Carbon sequestration during core formation implied by complex carbon polymerization View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2019-12

AUTHORS

Natalia V. Solomatova, Razvan Caracas, Craig E. Manning

ABSTRACT

Current estimates of the carbon flux between the surface and mantle are highly variable, and the total amount of carbon stored in closed hidden reservoirs is unknown. Understanding the forms in which carbon existed in the molten early Earth is a critical step towards quantifying the carbon budget of Earth's deep interior. Here we employ first-principles molecular dynamics to study the evolution of carbon species as a function of pressure in a pyrolite melt. We find that with increasing pressure, the abundance of CO2 and CO3 species decreases at the expense of CO4 and complex oxo-carbon polymers (CxOy) displaying multiple C-C bonds. We anticipate that polymerized oxo-carbon species were a significant reservoir for carbon in the terrestrial magma ocean. The presence of Fe-C clusters suggests that upon segregation, Fe-rich metal may partition a significant fraction of carbon from the silicate liquid, leading to carbon transport into the Earth's core. More... »

PAGES

789

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/s41467-019-08742-9

DOI

http://dx.doi.org/10.1038/s41467-019-08742-9

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1112165496

PUBMED

https://www.ncbi.nlm.nih.gov/pubmed/30770828


Indexing Status Check whether this publication has been indexed by Scopus and Web Of Science using the SN Indexing Status Tool
Incoming Citations Browse incoming citations for this publication using opencitations.net

JSON-LD is the canonical representation for SciGraph data.

TIP: You can open this SciGraph record using an external JSON-LD service: JSON-LD Playground Google SDTT

[
  {
    "@context": "https://springernature.github.io/scigraph/jsonld/sgcontext.json", 
    "about": [
      {
        "id": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/0402", 
        "inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/", 
        "name": "Geochemistry", 
        "type": "DefinedTerm"
      }, 
      {
        "id": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/04", 
        "inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/", 
        "name": "Earth Sciences", 
        "type": "DefinedTerm"
      }
    ], 
    "author": [
      {
        "affiliation": {
          "alternateName": "\u00c9cole Normale Sup\u00e9rieure de Lyon", 
          "id": "https://www.grid.ac/institutes/grid.15140.31", 
          "name": [
            "Laboratoire de G\u00e9ologie de Lyon, CNRS UMR 5276, Universit\u00e9 Claude Bernard Lyon 1, \u00c9cole Normale Sup\u00e9rieure de Lyon, 69007, Lyon, France"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Solomatova", 
        "givenName": "Natalia V.", 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "alternateName": "\u00c9cole Normale Sup\u00e9rieure de Lyon", 
          "id": "https://www.grid.ac/institutes/grid.15140.31", 
          "name": [
            "Laboratoire de G\u00e9ologie de Lyon, CNRS UMR 5276, Universit\u00e9 Claude Bernard Lyon 1, \u00c9cole Normale Sup\u00e9rieure de Lyon, 69007, Lyon, France"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Caracas", 
        "givenName": "Razvan", 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "alternateName": "University of California Los Angeles", 
          "id": "https://www.grid.ac/institutes/grid.19006.3e", 
          "name": [
            "Department of Earth, Planetary and Space Sciences, University of California, 90095, Los Angeles, CA, USA"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Manning", 
        "givenName": "Craig E.", 
        "type": "Person"
      }
    ], 
    "citation": [
      {
        "id": "https://doi.org/10.1016/j.epsl.2007.07.055", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1005110734"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.2138/rmg.2013.75.7", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1007874716"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.2138/am.2011.3577", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1011228324"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(93)90105-i", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1013363370"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0012-821x(93)90105-i", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1013363370"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1103/physrevb.91.104101", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1014320040"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1103/physrevb.91.104101", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1014320040"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1038/ncomms9702", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1017925119", 
          "https://doi.org/10.1038/ncomms9702"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/j.epsl.2008.06.005", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1019850112"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1038/nature04763", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1021302942", 
          "https://doi.org/10.1038/nature04763"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1038/nature04763", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1021302942", 
          "https://doi.org/10.1038/nature04763"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1038/nature04763", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1021302942", 
          "https://doi.org/10.1038/nature04763"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/s0012-821x(02)01145-7", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1025315393"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/s0012-821x(02)01145-7", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1025315393"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/j.gca.2011.01.004", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1028784457"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1007/bf00377759", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1029744499", 
          "https://doi.org/10.1007/bf00377759"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/j.epsl.2005.05.017", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1035094423"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/j.epsl.2005.05.017", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1035094423"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/j.chemgeo.2015.07.030", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1035679959"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1029/2007gl031349", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1035757776"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1073/pnas.1507889112", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1037366217"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1029/2010jb007819", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1041589426"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/0009-2541(94)00140-4", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1041984210"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1073/pnas.1312771110", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1043858631"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/b0-08-043751-6/02015-6", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1045427062"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1111/j.1945-5100.2006.tb00459.x", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1046032280"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1111/j.1945-5100.2006.tb00459.x", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1046032280"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1007/bf00405226", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1047062674", 
          "https://doi.org/10.1007/bf00405226"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1007/bf00405226", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1047062674", 
          "https://doi.org/10.1007/bf00405226"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.2138/rmg.2013.75.8", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1049456991"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/j.epsl.2010.06.039", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1050562782"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/s0016-7037(99)00196-9", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1052556047"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1063/1.447334", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1058025354"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1103/physreva.31.1695", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1060473124"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1103/physreva.31.1695", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1060473124"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1103/physrevb.50.17953", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1060573414"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1103/physrevb.50.17953", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1060573414"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1103/physrevb.54.11169", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1060581262"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1103/physrevb.54.11169", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1060581262"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1103/physrevlett.77.3865", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1060814179"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1103/physrevlett.77.3865", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1060814179"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.2475/ajs.276.4.455", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1070841297"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1038/s41598-017-00918-x", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1084537948", 
          "https://doi.org/10.1038/s41598-017-00918-x"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1093/acprof:oso/9780198742951.001.0001", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1098731507"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1103/physrevb.98.014108", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1105672526"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1103/physrevb.98.014108", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1105672526"
        ], 
        "type": "CreativeWork"
      }
    ], 
    "datePublished": "2019-12", 
    "datePublishedReg": "2019-12-01", 
    "description": "Current estimates of the carbon flux between the surface and mantle are highly variable, and the total amount of carbon stored in closed hidden reservoirs is unknown. Understanding the forms in which carbon existed in the molten early Earth is a critical step towards quantifying the carbon budget of Earth's deep interior. Here we employ first-principles molecular dynamics to study the evolution of carbon species as a function of pressure in a pyrolite melt. We find that with increasing pressure, the abundance of CO2 and CO3 species decreases at the expense of CO4 and complex oxo-carbon polymers (CxOy) displaying multiple C-C bonds. We anticipate that polymerized oxo-carbon species were a significant reservoir for carbon in the terrestrial magma ocean. The presence of Fe-C clusters suggests that upon segregation, Fe-rich metal may partition a significant fraction of carbon from the silicate liquid, leading to carbon transport into the Earth's core.", 
    "genre": "research_article", 
    "id": "sg:pub.10.1038/s41467-019-08742-9", 
    "inLanguage": [
      "en"
    ], 
    "isAccessibleForFree": true, 
    "isFundedItemOf": [
      {
        "id": "sg:grant.6384259", 
        "type": "MonetaryGrant"
      }
    ], 
    "isPartOf": [
      {
        "id": "sg:journal.1043282", 
        "issn": [
          "2041-1723"
        ], 
        "name": "Nature Communications", 
        "type": "Periodical"
      }, 
      {
        "issueNumber": "1", 
        "type": "PublicationIssue"
      }, 
      {
        "type": "PublicationVolume", 
        "volumeNumber": "10"
      }
    ], 
    "name": "Carbon sequestration during core formation implied by complex carbon polymerization", 
    "pagination": "789", 
    "productId": [
      {
        "name": "readcube_id", 
        "type": "PropertyValue", 
        "value": [
          "91ae96871628b50ee0f88541e2ae00fb919361e1504e45768c0f2be36f65e038"
        ]
      }, 
      {
        "name": "pubmed_id", 
        "type": "PropertyValue", 
        "value": [
          "30770828"
        ]
      }, 
      {
        "name": "nlm_unique_id", 
        "type": "PropertyValue", 
        "value": [
          "101528555"
        ]
      }, 
      {
        "name": "doi", 
        "type": "PropertyValue", 
        "value": [
          "10.1038/s41467-019-08742-9"
        ]
      }, 
      {
        "name": "dimensions_id", 
        "type": "PropertyValue", 
        "value": [
          "pub.1112165496"
        ]
      }
    ], 
    "sameAs": [
      "https://doi.org/10.1038/s41467-019-08742-9", 
      "https://app.dimensions.ai/details/publication/pub.1112165496"
    ], 
    "sdDataset": "articles", 
    "sdDatePublished": "2019-04-11T12:52", 
    "sdLicense": "https://scigraph.springernature.com/explorer/license/", 
    "sdPublisher": {
      "name": "Springer Nature - SN SciGraph project", 
      "type": "Organization"
    }, 
    "sdSource": "s3://com-uberresearch-data-dimensions-target-20181106-alternative/cleanup/v134/2549eaecd7973599484d7c17b260dba0a4ecb94b/merge/v9/a6c9fde33151104705d4d7ff012ea9563521a3ce/jats-lookup/v90/0000000364_0000000364/records_72834_00000001.jsonl", 
    "type": "ScholarlyArticle", 
    "url": "https://www.nature.com/articles/s41467-019-08742-9"
  }
]
 

Download the RDF metadata as:  json-ld nt turtle xml License info

HOW TO GET THIS DATA PROGRAMMATICALLY:

JSON-LD is a popular format for linked data which is fully compatible with JSON.

curl -H 'Accept: application/ld+json' 'https://scigraph.springernature.com/pub.10.1038/s41467-019-08742-9'

N-Triples is a line-based linked data format ideal for batch operations.

curl -H 'Accept: application/n-triples' 'https://scigraph.springernature.com/pub.10.1038/s41467-019-08742-9'

Turtle is a human-readable linked data format.

curl -H 'Accept: text/turtle' 'https://scigraph.springernature.com/pub.10.1038/s41467-019-08742-9'

RDF/XML is a standard XML format for linked data.

curl -H 'Accept: application/rdf+xml' 'https://scigraph.springernature.com/pub.10.1038/s41467-019-08742-9'


 

This table displays all metadata directly associated to this object as RDF triples.

188 TRIPLES      21 PREDICATES      62 URIs      21 LITERALS      9 BLANK NODES

Subject Predicate Object
1 sg:pub.10.1038/s41467-019-08742-9 schema:about anzsrc-for:04
2 anzsrc-for:0402
3 schema:author Nf79d6dd7dffa4028a2683c6eb6c2cb44
4 schema:citation sg:pub.10.1007/bf00377759
5 sg:pub.10.1007/bf00405226
6 sg:pub.10.1038/nature04763
7 sg:pub.10.1038/ncomms9702
8 sg:pub.10.1038/s41598-017-00918-x
9 https://doi.org/10.1016/0009-2541(94)00140-4
10 https://doi.org/10.1016/0012-821x(93)90105-i
11 https://doi.org/10.1016/b0-08-043751-6/02015-6
12 https://doi.org/10.1016/j.chemgeo.2015.07.030
13 https://doi.org/10.1016/j.epsl.2005.05.017
14 https://doi.org/10.1016/j.epsl.2007.07.055
15 https://doi.org/10.1016/j.epsl.2008.06.005
16 https://doi.org/10.1016/j.epsl.2010.06.039
17 https://doi.org/10.1016/j.gca.2011.01.004
18 https://doi.org/10.1016/s0012-821x(02)01145-7
19 https://doi.org/10.1016/s0016-7037(99)00196-9
20 https://doi.org/10.1029/2007gl031349
21 https://doi.org/10.1029/2010jb007819
22 https://doi.org/10.1063/1.447334
23 https://doi.org/10.1073/pnas.1312771110
24 https://doi.org/10.1073/pnas.1507889112
25 https://doi.org/10.1093/acprof:oso/9780198742951.001.0001
26 https://doi.org/10.1103/physreva.31.1695
27 https://doi.org/10.1103/physrevb.50.17953
28 https://doi.org/10.1103/physrevb.54.11169
29 https://doi.org/10.1103/physrevb.91.104101
30 https://doi.org/10.1103/physrevb.98.014108
31 https://doi.org/10.1103/physrevlett.77.3865
32 https://doi.org/10.1111/j.1945-5100.2006.tb00459.x
33 https://doi.org/10.2138/am.2011.3577
34 https://doi.org/10.2138/rmg.2013.75.7
35 https://doi.org/10.2138/rmg.2013.75.8
36 https://doi.org/10.2475/ajs.276.4.455
37 schema:datePublished 2019-12
38 schema:datePublishedReg 2019-12-01
39 schema:description Current estimates of the carbon flux between the surface and mantle are highly variable, and the total amount of carbon stored in closed hidden reservoirs is unknown. Understanding the forms in which carbon existed in the molten early Earth is a critical step towards quantifying the carbon budget of Earth's deep interior. Here we employ first-principles molecular dynamics to study the evolution of carbon species as a function of pressure in a pyrolite melt. We find that with increasing pressure, the abundance of CO<sub>2</sub> and CO<sub>3</sub> species decreases at the expense of CO<sub>4</sub> and complex oxo-carbon polymers (C<sub>x</sub>O<sub>y</sub>) displaying multiple C-C bonds. We anticipate that polymerized oxo-carbon species were a significant reservoir for carbon in the terrestrial magma ocean. The presence of Fe-C clusters suggests that upon segregation, Fe-rich metal may partition a significant fraction of carbon from the silicate liquid, leading to carbon transport into the Earth's core.
40 schema:genre research_article
41 schema:inLanguage en
42 schema:isAccessibleForFree true
43 schema:isPartOf N5edd7d2d0362464d977f6c8a8d387ee5
44 N8f8e94aab3584b318a2b8de30af1eb11
45 sg:journal.1043282
46 schema:name Carbon sequestration during core formation implied by complex carbon polymerization
47 schema:pagination 789
48 schema:productId N08399932d2c74e23ab419900f54d85e7
49 N13174755c388447198500f990a21711f
50 N441bed8e9cef46ea94175c95fe60d9ff
51 Nc40e999d85e0475ba3dd852d08c61af0
52 Nd4119a443435483d867e9ccbe0f5a86e
53 schema:sameAs https://app.dimensions.ai/details/publication/pub.1112165496
54 https://doi.org/10.1038/s41467-019-08742-9
55 schema:sdDatePublished 2019-04-11T12:52
56 schema:sdLicense https://scigraph.springernature.com/explorer/license/
57 schema:sdPublisher Nb6e05c583e7046739d159ed7ee9717e4
58 schema:url https://www.nature.com/articles/s41467-019-08742-9
59 sgo:license sg:explorer/license/
60 sgo:sdDataset articles
61 rdf:type schema:ScholarlyArticle
62 N08399932d2c74e23ab419900f54d85e7 schema:name pubmed_id
63 schema:value 30770828
64 rdf:type schema:PropertyValue
65 N13174755c388447198500f990a21711f schema:name readcube_id
66 schema:value 91ae96871628b50ee0f88541e2ae00fb919361e1504e45768c0f2be36f65e038
67 rdf:type schema:PropertyValue
68 N2235c2a2812d4a52a1b9d3e917af181b rdf:first N8e091332b90b4c45969fb8ec1914eaa9
69 rdf:rest N579f821737484cb9b887d4afe391262a
70 N441bed8e9cef46ea94175c95fe60d9ff schema:name dimensions_id
71 schema:value pub.1112165496
72 rdf:type schema:PropertyValue
73 N579f821737484cb9b887d4afe391262a rdf:first N8bfbdd807e1241eba43e142737f64f49
74 rdf:rest rdf:nil
75 N599c024d568b46e38e4f19eb71dfeaed schema:affiliation https://www.grid.ac/institutes/grid.15140.31
76 schema:familyName Solomatova
77 schema:givenName Natalia V.
78 rdf:type schema:Person
79 N5edd7d2d0362464d977f6c8a8d387ee5 schema:volumeNumber 10
80 rdf:type schema:PublicationVolume
81 N8bfbdd807e1241eba43e142737f64f49 schema:affiliation https://www.grid.ac/institutes/grid.19006.3e
82 schema:familyName Manning
83 schema:givenName Craig E.
84 rdf:type schema:Person
85 N8e091332b90b4c45969fb8ec1914eaa9 schema:affiliation https://www.grid.ac/institutes/grid.15140.31
86 schema:familyName Caracas
87 schema:givenName Razvan
88 rdf:type schema:Person
89 N8f8e94aab3584b318a2b8de30af1eb11 schema:issueNumber 1
90 rdf:type schema:PublicationIssue
91 Nb6e05c583e7046739d159ed7ee9717e4 schema:name Springer Nature - SN SciGraph project
92 rdf:type schema:Organization
93 Nc40e999d85e0475ba3dd852d08c61af0 schema:name nlm_unique_id
94 schema:value 101528555
95 rdf:type schema:PropertyValue
96 Nd4119a443435483d867e9ccbe0f5a86e schema:name doi
97 schema:value 10.1038/s41467-019-08742-9
98 rdf:type schema:PropertyValue
99 Nf79d6dd7dffa4028a2683c6eb6c2cb44 rdf:first N599c024d568b46e38e4f19eb71dfeaed
100 rdf:rest N2235c2a2812d4a52a1b9d3e917af181b
101 anzsrc-for:04 schema:inDefinedTermSet anzsrc-for:
102 schema:name Earth Sciences
103 rdf:type schema:DefinedTerm
104 anzsrc-for:0402 schema:inDefinedTermSet anzsrc-for:
105 schema:name Geochemistry
106 rdf:type schema:DefinedTerm
107 sg:grant.6384259 http://pending.schema.org/fundedItem sg:pub.10.1038/s41467-019-08742-9
108 rdf:type schema:MonetaryGrant
109 sg:journal.1043282 schema:issn 2041-1723
110 schema:name Nature Communications
111 rdf:type schema:Periodical
112 sg:pub.10.1007/bf00377759 schema:sameAs https://app.dimensions.ai/details/publication/pub.1029744499
113 https://doi.org/10.1007/bf00377759
114 rdf:type schema:CreativeWork
115 sg:pub.10.1007/bf00405226 schema:sameAs https://app.dimensions.ai/details/publication/pub.1047062674
116 https://doi.org/10.1007/bf00405226
117 rdf:type schema:CreativeWork
118 sg:pub.10.1038/nature04763 schema:sameAs https://app.dimensions.ai/details/publication/pub.1021302942
119 https://doi.org/10.1038/nature04763
120 rdf:type schema:CreativeWork
121 sg:pub.10.1038/ncomms9702 schema:sameAs https://app.dimensions.ai/details/publication/pub.1017925119
122 https://doi.org/10.1038/ncomms9702
123 rdf:type schema:CreativeWork
124 sg:pub.10.1038/s41598-017-00918-x schema:sameAs https://app.dimensions.ai/details/publication/pub.1084537948
125 https://doi.org/10.1038/s41598-017-00918-x
126 rdf:type schema:CreativeWork
127 https://doi.org/10.1016/0009-2541(94)00140-4 schema:sameAs https://app.dimensions.ai/details/publication/pub.1041984210
128 rdf:type schema:CreativeWork
129 https://doi.org/10.1016/0012-821x(93)90105-i schema:sameAs https://app.dimensions.ai/details/publication/pub.1013363370
130 rdf:type schema:CreativeWork
131 https://doi.org/10.1016/b0-08-043751-6/02015-6 schema:sameAs https://app.dimensions.ai/details/publication/pub.1045427062
132 rdf:type schema:CreativeWork
133 https://doi.org/10.1016/j.chemgeo.2015.07.030 schema:sameAs https://app.dimensions.ai/details/publication/pub.1035679959
134 rdf:type schema:CreativeWork
135 https://doi.org/10.1016/j.epsl.2005.05.017 schema:sameAs https://app.dimensions.ai/details/publication/pub.1035094423
136 rdf:type schema:CreativeWork
137 https://doi.org/10.1016/j.epsl.2007.07.055 schema:sameAs https://app.dimensions.ai/details/publication/pub.1005110734
138 rdf:type schema:CreativeWork
139 https://doi.org/10.1016/j.epsl.2008.06.005 schema:sameAs https://app.dimensions.ai/details/publication/pub.1019850112
140 rdf:type schema:CreativeWork
141 https://doi.org/10.1016/j.epsl.2010.06.039 schema:sameAs https://app.dimensions.ai/details/publication/pub.1050562782
142 rdf:type schema:CreativeWork
143 https://doi.org/10.1016/j.gca.2011.01.004 schema:sameAs https://app.dimensions.ai/details/publication/pub.1028784457
144 rdf:type schema:CreativeWork
145 https://doi.org/10.1016/s0012-821x(02)01145-7 schema:sameAs https://app.dimensions.ai/details/publication/pub.1025315393
146 rdf:type schema:CreativeWork
147 https://doi.org/10.1016/s0016-7037(99)00196-9 schema:sameAs https://app.dimensions.ai/details/publication/pub.1052556047
148 rdf:type schema:CreativeWork
149 https://doi.org/10.1029/2007gl031349 schema:sameAs https://app.dimensions.ai/details/publication/pub.1035757776
150 rdf:type schema:CreativeWork
151 https://doi.org/10.1029/2010jb007819 schema:sameAs https://app.dimensions.ai/details/publication/pub.1041589426
152 rdf:type schema:CreativeWork
153 https://doi.org/10.1063/1.447334 schema:sameAs https://app.dimensions.ai/details/publication/pub.1058025354
154 rdf:type schema:CreativeWork
155 https://doi.org/10.1073/pnas.1312771110 schema:sameAs https://app.dimensions.ai/details/publication/pub.1043858631
156 rdf:type schema:CreativeWork
157 https://doi.org/10.1073/pnas.1507889112 schema:sameAs https://app.dimensions.ai/details/publication/pub.1037366217
158 rdf:type schema:CreativeWork
159 https://doi.org/10.1093/acprof:oso/9780198742951.001.0001 schema:sameAs https://app.dimensions.ai/details/publication/pub.1098731507
160 rdf:type schema:CreativeWork
161 https://doi.org/10.1103/physreva.31.1695 schema:sameAs https://app.dimensions.ai/details/publication/pub.1060473124
162 rdf:type schema:CreativeWork
163 https://doi.org/10.1103/physrevb.50.17953 schema:sameAs https://app.dimensions.ai/details/publication/pub.1060573414
164 rdf:type schema:CreativeWork
165 https://doi.org/10.1103/physrevb.54.11169 schema:sameAs https://app.dimensions.ai/details/publication/pub.1060581262
166 rdf:type schema:CreativeWork
167 https://doi.org/10.1103/physrevb.91.104101 schema:sameAs https://app.dimensions.ai/details/publication/pub.1014320040
168 rdf:type schema:CreativeWork
169 https://doi.org/10.1103/physrevb.98.014108 schema:sameAs https://app.dimensions.ai/details/publication/pub.1105672526
170 rdf:type schema:CreativeWork
171 https://doi.org/10.1103/physrevlett.77.3865 schema:sameAs https://app.dimensions.ai/details/publication/pub.1060814179
172 rdf:type schema:CreativeWork
173 https://doi.org/10.1111/j.1945-5100.2006.tb00459.x schema:sameAs https://app.dimensions.ai/details/publication/pub.1046032280
174 rdf:type schema:CreativeWork
175 https://doi.org/10.2138/am.2011.3577 schema:sameAs https://app.dimensions.ai/details/publication/pub.1011228324
176 rdf:type schema:CreativeWork
177 https://doi.org/10.2138/rmg.2013.75.7 schema:sameAs https://app.dimensions.ai/details/publication/pub.1007874716
178 rdf:type schema:CreativeWork
179 https://doi.org/10.2138/rmg.2013.75.8 schema:sameAs https://app.dimensions.ai/details/publication/pub.1049456991
180 rdf:type schema:CreativeWork
181 https://doi.org/10.2475/ajs.276.4.455 schema:sameAs https://app.dimensions.ai/details/publication/pub.1070841297
182 rdf:type schema:CreativeWork
183 https://www.grid.ac/institutes/grid.15140.31 schema:alternateName École Normale Supérieure de Lyon
184 schema:name Laboratoire de Géologie de Lyon, CNRS UMR 5276, Université Claude Bernard Lyon 1, École Normale Supérieure de Lyon, 69007, Lyon, France
185 rdf:type schema:Organization
186 https://www.grid.ac/institutes/grid.19006.3e schema:alternateName University of California Los Angeles
187 schema:name Department of Earth, Planetary and Space Sciences, University of California, 90095, Los Angeles, CA, USA
188 rdf:type schema:Organization
 




Preview window. Press ESC to close (or click here)


...