The Figueroa Sulfide (also known as Figueroa Hydrothermal vent or Figueroa Massive Sulfide) is a geological formation in California, USA, dating to roughly between 185 and 181 million years ago and covering the Pliensbachian-Toarcian stages of the Jurassic Period in the Mesozoic Era.[1][2][3] This deposits represent deep sea Hydrothermal vents, with the oldest confirmed record of Siboglinidae and adjecent biotas, being one of the oldest records of such ecosystem, with other similar ones along the American Continent, for example from Los Molles Formation.[2][4][5]
| Figueroa Sulfide | |
|---|---|
| Stratigraphic range: Pliensbachian-Toarcian ~ | |
| Type | Geological formation |
| Unit of | Franciscan Complex |
| Area | San Rafael Mountains |
| Thickness | 40 m |
| Lithology | |
| Primary | sulfide lens; lithified chert |
| Location | |
| Location | California |
| Coordinates | 34°42′N 119°48′W / 34.7°N 119.8°W |
| Approximate paleocoordinates | 23°12′S 57°00′W / 23.2°S 57.0°W |
| Region | California |
| Country |  United States |
| Type section | |
| Named for | Figueroa Mountain |
  Figueroa Sulfide (the United States) | |
Paleoenvironment
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The Figueroa Sulfide is located in the San Rafael Mountains and is part of the Franciscan Complex, which formed during subduction of the Farallon Plate. This geological formation includes altered basalts, serpentinites, cherts, and tectonically sheared mudstones.[3][6] The Figueroa Sulfide consists of a 1.5-meter-thick sulfide lens with a silicified core, flanked by more friable sulfides, and is structurally overlain by altered volcanics and cherts. The deposit shows evidence of tectonic brecciation and oxidation before silica deposition. Though small and not viable for large-scale mining, its mineralization and vent structures suggest similarities to modern Hydrothermal vent systems.[3][6]
Biostratigraphic analysis of the Figueroa Sulfide, based on radiolarian fossils extracted from chert samples, indicates a late Pliensbachian to early Toarcian age. The presence of key radiolarian taxa, such as Parahsuum ovale and Bagotum sp., supports this dating.[1][2] Taphonomically, fossils found in the deposit, including brachiopods, gastropods, and vestimentiferan tubes, are preserved as pyrite molds, replicating fine details of the original shells and tubes. These fossils suggest an ancient hydrothermal vent community, where organisms like tube worms and brachiopods likely relied on chemosynthetic bacteria for nutrition, mirroring modern vent ecosystems.[1][2]
The Figueroa sulfide fossil assemblage differs from modern vent communities in species diversity, composition, and trophic structure.[1][2] Unlike modern vents, the Figueroa Sulfide has only three species, lacks common taxa such as Vesicomyidae and Bathymodiolus bivalves, arthropods, and gastropods, and has no predators. Possible explanations for these differences include taphonomic bias, where only high-temperature vent species were fossilized, and a genuinely low-diversity Jurassic vent ecosystem. Some "missing" taxa, such as Vesicomyidae, likely evolved later, supported by their fossil record starting in the early Cretaceous and molecular divergence estimates.[1][2]
Biota
editRadiolarians
edit| Genus | Species | Stratigraphic position | Material | Notes | Images |
|---|---|---|---|---|---|
| Bagotum[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Bagotidae | |
| Canoptum[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Parvicingulidae | |
| Canutus[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Bagotidae | |
| Crucella[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Hagiastridae | |
| Dictyomitrella[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Parvicingulidae | |
| Eucyrtidiellum[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Eucyrtidiellidae | |
| Katroma[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Syringocapsidae | |
| Napora[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Ultranaporidae | |
| Pantanellium[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Pantanelliidae | |
| Parahsuum[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Hsuidae | |
| Paronaella[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Angulobracchiidae | |
| Praeconocaryomma[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Praeconocaryommidae | |
| Pseudoristola[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Parvicingulidae | |
| Staurolonche[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Stylosphaeridae | |
| Stichocapsa[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Eucyrtidiidae | |
| Transhsuum[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Hsuidae | |
| Triactoma[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Xiphostylidae | |
| Trillus[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Pantanelliidae | |
| Zartus[1][2] |
|
|
Calcareous Skeletons | A Radiolarian of the family Pantanelliidae |
Brachiopoda
edit| Genus | Species | Stratigraphic position | Material | Notes | Images |
|---|---|---|---|---|---|
| Anarhynchia[2] |
|
|
Shells | A Brachiopod of the family Peregrinellidae |
Gastropoda
edit| Genus | Species | Stratigraphic position | Material | Notes | Images |
|---|---|---|---|---|---|
| Francisciconcha[2] |
|
|
Shells | A Top Snail of the family Trochidae |
Polychaeta
edit| Genus | Species | Stratigraphic position | Material | Notes | Images |
|---|---|---|---|---|---|
| Siboglinidae[1][2] |
|
|
Cylindrical tubes | A Vestimentiferan, considered to be similar to the modern genus Ridgeia, latter resolved among modern vestimentiferans.[7] |
Bibliography
edit- ^ a b c d e f g h i j k l m n o p q r s t u v w x y Little, Crispin T. S.; Herrington, Richard J.; Haymon, Rachel M.; Danelian, Taniel (1999). "Early Jurassic hydrothermal vent community from the Franciscan Complex, San Rafael Mountains, California" (PDF). Geology. 27 (2): 167. doi:10.1130/0091-7613(1999)027<0167:ejhvcf>2.3.co;2. ISSN 0091-7613.
- ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab Little, C. T.; Danelian, T.; Herrington, R. J.; Haymon, R. M. (2004). "Early Jurassic hydrothermal vent community from the Franciscan Complex" (PDF). Journal of Paleontology. 78 (3): 542–559. doi:10.1666/0022-3360(2004)078<0542:ejhvcf>2.0.co;2. ISSN 0022-3360.
- ^ a b c Hagstrum, Jonathan T.; Murchey, Benita L.; Bogar, Robert S. (1996-01-10). "Equatorial origin for Lower Jurassic radiolarian chert in the Franciscan Complex, San Rafael Mountains, southern California". Journal of Geophysical Research: Solid Earth. 101 (B1): 613–626. doi:10.1029/95jb02854. ISSN 0148-0227.
- ^ Georgieva, Magdalena N.; Little, Crispin T.S.; Maslennikov, Valeriy V.; Glover, Adrian G.; Ayupova, Nuriya R.; Herrington, Richard J. (2021). "The history of life at hydrothermal vents". Earth-Science Reviews. 217: 103602. doi:10.1016/j.earscirev.2021.103602. ISSN 0012-8252.
- ^ Gómez-Pérez, Irene (2003). "An Early Jurassic deep-water stromatolitic bioherm related to possible methane seepage (Los Molles Formation, Neuquén, Argentina)". Palaeogeography, Palaeoclimatology, Palaeoecology. 201 (1–2): 21–49. doi:10.1016/s0031-0182(03)00508-x. ISSN 0031-0182.
- ^ a b Wahl, A.D. (1995). "The geology of the Franciscan Complex, San Rafael Mountains me´lange, California". Master’s thesis, University of California, Santa Barbara: 1–121.
- ^ a b Georgieva, Magdalena N.; Little, Crispin T. S.; Watson, Jonathan S.; Sephton, Mark A.; Ball, Alexander D.; Glover, Adrian G. (2017-12-28). "Identification of fossil worm tubes from Phanerozoic hydrothermal vents and cold seeps". Journal of Systematic Palaeontology. 17 (4): 287–329. doi:10.1080/14772019.2017.1412362. ISSN 1477-2019.