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View full screen - View 1 of Lot 4. Sea Lily (Crinoid) Colony on Driftwood.

Sea Lily (Crinoid) Colony on Driftwood

Early Jurassic Period (approx. 180 million years aไgo), Holzmaden, Germany

Live auction begins on:

July 16, 02:00 PM GMT

Estimate

30,000 - 50,000 USD

Bid

20,000 USD

Lot Details

Description

Sea Lily (Crinoid) Colony on Driftwood

Seirocrinus subangularis

Early Jurassic Period (approx. 180 million years ago)

Holzmaden, Germany


41 x 22¼ x 1⅛ inches (104.1 x 56.5 x 2.9 cm). Colony measures 3🧸4¾ x 14 inches (88.3 x 35.6 cm). 98 pounds (44.5 kg).


Numerous sea lily (crinoid) individuals preserved nicely together attached to driftwood on a trimmed matrix slab. Many individual examples show comple🀅te heads and stems. The metallic surfaces on some of the lilies indicate the presence of pyrite. The size ranges of these individuals suggest they were not fully grown at time of death.

This shimmering fossil mural features a colony of crinoids — marine invertebrates colloquially known as "sea lilies" — that lived 180 million years ago in the prehistoric Tethys Ocean that covered much of present-day Europe and Asia. Living almost their entire lives attached to the piece of driftwood seen here, these crinoids flourished in a rich underwater world alongside other marine animals including fish, ammonites, and belemnites. As sessile filter feeders, crinoids relied on the movement of the driftwood or floating debris to which they were attached to venture into areas with adequate food supply. Crinoids were nevertheless able to bend their stalks and flex and extend their arms — the five central appendages in their crowns — so that their mouths could face the water current💖 to capture potential food.


Crinoids bred once a year when their eggs or sperm were released into the water. Once the eggs were released from the parent and fertilized, the resulting embryo would attach itself to a solid substrate such as driftwood where it would develop for several days into a barrel-shap꧙ed, free swimming larva. After several more days, the larva would reattach to the driftwood and develop a rudimentary stem, mouth, and five small arm-like tentacles known as podia. After several more weeks, the crinoid would reach the stalked, sessile stage, where it formed true arms, feather-like pinnules, and a complete set of podia that covered the pinnules and helped move food toward the mouth.


For a reason lost to time, this colony of crinoids succumbed to death and became buried on the sea floor, where the low-oxygen environment allowed for their pristine preservation and🎃 fossilization. Over millions of years, the sediment and animal remains surrounding this crinoid colony petrified and became the shimmering, pyritized Posidonia shale seen here, now famously extracted from the quarries of Holzmaden, Germany.

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