@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/RAPy2SDLK9PFzDwnH6m85f4UUYCREPEbmSFR3OhoMbqPM/> .
@prefix this: <https://w3id.org/sciencelive/np/RAPy2SDLK9PFzDwnH6m85f4UUYCREPEbmSFR3OhoMbqPM> .
@prefix xsd: <http://www.w3.org/2001/XMLSchema#> .

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

sub:assertion {
  <http://purl.org/aida/Erosion%20of%20the%20Barents%20Shelf%20and%20its%20terrestrial%20hinterland%20equated%20to%201%2C548%2C180%20km%C2%B3%20over%20the%20entire%2047%20glacial-interglacial%20cycles%20spanning%20the%20late%20Plio-Pleistocene.>
    a hycl:AIDA-Sentence;
    cito:obtainsSupportFrom <https://doi.org/10.1016/j.earscirev.2024.104936>, <https://doi.org/10.18710/3DNZCM> .
}

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" .
  
  this: dcterms:created "2026-03-13T14:01:10.000Z"^^xsd:dateTime;
    dcterms:creator <https://w3id.org/np/RALe_3U-0OKr-rc5FzaSc7xw1nPuGq1LkWoncmx6DXAV4/ai-mistral-ji>;
    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/Erosion%20of%20the%20Barents%20Shelf%20and%20its%20terrestrial%20hinterland%20equated%20to%201%2C548%2C180%20km%C2%B3%20over%20the%20entire%2047%20glacial-interglacial%20cycles%20spanning%20the%20late%20Plio-Pleistocene.>;
    npx:wasCreatedAt <https://platform.sciencelive4all.org>;
    rdfs:label "AIDA sentence: Erosion of the Barents Shelf and its terrestrial hinterland equated to 1,548,180 km³ over the entire 47 glacial-interglacial cycles spanning the late Plio-Pleistocene.";
    nt:wasCreatedFromTemplate <https://w3id.org/np/RALmXhDw3rHcMveTgbv8VtWxijUHwnSqhCmtJFIPKWVaA> .
  
  sub:sig npx:hasAlgorithm "RSA";
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    npx:hasSignatureTarget this:;
    npx:signedBy <https://w3id.org/np/RALe_3U-0OKr-rc5FzaSc7xw1nPuGq1LkWoncmx6DXAV4/ai-mistral-ji> .
}