Acropora cervicornis
The staghorn coral is a branching, stony coral, within the Order Scleractinia. It is characterized by thick, upright branches which can grow in excess of 2 meters (6.5 ft) in height and resemble the antlers of a stag, hence the name, Staghorn. It grows within various areas of a reef but is most commonly found within shallow fore and back reefs, as well as patch reefs, where water depths rarely exceed 20 meters (65 ft). Staghorn corals can exhibit very fast growth, adding up to 5 cm in new skeleton for every 1 cm of existing skeleton each year, making them one of the fastest growing fringe coral species in the Western Atlantic. Due to this fast growth, Acropora cervicornis, serve as one of the most important reef building corals, functioning as marine nurseries for juvenile fish, buffer zones for erosion and storms, and center points of biodiversity in the Western Atlantic.

Albert Kok at Dutch Wikipedia ( Original text: albert kok ) · 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
- AcroporaPBDB
- Diet
- photosymbiotic, suspension feederPBDB, for Acroporidae
- Life habit
- colonial, clonalPBDB, for Acroporidae
- Motility
- stationary, attachedPBDB, for Scleractinia
- Vision
- blindPBDB, for Anthozoa
- Environment
- marinePBDB, for Scleractinia
Time the record covers
At least 5.3 million years on record.
The record covers at least 5.333 Mya to 11.7 ka. No occurrence read is dated outside 7.246 Mya to 0 Mya.
277 occurrences of Acropora cervicornis 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
277 occurrences- Miocene2%
- Pliocene15%
- Pleistocene76%
- Holocene6%
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
23 formations
- Seroe Domi Formation23
- Hato Formation23
- San Luis Formation22
- Ironshore Formation14
- Quebrada Chocolate Formation · Limon Group13
- Isla Colon Formation · Bocas del Toro Group13
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The named rock units Acropora cervicornis has been recovered from, largest first. Drawn where the rock is now, not where it formed. 128 occurrences have no formation on record, which is common for older literature.
Acropora cervicornis and its relatives
PleistoceneWhere Acropora cervicornis and its relatives were recorded in the Pleistocene.
Found in the same rock
272 taxa- Agaricia agaricites44 sites
- Acropora palmata43 sites
- Porites astreoides40 sites
- Pseudodiploria strigosa40 sites
- Siderastrea siderea35 sites
- Colpophyllia natans29 sites
- Porites furcata29 sites
- Orbicella annularis26 sites
- Orbicella limbata26 sites
- Stylophora granulata25 sites
- Caulastrea portoricensis24 sites
- Pseudodiploria clivosa23 sites
- Manicina areolata21 sites
- Stylophora affinis21 sites
- Porites baracoaensis20 sites
- Dichocoenia stokesi19 sites
- Madracis decactis19 sites
- Stylophora monticulosa19 sites
- Montastrea cavernosa18 sites
- Solenastrea bournoni18 sites
- Diploria labyrinthiformis16 sites
- Orbicella faveolata16 sites
- Stephanocoenia intersepta16 sites
- Porites porites14 sites
The Paleobiology Database records 89 sites for Acropora cervicornis, 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
47 references- Ecological persistence interrupted in Caribbean coral reefs58
- Broad-scale patterns in Pleistocene coral reef communities from the Caribbean: implications for ecology and management23
- Origination preceding extinction during late Cenozoic turnover of Caribbean reefs23
- Pliocene to Pleistocene reef coral assemblages in the Limon Group of Costa Rica23
- Neogene reef coral assemblages of the Bocas del Toro region, Panama: the rise of Acropora palmata22
- Community structure of Pleistocene coral reefs of Curacao, Netherlands Antilles21
- Coral associations of the Pleistocene Ironshore Formation, Grand Cayman14
- Overlapping species boundaries and hybridization within the Montastrea "annularis" reef coral complex in the Pleistocene of the Bahama Islands11
- Coral assemblages and reef environments in the Bahamas Drilling Project cores9
- Personal data5
- Zooxanthellate scleractinian corals of the Bowden shell bed, Southeast Jamaica5
- Taxonomic vetting of Pleistocene coral occurrence data4
Each of the 277 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. 35 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 Acropora cervicornis
- Source
- Wikipedia/Commons
- Credit
- Albert Kok at Dutch Wikipedia ( Original text: albert kok )
- Licence
- Public Domain
- Commercial use
- the licence allows it
3D model
- Source
- Sketchfab
- Licence
- CC0 Public Domain
- Commercial use
- the licence allows it
Smithsonian Open Access and MorphoSource were 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 itAcropora through timeFormations of the PleistoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Lamarck 1816)