Echinophyllia
Echinophyllia is a genus of large polyp stony corals. Members of this genus are colonial corals and are generally foliaceous, usually with very thin leaves. They are native to the Indo-Pacific and are sometimes found in reef aquariums.

Francesca Benzoni · CC BY 3.0 · via Wikipedia/Commons. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.
On record
Recorded, not inferred- Sits inside
- LobophylliidaePBDB
- Diet
- microcarnivore, photosymbioticPBDB, for Scleractinia
- Life habit
- intermediate-level epifaunal, colonial, clonalPBDB, for Scleractinia
- Motility
- stationary, attachedPBDB, for Scleractinia
- Vision
- blindPBDB, for Anthozoa
- Environment
- marinePBDB, for Scleractinia
Time the record covers
At least 72 million years on record.
The record covers at least 72.2 Mya to 11.7 ka. No occurrence read is dated outside 83.6 Mya to 0 Mya.
40 occurrences of Echinophyllia on record, most of them in the Pleistocene. The Paleobiology Database records this as a living group. Bar height is expected occurrences, not a count: each fossil is spread across the span it is dated to, so a tall narrow bar means tight dating and a low wide one means loose.
When
40 occurrences- Late Cretaceous3%
- Oligocene3%
- Miocene20%
- Pliocene9%
- Pleistocene46%
- Holocene20%
These are dates about fossils, not the animal: the record can only begin after it arose and end before it died out, so either end may reach further. Shares are expected occurrences: a fossil dated to a span is counted partly in each period it straddles. More on what this infers.
Found in
8 formations
- Ghasr Ghand Formation2
- Numa Formation2
- Salayar Formation2
- Darkhunish Formation1
- Era Beds Formation1
- Nabire Formation1
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The named rock units Echinophyllia has been recovered from, largest first. Drawn where the rock is now, not where it formed. 29 occurrences have no formation on record, which is common for older literature.
Echinophyllia and its relatives
PleistoceneWhere Echinophyllia and its relatives were recorded in the Pleistocene.
Found in the same rock
319 taxa- Porites9 sites
- Stylophora pistillata7 sites
- Cyphastrea6 sites
- Favia6 sites
- Leptastrea purpurea6 sites
- Montipora6 sites
- Acropora5 sites
- Alveopora5 sites
- Cyphastrea chalcidicum5 sites
- Cyphastrea serailia5 sites
- Dipsastraea pallida5 sites
- Favites abdita5 sites
- Galaxea fascicularis5 sites
- Goniastrea retiformis5 sites
- Hydnophora exesa5 sites
- Platygyra daedalea5 sites
- Plesiastrea versipora5 sites
- Pocillopora damicornis5 sites
- Acanthastrea echinata4 sites
- Dipsastraea favus4 sites
- Dipsastraea speciosa4 sites
- Duncanopsammia peltata4 sites
- Echinopora gemmacea4 sites
- Favites4 sites
The Paleobiology Database records 17 sites for Echinophyllia, and this reads all of them. The number is how many of those sites it was catalogued from too. The 24 sharing the most are listed.
This is not a list of everything alive at the time. It is only what has come out of the same ground as this animal and been written down.
Entered from
27 references- Variations in Pleistocene coral assemblages in space and time in southern and northern central Ryukyu Islands, Japan4
- Coral reefs at 34°N, Japan: Exploring the end of environmental gradients3
- Carbonate deposition in accretionary prism settings: Early Miocene coral limestones and corals of the Makran Mountain Range in southern Iran3
- Facies, Fossil Record, and Age of Pleistocene Reefs from the Red Sea (Saudi Arabia)3
- Evolutionary dynamics of Indo-Pacific reef corals throughout the Neogene2
- Interstadial coral reef terraces and relative sea-level changes during marine oxygen isotope stages 3-4, Kikai Island, central Ryukyus, Japan2
- Environmental control of Holocene changes to the world's most northern hermatypic coral outcrop2
- Geological and geographical distribution of reef-corals in Japan2
- Tiarei outer ridge: Sites M0009, M0021, and M0024-M00261
- Faaa: Sites M0019 and M00201
- Pleistocene reef development in the southwest Ryukyu Islands, Japan1
- Model of fringing reef development in response to progressive sea level fall over the last 7000 years (Kikai-jima, Ryukyu Islands, Japan)1
Each of the 40 occurrences read was entered from one of these publications, ordered by how many each accounts for. This is not a search for papers mentioning the name. 15 further references are not listed. Entries link to doi.org where the Paleobiology Database holds an identifier, and to its own record where it does not. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.
Media and terms
Media content2
Picture of Echinophyllia
- Source
- Wikipedia/Commons
- Credit
- Francesca Benzoni
- Licence
- CC BY 3.0
- Commercial use
- the licence allows it
3D model
- Source
- Sketchfab
- Licence
- CC Attribution-NonCommercial-NoDerivs
- Commercial use
- the licence does not allow it
Smithsonian Open Access was not reached for this taxon, so this list is what the others held rather than everything there is.
The description on this site
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itLobophylliidae through timeFormations of the PleistoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Klunzinger 1879