Favites complanata
Favites complanata is a species of stony coral in the family Merulinidae, sometimes known as the larger star coral. It is native to the Indo-Pacific region and its range extends from the Red Sea and Indian Ocean to the western and central Pacific Ocean. This is an uncommon species of coral and seems to be decreasing in abundance, and the International Union for Conservation of Nature has rated its conservation status as being "near threatened".

NPS - Larry Basch · Public Domain · 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
- FavitesPBDB
- 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 2.5 million years on record.
The record covers at least 2.58 Mya to 11.7 ka. No occurrence read is dated outside 5.333 Mya to 0 Mya.
26 occurrences of Favites complanata 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
26 occurrences- Pliocene11%
- Pleistocene78%
- Holocene12%
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
4 formations
- Samadai Formation2
- Chaya Formation2
- Naha Formation · Ryukyu Group1
- Shagra Formation1
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The named rock units Favites complanata has been recovered from, largest first. Drawn where the rock is now, not where it formed. 20 occurrences have no formation on record, which is common for older literature.
Favites complanata and its relatives
PleistoceneWhere Favites complanata and its relatives were recorded in the Pleistocene.
Found in the same rock
60 taxa- Goniastrea retiformis4 sites
- Platygyra daedalea4 sites
- Echinopora gemmacea3 sites
- Porites solida3 sites
- Acanthastrea echinata2 sites
- Cardium2 sites
- Clypeaster2 sites
- Clypeaster reticulatus2 sites
- Cyphastrea serailia2 sites
- Galaxea fascicularis2 sites
- Gloripallium pallium2 sites
- Heterocentrotus2 sites
- Hyotissa virleti2 sites
- Laganum depressum2 sites
- Lithophaga2 sites
- Lucina2 sites
- Pecten vasseli2 sites
- Acervulina1 site
- Acropora1 site
- Acropora humilis1 site
- Acropora pharaonis1 site
- Acroporidae1 site
- Alectryonella plicatula1 site
- Brissus1 site
The Paleobiology Database records 4 sites for Favites complanata, 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
12 references- Facies, Fossil Record, and Age of Pleistocene Reefs from the Red Sea (Saudi Arabia)6
- Quaternary fossil coral communities in uplifted strata along the Balochistan coast of Pakistan: understanding modern coral decline in the Arabian Sea4
- Limited membership in Pleistocene reef coral assemblages from the Huon Peninsula, Papua New Guinea: constancy during global change4
- Taxonomic Study of Faviidae Family- Quaternary Corals of Okha-Mandal Taluka, Saurashtra Coast, Gujarat2
- Recurrent patterns of coral community and sediment facies development through successive phases of Holocene inner-shelf reef growth and decline2
- Pliocene and Plio-Pleistocene macrofauna from the Red Sea coastal plain (Egypt): biostratigraphy and biogeography2
- Quaternary corals (Scleractinia: Merulinidae) from the Egyptian and Saudi Arabian Red Sea Coast1
- Pliocene corals from the Togopi Formation of the Dent Peninsula, Sabah, northeastern Borneo, Malaysia1
- Quaternary corals of Okha- An evidence of Sea level changes and environment of deposition1
- Variations in Pleistocene coral assemblages in space and time in southern and northern central Ryukyu Islands, Japan1
- Raised coral terraces at Malakula, Vanuatu, southwest Pacific, indicate high sea level during marine isotope stage 31
- Les Madreporaires fossiles de Mare [The fossil corals from Mare]1
Each of the 26 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. 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 content1
Picture of Favites complanata
- Source
- Wikipedia/Commons
- Credit
- NPS - Larry Basch
- Licence
- Public Domain
- Commercial use
- the licence allows it
No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.
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 itFavites through timeFormations of the PleistoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Ehrenberg 1834)