkane analyses, the GC was heated from 120 deg C to 250 deg C at 20 deg C/min, then at 6 deg C/min to 325 deg C and then held at 325 deg C for 12 min. Helium was used as the carrier gas at a constant flow of 1.1 mL/min. Compounds were pyrolyzed in a ceramic reactor at 1400 deg C. 1 uL of sample was injected along with 0.5 uL of a mix of n-alkanes of known isotopic composition (A. Schimmelmann, Indiana University, Bloomington, Indiana). For lupeol analyses, this mix included nC26-, nC28-, nC32-, nC34- and nC41-alkanes. For n-alkane analyses, the co-injection standards were nC21 and nC23. At the beginning and the end of the sequence, as well as after every 4-6 sample injections, a mixture of additional n-alkane standards of known isotopic composition was analyzed with the co-injection standards, in place of a sample. For isoprenoid sequences, this external standard was nC38-alkane. For n-alkane sequences, nC28-, nC32- and nC34-alkanes were used as external standards.

BCO-DMO Data Processing Notes:

- reformatted column names to comply with BCO-DMO standards.
- converted lat/lons from degree minute format to decimal degrees.
- converted date format from YYMMDD to YYYY/MM/DD

1b:T732,This project will survey the taxonomic, genetic, and functional diversity of the organisms found in marine lakes, and investigate the processes that cause gains and losses in this biodiversity. Marine lakes formed as melting ice sheets raised sea level after the last glacial maximum and flooded hundreds of inland valleys around the world. Inoculated with marine life from the surrounding sea and then isolated to varying degrees for the next 6,000 to 15,000 years, these marine lakes provide multiple, independent examples of how environments and interactions between species can drive extinction and speciation. Researchers will survey the microbes, algae, invertebrates, and fishes present in 40 marine lakes in Palau and Papua, and study how diversity has changed over time by retrieving the remains of organisms preserved in sediments on the lake bottoms. The project will test whether the number of species, the diversity of functional roles played by organisms, and the genetic diversity within species increase and decrease in parallel; whether certain species can greatly curtail diversity by changing the environment; whether the size of a lake determines its biodiversity; and whether the processes that control diversity in marine organisms are similar to those that operate on land. Because biodiversity underlies the ecosystem services on which society depends, society has a great interest in understanding the processes that generate and retain biodiversity in nature. This project will also help conserve areas of economic importance. Marine lakes in the study region are important for tourism, and researchers will work closely with governmental and non-governmental conservation and education groups and with diving and tourism businesses to raise awareness of the value and threats to marine lakes in Indonesia and Palau.6:["$","$L19",null,{"dataset":{"_id":"709224","description":"

Lipid and water δ²H and δ¹⁸O from B. gymnorhiza mangroves in Palau during 2013.

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All methodology was described in Ladd & Sachs, GCA, 2017, doi: 10.1016/j.gca.2017.01.046

Leaf and stem samples were collected from three replicate trees on the north shore of each lake and stored frozen prior to analysis. Water samples were collected from 1cm below the lake surface, and salinity was measured with a refractometer.

Leaf and stem water were cryogenically extracted on a vacuum line at ETH Zurich. Leaf lipids were extracted using a Dionex Accelerated Solvent Extractor (ASE 200). Total lipid extracts were saponified with KOH in MeOH (12 hours at 60 deg C). Following saponification, hexane soluble lipids were then separated into hydrocarbon, wax ester, alcohol and polar fractions via a silica gel column chromatography. Alcohol fractions were acetylated with acetic anhydride of known H isotopic composition prior to analysis by GC.

\n","processing":"$1a","bcodmoProcessing":"","title":"Isotopes from B. gymnorhiza mangroves in Palau during 2013","nickname":"B. gymnorhiza isotopes","dataUrl":"","currentState":"Final no updates expected","currentStateId":"7","validated":true,"restricted":false,"version":"1","version_date":"2017-07-19T04:00:00.000Z","abstract":"Isotopes from B. gymnorhiza mangroves in Palau during 2013. Leaf and stem samples were collected from three replicate trees on the north shore of each lake and stored frozen prior to analysis. Water samples were collected from 1cm below the lake surface, and salinity was measured with a refractometer.","citation":"Sachs, J. P., Ladd, N. (2021) Isotopes from B. gymnorhiza mangroves in Palau during 2013. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2017-07-19 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.709224.1 [access date]","citationParts":{"identifier":"doi:10.26008/1912/bco-dmo.709224.1","versionDate":"2017-07-19","versionId":"1","year":"2021","title":"Isotopes from B. gymnorhiza mangroves in Palau during 2013","authors":"Sachs, J. 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Sample number

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unique sample identification or number; any combination of alpha numeric characters; precise definition is file dependent

"}},{"_id":"712470","name":"lat","format":"","frictionlessType":"","description":"

Latitude; N is positive

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

"}},{"_id":"712471","name":"lon","format":"","frictionlessType":"","description":"

Longitude; E is positive

","units":{"_id":"","name":"decimal degrees"},"type":{"_id":"731","name":"longitude","description":"

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

"}},{"_id":"712472","name":"date","format":"","frictionlessType":"","description":"

Date that sampling occurred; YYYY/MM/DD

","units":{"_id":"","name":"unitless"},"type":{"_id":"1070","name":"date","description":"

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)

"}},{"_id":"712473","name":"time","format":"","frictionlessType":"","description":"

Time that sampling occurred; HH:MM

","units":{"_id":"","name":"unitless"},"type":{"_id":"1075","name":"time","description":"

Time GMT defined as HHMM; time of day; generally reported in GMT as HHMM (hours and minutes) but may also be HH.H (decimal hours) or HHMMSS (hours; minutes and seconds); in EqPac time is reported as Hawaii local time

"}},{"_id":"712474","name":"salinity","format":"","frictionlessType":"","description":"

Salinity of sample

","units":{"_id":"","name":"ppt"},"type":{"_id":"955","name":"sal","description":"

Salinity: The amount (mass or quantity of matter) of salt per amount (volume or mass) of a body of water.

"}},{"_id":"712475","name":"dD_surface_water","format":"","frictionlessType":"","description":"

H isotopes of surface water

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"671779","name":"d2H","description":"

Isotopic ratio of deuterium (\"2H\" or \"D\") to a single hydrogen (2H:1H). Also called dD.

"}},{"_id":"712476","name":"s1_dD_surface_water","format":"","frictionlessType":"","description":"

1 standard deviation (analytical) of surface water H isotopes

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1974","name":"standard deviation","description":"

Generic standard deviation value, taking on the units of the parameter that it is tied to.

"}},{"_id":"712477","name":"d18O_surface_water","format":"","frictionlessType":"","description":"

O isotopes of surface water

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1632","name":"d18O","description":"

d18O is the isotope ratio of 18O to 16O. delta180.

"}},{"_id":"712478","name":"s1_d18O_surface_water","format":"","frictionlessType":"","description":"

1 standard deviation (analytical) of surface water O isotopes

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1974","name":"standard deviation","description":"

Generic standard deviation value, taking on the units of the parameter that it is tied to.

"}},{"_id":"712479","name":"lupeol_dD","format":"","frictionlessType":"","description":"

H isotopes of Lupeol

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"671779","name":"d2H","description":"

Isotopic ratio of deuterium (\"2H\" or \"D\") to a single hydrogen (2H:1H). Also called dD.

"}},{"_id":"712480","name":"lupeol_St_dev","format":"","frictionlessType":"","description":"

1 standard deviation (analytical) of lupeol H isotopes

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1974","name":"standard deviation","description":"

Generic standard deviation value, taking on the units of the parameter that it is tied to.

"}},{"_id":"712481","name":"lupeol_n","format":"","frictionlessType":"","description":"

Number of replicate measurements of Lupeol H isotopes

","units":{"_id":"","name":"number"},"type":{"_id":"903","name":"number","description":"

number of organisms counted/observed, a generic term, specific to the data set in which it appears

"}},{"_id":"712482","name":"nC31_dD","format":"","frictionlessType":"","description":"

H isotopes of nC31-alkane

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"671779","name":"d2H","description":"

Isotopic ratio of deuterium (\"2H\" or \"D\") to a single hydrogen (2H:1H). Also called dD.

"}},{"_id":"712483","name":"nC31_st_dev","format":"","frictionlessType":"","description":"

1 standard deviation (analytical) of nC31 H isotopes

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1974","name":"standard deviation","description":"

Generic standard deviation value, taking on the units of the parameter that it is tied to.

"}},{"_id":"712484","name":"nC31_n","format":"","frictionlessType":"","description":"

Number of replicate measurements of nC31 H isotopes

","units":{"_id":"","name":"number"},"type":{"_id":"903","name":"number","description":"

number of organisms counted/observed, a generic term, specific to the data set in which it appears

"}},{"_id":"712485","name":"historic_sal","format":"","frictionlessType":"","description":"

Average salinity measured by Coral Reef Research Foundation from 2007-2013

","units":{"_id":"","name":"ppt"},"type":{"_id":"955","name":"sal","description":"

Salinity: The amount (mass or quantity of matter) of salt per amount (volume or mass) of a body of water.

"}},{"_id":"712486","name":"hist_sal_stdev","format":"","frictionlessType":"","description":"

Standard deviation of historical salinity measurements

","units":{"_id":"","name":"ppt"},"type":{"_id":"1974","name":"standard deviation","description":"

Generic standard deviation value, taking on the units of the parameter that it is tied to.

"}},{"_id":"712487","name":"hist_sal_n","format":"","frictionlessType":"","description":"

Number of measurements of salinity

","units":{"_id":"","name":"number"},"type":{"_id":"903","name":"number","description":"

number of organisms counted/observed, a generic term, specific to the data set in which it appears

"}},{"_id":"712488","name":"xylem_water_dD","format":"","frictionlessType":"","description":"

H isotopes of xylem water

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"671779","name":"d2H","description":"

Isotopic ratio of deuterium (\"2H\" or \"D\") to a single hydrogen (2H:1H). Also called dD.

"}},{"_id":"712489","name":"s1_XW_dD","format":"","frictionlessType":"","description":"

1 standard deviation (analytical) of xylem water H isotopes

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1974","name":"standard deviation","description":"

Generic standard deviation value, taking on the units of the parameter that it is tied to.

"}},{"_id":"712490","name":"leaf_water_dD","format":"","frictionlessType":"","description":"

H isotopes of leaf water

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"671779","name":"d2H","description":"

Isotopic ratio of deuterium (\"2H\" or \"D\") to a single hydrogen (2H:1H). Also called dD.

"}},{"_id":"712491","name":"s1_LW_dD","format":"","frictionlessType":"","description":"

1 standard deviation (analytical) of leaf water H isotopes

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1974","name":"standard deviation","description":"

Generic standard deviation value, taking on the units of the parameter that it is tied to.

"}},{"_id":"712492","name":"d18O_xw","format":"","frictionlessType":"","description":"

O isotopes of xylem water

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1632","name":"d18O","description":"

d18O is the isotope ratio of 18O to 16O. delta180.

"}},{"_id":"712493","name":"s1_d18O_xw","format":"","frictionlessType":"","description":"

1 standard deviation (analytical) of xylem water O isotopes

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1974","name":"standard deviation","description":"

Generic standard deviation value, taking on the units of the parameter that it is tied to.

"}},{"_id":"712494","name":"d18O_lw","format":"","frictionlessType":"","description":"

O isotopes of leaf water

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1632","name":"d18O","description":"

d18O is the isotope ratio of 18O to 16O. delta180.

"}},{"_id":"712495","name":"s1_d18O_lw","format":"","frictionlessType":"","description":"

1 standard deviation (analytical) of leaf water O isotopes

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1974","name":"standard deviation","description":"

Generic standard deviation value, taking on the units of the parameter that it is tied to.

"}},{"_id":"712496","name":"avg_rain_d2H_leaf_water_model","format":"","frictionlessType":"","description":"

H rain water in Koror for closest three rain events

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"671779","name":"d2H","description":"

Isotopic ratio of deuterium (\"2H\" or \"D\") to a single hydrogen (2H:1H). Also called dD.

"}},{"_id":"712497","name":"s1_rain_d2H","format":"","frictionlessType":"","description":"

1 standard deviation of rain water H isotopes

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1974","name":"standard deviation","description":"

Generic standard deviation value, taking on the units of the parameter that it is tied to.

"}},{"_id":"712498","name":"avg_rain_d18O","format":"","frictionlessType":"","description":"

O rain water in Koror for closest three rain events

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1632","name":"d18O","description":"

d18O is the isotope ratio of 18O to 16O. delta180.

"}},{"_id":"712499","name":"s1_rain_d18O","format":"","frictionlessType":"","description":"

1 standard deviation of rain water O isotopes

","units":{"_id":"","name":"per mil (0/00)"},"type":{"_id":"1974","name":"standard deviation","description":"

Generic standard deviation value, taking on the units of the parameter that it is tied to.

"}},{"_id":"712500","name":"ISO_DateTime_UTC","format":"","frictionlessType":"","description":"

DateTime ISO_UTC formatted

","units":{"_id":"","name":"unitless"},"type":{"_id":"1908","name":"ISO_DateTime_UTC","description":"

Date/Time (UTC) ISO formatted
\nThis standard is based on ISO 8601:2004(E) and takes on any of the following forms:
\n2009-08-30T09:05:00[.xx] (local time)
\n2009-08-30T14:05:00[.xx]Z (UTC time)
\n2009-08-30T14:05:00[.xx]-05:00
\nThe dashes and the colons can be dropped.
\nThe T can also be dropped \"by mutual agreement\", but one needs the trailing Z if the time is UTC.

Sample ISO_datetime_utc:
\n2009-08-30T14:05:00[.xx]Z (UTC time)

Format: YYYY-mm-ddTHH:MM:SS[.xx]Z (UTC time)

"}}],"related_publications":[],"related_datasets":[],"services":[{"grouping":"","items":[{"name":"View Data","description":"An in-browser view of the primary tabular data file","url":"https://www.bco-dmo.org/dataset/709224/data/view","contentType":"text/html","actionType":"view"}]},{"grouping":"Metadata","items":[{"name":"HTML","description":"A simple HTML page of the dataset metadata","url":"https://www.bco-dmo.org/dataset/709224/description","contentType":"text/html","actionType":"view"},{"name":"PDF","description":"A PDF of the HTML dataset metadata","url":"https://www.bco-dmo.org/dataset/709224/Dataset_description.pdf","contentType":"application/pdf","actionType":"download"},{"name":"ISO 19115-2 (NOAA Profile)","description":"","url":"https://www.bco-dmo.org/dataset/709224/iso","contentType":"application/xml","actionType":"download"}]}],"programs":[{"_id":"2031","name":"Dimensions of Biodiversity","acronym":"Dimensions of Biodiversity"}],"projects":[{"_id":"2238","name":"Do Parallel Patterns Arise from Parallel Processes?","acronym":"PaPaPro","description":"$1b"}],"archives":[{"id_value":"10.26008/1912/bco-dmo.709224.1","url":"https://doi.org/10.26008/1912/bco-dmo.709224.1","date_assigned":"2021-05-26","version_date":"2017-07-19","archiver":"Marine Biological Laboratory/Woods Hole Oceanographic Institution Library (MBLWHOI DLA)","archiver_id":"272"}],"license":{"name":"Creative Commons Attribution 4.0","id":"CC-BY-4.0","uri":"https://creativecommons.org/licenses/by/4.0/","spdxUri":"https://spdx.org/licenses/CC-BY-4.0"},"metrics":{"views":{"count":113},"downloads":{"count":300}}}}]