#Jurassic echinoidea fossil
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uk-fossils · 1 month ago
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Pseudodiadema depressum Regular Echinoid Fossil, Oxfordian Stage, Jurassic France | Authentic Specimen + COA
Pseudodiadema depressum Regular Echinoid Fossil – Oxfordian Stage, Late Jurassic, Cricqueboeuf, Normandy, France
This fine fossil specimen represents Pseudodiadema depressum, a regular echinoid (sea urchin) from the Oxfordian stage of the Late Jurassic, approximately 159 to 154 million years ago. It was recovered from the fossil-rich marine limestone beds of Cricqueboeuf, a renowned site in Normandy, northern France.
Fossil Type & Species:
Type: Invertebrate Fossil (Regular Echinoid / Sea Urchin)
Species: Pseudodiadema depressum
Phylum: Echinodermata
Class: Echinoidea
Order: Cidaroida
Superfamily: Pseudodiadematoidea
Family: Pseudodiadematidae
Described by: Cotteau, 1863
Geological & Stratigraphic Details:
Location: Cricqueboeuf, Calvados, Normandy, France
Formation: Oxfordian marine limestones
Geological Stage: Oxfordian (Upper Jurassic)
Age: ~159–154 million years ago
Biozone: Perisphinctes ammonite zone (regional correlation)
Depositional Environment: Shallow marine carbonate platform with calm, warm seas; ideal for the preservation of delicate echinoid shells in fine-grained limestones
Morphology & Features: This Pseudodiadema depressum specimen features:
Sub-hemispherical, symmetrical test with clear ambital outline
Densely arranged primary and secondary tubercles forming a detailed lattice across the shell
Well-developed ambulacral and interambulacral zones, sometimes showing fine pore structures
No spines attached, but tubercle structure suggests strong spine-bearing capability
Subtle colour variations from beige to pale brown, depending on matrix contact
Notable: Pseudodiadema depressum is a classic species of Jurassic echinoid used in palaeoenvironmental and biostratigraphic studies. Its compact test and distinctive tubercle patterning make it both scientifically important and visually appealing.
Specimen Details:
Origin: Cricqueboeuf, Normandy, France
Species: Pseudodiadema depressum
Fossil Type: Echinoid Shell (Regular Sea Urchin)
Geological Stage: Oxfordian, Late Jurassic
Size Reference: Scale rule square = 1cm (please refer to the listing photo for full size)
Note: You will receive the exact specimen shown in the photographs
Authenticity & Quality: All our fossils are genuine and professionally selected. This specimen includes a Certificate of Authenticity. No restorations or artificial enhancements are applied.
Why Choose This Fossil? Perfect for:
Fossil and echinoderm collectors
Academic and educational purposes
Natural history displays
Unique gifts with palaeontological value
Shipping & Packaging: Eco-conscious packaging and tracked global shipping ensure secure and swift delivery. Each fossil is packed with care to preserve detail and structure.
Own a finely preserved sea urchin from the Jurassic oceans of France with this authentic Pseudodiadema depressum echinoid fossil.
All of our Fossils are 100% Genuine Specimens & come with a Certificate of Authenticity.
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justonemorerock · 4 years ago
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New Sand Dollars (Echinoidea) have just gone live on both stores! Sand Dollar Fossils (Echinoidea) are fossilised sea urchins from the Jurassic period and are around approximately 145 - 200 million years old. Keywords: Transformation & Growth. https://www.instagram.com/p/CVhSST6vsnJ/?utm_medium=tumblr
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fenglichina-blog · 8 years ago
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Chalk Industrial Grinding Machine
Chalk is a soft, white, porous sedimentary carbonate rock, a form of limestone composed of the mineral calcite. Calcite is calcium carbonate or CaCO3. It forms under reasonably deep marine conditions from the gradual accumulation of minute calcite shells (coccoliths) shed from micro-organisms called coccolithophores. Flint (a type of chert unique to chalk) is very common as bands parallel to the bedding or as nodules embedded in chalk. It is probably derived from sponge spicules or other siliceous organisms as water is expelled upwards during compaction. Flint is often deposited around larger fossils such as Echinoidea which may be silicified (i.e. replaced molecule by molecule by flint).
Chalk as seen in Cretaceous deposits of Western Europe is unusual among sedimentary limestones in the thickness of the beds. Most cliffs of chalk have very few obvious bedding planes unlike most thick sequences of limestone such as the Carboniferous Limestone or the Jurassic oolitic limestones. This presumably indicates very stable conditions over tens of millions of years.
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uk-fossils · 1 month ago
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Acrosalenia hemicidaroides Echinoid Fossil + Spines, Bajocian Stage, Jurassic France | Rare Authentic Specimen + COA
Acrosalenia hemicidaroides Echinoid Fossil with Spines – Bajocian Stage, Middle Jurassic, Neufchâteau, France
This exceptionally rare fossil specimen features a beautifully preserved Acrosalenia hemicidaroides echinoid, complete with fossilised spines, from the Bajocian stage of the Middle Jurassic, approximately 170 to 168 million years ago. It was discovered in the renowned marine fossil deposits of Neufchâteau, northeastern France.
Fossil Type & Species:
Type: Invertebrate Fossil (Echinoid/Sea Urchin + Detached Spines)
Species: Acrosalenia hemicidaroides
Phylum: Echinodermata
Class: Echinoidea
Order: Cidaroida
Family: Hemicidaridae
Described by: d'Orbigny, 1850 (species known since the mid-19th century)
Geological & Stratigraphic Details:
Location: Neufchâteau, Vosges, France
Formation: Bajocian marine limestone/marl layers
Geological Stage: Bajocian, Middle Jurassic
Age: ~170–168 million years ago
Depositional Environment: Shallow marine carbonate platform, ideal for echinoderm preservation due to low-energy sedimentation and early calcite mineralisation
Biozone: Bajocian ammonite biozones (exact echinoid zonation not formally assigned)
Morphology & Features: This fossil displays key traits of Acrosalenia hemicidaroides:
Spherical to sub-hemispherical test (shell) with intricate tubercle patterns
Thick, robust primary spines, often found detached and fossilised alongside the test
Ambulacral plating in orderly radial arrangement with fine granulation
Distinct oral and aboral surfaces, sometimes visible in partially exposed or prepared examples
Colour ranges from pale grey to light brown due to local matrix mineralisation
Notable: This species is a classic example of Jurassic cidaroid echinoids and is rarely found with spines preserved in association. The presence of spines makes this a scientifically significant and highly aesthetic specimen, ideal for both collectors and educators.
Specimen Details:
Origin: Neufchâteau, France
Species: Acrosalenia hemicidaroides
Fossil Type: Echinoid (Sea Urchin) Test and Spines
Geological Stage: Bajocian, Middle Jurassic
Size Reference: Scale rule square = 1cm (see listing photos for accurate sizing)
Note: The specimen pictured is the exact item you will receive
Authenticity & Quality: All our fossils are guaranteed genuine and carefully selected. This piece includes a Certificate of Authenticity and has not been restored or enhanced.
Why Choose This Fossil? An ideal specimen for:
Serious fossil collectors and echinoderm enthusiasts
Museum or university-level palaeontology displays
Decorative fossil showcases
Education in marine palaeobiology and Jurassic ecosystems
Shipping & Packaging: All items are professionally packed with eco-conscious materials and shipped via tracked services for safe delivery.
Add a stunning piece of Jurassic marine life to your collection with this rare Acrosalenia hemicidaroides echinoid fossil complete with spines from Neufchâteau, France.
All of our Fossils are 100% Genuine Specimens & come with a Certificate of Authenticity.
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