Nanopublications

@prefix cito: <http://purl.org/spar/cito/> .
@prefix dcterms: <http://purl.org/dc/terms/> .
@prefix foaf: <http://xmlns.com/foaf/0.1/> .
@prefix hycl: <http://purl.org/petapico/o/hycl#> .
@prefix np: <http://www.nanopub.org/nschema#> .
@prefix npx: <http://purl.org/nanopub/x/> .
@prefix nt: <https://w3id.org/np/o/ntemplate/> .
@prefix prov: <http://www.w3.org/ns/prov#> .
@prefix rdfs: <http://www.w3.org/2000/01/rdf-schema#> .
@prefix sub: <https://w3id.org/sciencelive/np/RA2-UFcnlEqpluz6lIcOUqUBN2gSKi-z_KU4Z84Lk-Hd4/> .
@prefix this: <https://w3id.org/sciencelive/np/RA2-UFcnlEqpluz6lIcOUqUBN2gSKi-z_KU4Z84Lk-Hd4> .
@prefix xsd: <http://www.w3.org/2001/XMLSchema#> .

sub:Head {
  this: np:hasAssertion sub:assertion ;
    np:hasProvenance sub:provenance ;
    np:hasPublicationInfo sub:pubinfo ;
    a np:Nanopublication .
}

sub:assertion {
<http://purl.org/aida/Oxygen%20isotopes%20of%20redeposited%20foraminifera%20in%20the%208.2%20ka%20layer%20in%20core%20MD95-2011%20show%20%CE%B418O%20values%20of%202.95%E2%80%B0%2C%20indicating%20a%20cooling%20interpretation%20derived%20from%20older%20sediments.> cito:obtainsSupportFrom <https://doi.org/10.1038/s41467-024-47347-9> , <https://doi.org/10.18710/6KDQ7I> ;
a hycl:AIDA-Sentence .
}

sub:provenance {
sub:assertion prov:wasAttributedTo <https://w3id.org/np/RALe_3U-0OKr-rc5FzaSc7xw1nPuGq1LkWoncmx6DXAV4/ai-mistral-ji> .
}

sub:pubinfo {
  <https://w3id.org/np/RALe_3U-0OKr-rc5FzaSc7xw1nPuGq1LkWoncmx6DXAV4/ai-mistral-ji> foaf:name "ai-mistral-ji" .
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    dcterms:license <https://creativecommons.org/licenses/by/4.0/> ;
    npx:hasNanopubType hycl:AIDA-Sentence , <http://purl.org/petapico/o/hycl> ;
    npx:introduces <http://purl.org/aida/Oxygen%20isotopes%20of%20redeposited%20foraminifera%20in%20the%208.2%20ka%20layer%20in%20core%20MD95-2011%20show%20%CE%B418O%20values%20of%202.95%E2%80%B0%2C%20indicating%20a%20cooling%20interpretation%20derived%20from%20older%20sediments.> ;
    npx:wasCreatedAt <https://platform.sciencelive4all.org> ;
    rdfs:label "AIDA sentence: Oxygen isotopes of redeposited foraminifera in the 8.2 ka layer in core MD95-2011 show δ18O values of 2.95‰, indicating a cooling interpretation derived from older sediments." ;
    nt:wasCreatedFromTemplate <https://w3id.org/np/RALmXhDw3rHcMveTgbv8VtWxijUHwnSqhCmtJFIPKWVaA> .
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    npx:hasSignatureTarget this: ;
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