Fucoides serra
Smithsonian Institution · CC0 · via Smithsonian. 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
- FucoidesPBDB
- Diet
- "photoautotroph"PBDB, for Algae
Time the record covers
At least 6.2 million years on record.
The record covers at least 475.6 Mya to 469.4 Mya. No occurrence read is dated outside 488.9 Mya to 458.2 Mya.
17 occurrences of Fucoides serra on record, most of them in the Ordovician. 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
17 occurrences- Cambrianunder 1%
- Ordovician99%
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
6 formations
- Aorangi Mine Formation12
- Ningkuo Formation1
- Lower Road River Formation · Road River Group1
- Al Rose Formation1
- Cochinoca-Escaya Magmatic Sedimentary Complex Formation1
- Sementsovskaya Formation1
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The named rock units Fucoides serra has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Fucoides serra and its relatives
OrdovicianWhere Fucoides serra and its relatives were recorded in the Ordovician.
Found in the same rock
82 taxa- Isograptus victoriae maximodivergens9 sites
- Didymograptus8 sites
- Pseudisograptus6 sites
- Baltograptus deflexus5 sites
- Isograptus caduceus imitatus5 sites
- Tetragraptus reclinatus5 sites
- Isograptus4 sites
- Phyllograptus4 sites
- Pseudisograptus hastatus4 sites
- Tetragraptus amii4 sites
- Tetragraptus quadribrachiatus4 sites
- Cardiograptus morsus3 sites
- Dichograptus3 sites
- Didymograptus extensus3 sites
- Goniograptus3 sites
- Goniograptus macer3 sites
- Tetragraptus3 sites
- Tristichograptus sp.3 sites
- Apiograptus2 sites
- Cryptograptus2 sites
- Etagraptus harti2 sites
- Graptoloidea2 sites
- Harrisgraptus eocaduceus2 sites
- Isograptus caduceus australis2 sites
The Paleobiology Database records 17 sites for Fucoides serra, 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
6 references- Ordovician Geology and Graptolite faunas of the Aorangi Mine area, North-west Nelson, New Zealand12
- Early-Middle Ordovician graptolites from the Argentine Puna: quantitative paleobiogeographic analysis based on a systematic revision1
- Legend of the Central European series of sheets of the State Geological Map of the Russian Federation, scale 1:1,000,000 (third generation)1
- The sequence and correlation of Early Ordovician (Arenig) graptolite faunas in the Richardson Trough and Misty Creek Embayment, Yukon Territory and District of Mackenzie, Canada1
- Definition of a global boundary stratotype for the Darriwilian Stage of the Ordovician System1
- Fauna of the Lower Ordovician Al Rose Formation, Mazourka Canyon, Inyo County, California1
Each of the 17 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 Fucoides serra
- Source
- Smithsonian
- Credit
- Smithsonian Institution
- Licence
- CC0 — this site’s default, not the record’s
- Commercial use
- the licence allows it
No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itFucoides through timeFormations of the OrdovicianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Brongniart 1828)