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Pheidole microps

Body symmetry

Namigai et al 2014
bilaterally symmetric
URI: http://purl.obolibrary.org/obo/PATO_0001324

Definission: being symmetric about a plane running from frontal end to caudal end (head to tail), and having nearly identical right and left halves

smon-e tute j'argistrassion

behavioral circadian rhythm

Lewis and Taylor 1965
diurnal
URI: http://www.wikidata.org/entity/Q906470

Definission: animal behavior characterized by activity during the day, with a period of inactivity at night.

smon-e tute j'argistrassion
(adult)

developmental mode

Insect Development
holometabolous
URI: http://eol.org/schema/terms/holometabolous

Definission: Development of insects with complete metamorphosis which involves a pupal stage.

smon-e tute j'argistrassion

geographic distribution

1 argistrassion ëstërmà — smon-e tut

Antweb
Ecuador
URI: http://www.geonames.org/3658394

smon-e tute j'argistrassion
Antweb
Guyana
URI: http://www.geonames.org/3378535

smon-e tute j'argistrassion
Antweb
French Guiana
URI: http://www.geonames.org/3381670

smon-e tute j'argistrassion
Antweb
Peru
URI: http://www.geonames.org/3932488

smon-e tute j'argistrassion
Guyana Species List
Guyana
URI: http://www.geonames.org/3378535

smon-e tute j'argistrassion

habitat

TreatmentBank
plant litter
URI: http://purl.obolibrary.org/obo/ENVO_01000628

Definission: dead plant material, such as leaves, bark, needles, and twigs, that has fallen to the ground

smon-e tute j'argistrassion
TreatmentBank
lagh
URI: http://purl.obolibrary.org/obo/ENVO_01000252

smon-e tute j'argistrassion
Antweb
wet forest
URI: http://eol.org/schema/terms/wet_forest

smon-e tute j'argistrassion
Antweb
wet forest
URI: http://eol.org/schema/terms/wet_forest

smon-e tute j'argistrassion
Antweb
wet forest
URI: http://eol.org/schema/terms/wet_forest

smon-e tute j'argistrassion

number of records in gbif

GBIF data coverage

17

soil composition

TreatmentBank
seul sabios
URI: http://purl.obolibrary.org/obo/ENVO_00002229

Definission: Arenosols are sandy soils, including both soils developed in residual sands after in situ weathering of usually quartz-rich sediments or rock, and soils developed in recently deposited sands such as dunes in deserts and beach lands.

smon-e tute j'argistrassion