Tridacna
Tridacna is a genus of large saltwater clams, marine bivalve molluscs in the subfamily Tridacninae, the giant clams. Many Tridacna species are threatened. They have heavy shells, fluted with 4 to 6 folds. The mantle is often brightly coloured. They inhabit shallow waters of coral reefs in warm seas of the Indo-Pacific region. These clams are popular in marine aquaria, and in some areas, such as the Philippines, members of the genus are farmed for the marine aquarium trade. They live in symbiosis with photosynthetic algae (zooxanthellae). Some species are eaten by humans.

Charles J. Sharp · CC BY-SA 4.0 · 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
- TridacninaePBDB
- Diet
- photosymbiotic, suspension feederPBDB, for Tridacninae
- Life habit
- epifaunal, solitaryPBDB, for Tridacninae
- Motility
- stationary, attachedPBDB, for Tridacninae
- Vision
- limitedPBDB
- Environment
- marinePBDB, for Tridacninae
Time the record covers
At least 20 million years on record.
The record covers at least 20.45 Mya to 11.7 ka. No occurrence read is dated outside 23.04 Mya to 0 Mya.
83 occurrences of Tridacna 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
83 occurrences- Miocene13%
- Pliocene2%
- Pleistocene72%
- 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
11 formations
- Aldabra Limestone Formation8
- Cilanang Formation3
- Abbas Formation2
- Lower Gelingseh Formation2
- Takamaka Limestone Formation2
- Ryukyu Limestone Formation · Sakishima Group1
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The named rock units Tridacna has been recovered from, largest first. Drawn where the rock is now, not where it formed. 60 occurrences have no formation on record, which is common for older literature.
Tridacna and its relatives
PleistoceneWhere Tridacna and its relatives were recorded in the Pleistocene.
Found in the same rock
719 taxa- Conus10 sites
- Spondylus9 sites
- Anadara (Anadara) antiquata8 sites
- Strombus8 sites
- Cerithium7 sites
- Chlamys7 sites
- Conus arenatus7 sites
- Acar plicata6 sites
- Cypraea6 sites
- Natica6 sites
- Periglypta reticulata6 sites
- Strombus (Gibberulus) gibberulus6 sites
- Turbo (Turbo) petholatus6 sites
- Barbatia5 sites
- Chama5 sites
- Codakia tigerina5 sites
- Mitra5 sites
- Naria erosa5 sites
- Rhinoclavis5 sites
- Strombus fasciatus5 sites
- Tellina5 sites
- Tritia5 sites
- Turbo (Marmarostoma) radiatus5 sites
- Acropora4 sites
The Paleobiology Database records 27 sites for Tridacna, 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
41 references- Faunal response to the instability of reef habitats: Pleistocene molluscan assemblages of Aldabra Atoll10
- Pleistocene Coral Reef Terraces on the Saudi Arabian Side of the Gulf of Aqaba, Red Sea8
- Skwarko, 19945
- Late Pleistocene molluscan assemblages from the coral reefs of the Kenya coast5
- Molluschi delle spiagge emerse del Mar Rosso e dell'Oceano Indiano, parte II (Lamellibranchi) [Mollusks from raised beaches bordering the Red Sea and the Indian Ocean, part II (bivalves)]5
- Biofacies and diagenetic alterations of the Pleistocene coral reefs, northwest Red Sea coast, Saudi Arabia4
- The Fossil Coral Reefs of Al-Aqaba, Jordan4
- Pleistocene mollusc assemblage in the slightly raised atoll lagoon of Niau (Tuamotu, French Polynesia)3
- Radiocarbon ages of beach rocks and late Holocene sea-level changes in the southern part of the Nansei Islands, southwest of Japan3
- Mollusques Pleistocenes de la Cote Francaise des Somalis [Pleistocene molluscs from French Somaliland]3
- Pleistocene morphology and Holocene emergence of Christmas (Kiritimati) Island, Pacific Ocean2
- The geology of the Farsan Islands, Oizan and Kamaran Island, Red Sea. Part 2.- Molluscan palaeontology.2
Each of the 83 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. 29 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 content3
Picture of Tridacna
- Source
- Wikipedia/Commons
- Credit
- Charles J. Sharp
- Licence
- CC BY-SA 4.0
- Commercial use
- the licence allows it
Photogrammetry
- Source
- MorphoSource
- Licence
- not stated by the source
- Commercial use
- cannot be read from the licence given — check the record
- Specimen
- Tridacna gigas · MST:PALEO:MST-SP-3741
3D model
- Source
- Sketchfab
- Licence
- CC0 Public Domain
- Commercial use
- the licence allows 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
- Source
- Wikipedia, “Tridacna”
- 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 itTridacninae through timeFormations of the PleistoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Bruguière 1797