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PrefixNamespace IRI
n2http://purl.obolibrary.org/obo/
rdfshttp://www.w3.org/2000/01/rdf-schema#
obohttp://www.geneontology.org/formats/oboInOwl#
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
owlhttp://www.w3.org/2002/07/owl#
xsdhhttp://www.w3.org/2001/XMLSchema#
Subject Item
n2:ENVO_01000261
rdf:type
owl:Class
rdfs:label
lysocline
rdfs:subClassOf
n2:ENVO_01000295 n2:ENVO_01000258 _:vb1218395
obo:created_by
pbuttigieg
obo:creation_date
2013-10-06T20:16:10Z
n2:IAO_0000115
A layer within a marine water body where the rate of calcite dissolution changes rapidly with depth. The increase in the rate of calcite dissolution with depth is largely due to the concomitant fall in calcite saturation.
obo:hasOBONamespace
ENVO
obo:id
ENVO:01000261
Subject Item
_:vb1218395
rdf:type
owl:Restriction
owl:onProperty
n2:BFO_0000050
owl:someValuesFrom
n2:ENVO_00001999