Middle Triassic Ammonoid Fossils From Nevada

Visit a world-famous fossil locality in the Great Basin Desert of Nevada, a specific place that yields some 41 species of ammonoids, in addition to five species of pelecypods and four varieties of belemnites from the Middle Triassic Prida Formation, which is roughly 235 million years old; many paleontologists consider this specific site the single best Middle Triassic, late Anisian Stage ammonoid locality in the world. All told, the Prida Formation yields 68 species of ammonoids spanning the entire Middle Triassic age, or roughly 241 to 227 million years ago.

Also, take a side trip to a classic Late Pleistocene mollusk locality in Nevada, where beaucoup freshwater gastropods and pelecypods occur in the famous Sehoo Formation, approximately 24 to 13 thousand years old.

At left is Parafrenchites meeki, 18mm in diameter. At right is Paraceratites vogdesi, 19mm in diameter.

Contents For--Middle Triassic Ammonoid Fossils From Nevada:

 Images Of Prida Fm. Fossils  Images Of Prida Fm. Ammonoids  Images Of Prida Fm. Fossils In Matrix
     
On-Site Prida Fm. Images Images Of Sehoo Fm. Mollusks On-Site Sehoo Fm. Images
     
Ammonoids Geologic History Links To The Triassic Period Links To Ammonoids
     
BLM Rules For Fossil Collecting My Other Web Pages My Email Address

Geologic History Of Ammonoids

Based on their distinctive suture patterns (a suture is the juncture of the internal partition which separates the cephalopod shell chambers with the shell wall), all ammonoid and ammonite cephalopods can be classified into three separate orders: goniatitic (species with nonserrated sutures, generally considered the most primitive varieties); ceratitic (sutures with serrated lobes)--the kind found in the Middle Triassic Prida Formation discussed at this Web Page; and ammonitic (very complex suturing--usually referred to as the most advanced order of ammonites)--the only order that can properly be termed an ammonite; the goniatitic and ceratitic types are necessarily called ammonoids. The goniatites first appear in the geologic record during the Devonian Period, some 370 million years ago; they persisted all the way up to the great dying at the conclusion of the Permian Period (when trilobites finally disappeared, as well), 248 million years ago. During the Permian Period both ammonoid and the ammonite varieties became common. But by Triassic times (248 to roughly 206 million years ago), only the ceratitic forms proved particularly successful. They, too, died out at the conclusion of that geologic period, leaving only the ammonitic types, the ammonites proper, to carry on the cephalopodal heritage.

Throughout the Jurassic Period (195 to 150 million years ago) ammonitic ammonites thrived, becoming increasingly complex and numerous in the oceans of the Mesozoic world. And, even though ammonites began a long, slow decline over many millions of years during the latter part of the Cretaceous Period, they nevertheless persisted right up to the close of the Mesozoic Era (roughly 65 million years ago), becoming extinct along with all the sensational, terrestrial giants of that age--the dinosaur.

Images Of Fossils From The Prida Formation, Nevada

Middle Triassic (235 Million Years Old)

The fossils imaged here came an isolated outcrop of the Middle Triassic Prida Formation in Nevada on Public Lands (at least at the last time of collecting the site resided on Bureau of Land Management-administered Public Lands). It's a world-famous locality, well known to many amateur ammonoid enthusiasts and professional paleontologists alike--a specific place that yields 41 species of ammonoids, plus five kinds of pelecypods (a remarkable halobiid clam known as Daonella) and four varieties of belemnites; all told, the Prida Formation bears 68 species of ammonoids that span the entire middle Triassic age, or roughly 241 to 227 million years ago. As a matter of fact, the specific Prida Formation site referred to here yields one of the most complete middle Triassic ammonoid successions in the world; and many cephalopod specialists and paleontologists, in general, consider it the single best Middle Triassic, late Anisian Stage (roughly 235 million years old) ammonoid locality in existence. Literally tons of ammonoid-bearing limestones have been removed from the site since its discovery by silver miners in the latter half of the 1800s; that well-preserved, identifiable fossils still occur there, after such concerted searching by hordes of avid ammonoid enthusiasts over many decades, is somewhat of a miracle. In the late 1980s, for example, many law-abiding, conscientious amateur collectors, plus swarms of irresponsible, lawbreaking commercial ammonoid hunters (it is illegal to either sell or barter--in other words, trade--fossils collected on Public Lands) "simultaneously rediscovered" the great fossil locality, creating over the past couple of decades an often frenzied frequency of overcollecting.


The geologic age of the specific, classic ammonoid site is transitional latest Anisian/earliest Ladinian Stage of the Triassic Period, which places the fossils found there directly in the middle of the Mid Triassic, or roughly 235 million years old. At that distant geologic date, what is now the classic Prida fossil locality in the arid Great Basin Desert of Nevada rested at the bottom of a shallow, tropical, warmwater Triassic seaway near the equator.


Please Note: I have heard that the Bureau of Land Management carefully monitors fossil collecting activities at the incomparable MiddleTriassic Prida ammonoid outcrops: the upshot, accordingly, is that commercial fossil collectors caught raiding the Prida strata will most certainly be prosecuted to the fullest extent of the law. There has also been talk that, because commercial collectors have so horribly desecrated the area, the Bureau of Land Management will eventually place the world-class Prida ammonoid locality into a special land-use category called an "Area Of Critical Environmental Concern," a designation that would permanently close the site to all but trained scientists with a degree from an accredited university.

Images Of Ammonoids Free Of Matrix

Middle Triassic Prida Formation, Nevada

Late Anisian/Early Ladinian Stage, 235 Million Years Old

AMMONOIDEA (Ammonoids)

BEYRICHITIDAE

 CERATITIDAE

LONGOBARDITIDAE

JAPONITIDAE

PROTEUSITIDAE

ARCESTIDAE

Images Of Fossils Still In Limestone Matrix

Middle Triassic Prida Formation, Nevada

Late Anisian/Early Ladinian Stage, 235 Million Years Old

AMMONOIDEA (Ammonoids)

 

 BEYRICHITIDAE

 CERATITIDAE

 

 LONGOBARDITIDAE

APLOCOCERATIDAE

PROTEUSITIDAE

Images Of Nonammonoid Fossils In Limestone Matrix

Middle Triassic Prida Formation, Nevada

Late Anisian/Early Ladinian Stage, 235 Million Years Old

COELEOIDEA

XIPHOTEUTHIDIDAE (Belemnites)

PELECYPODA

POSIDONIIDAE (halobiid clams)

 CRINOIDEA

On-Site Images From The Middle Triassic Prida Formation

   
       
   
       
   

Freshwater Mollusks From The Sehoo Formation, Nevada

Upper Pleistocene (24 To 13 Thousand Years Old)

Whenever I visit the incomparable ammonoid-bearing outcrops of the MiddleTriassic Prida Formation, I like to stop off along the way, in Nevada, to hike and fossil-hunt amidst the great badlands deposits of the Upper Pleistocene Sehoo Formation. The Sehoo is roughly 24,000 to 13,000 years old and bears locally plentiful perfectly preserved fossil freshwater gastropods and pelecypods that lived in and around a pluvial lake (created primarily from rainfall) during a particularly wet and cool interglacial period of the late Pleistocene epoch--an interval that, on a world-wide level, geologists believe was fully 2.5 degrees Celsius colder, 65 percent wetter, and experienced 10 percent less evaporation than at present. The Sehoo pluvial system, as a matter of fact, was one of the last great freshwater lakes that existed in late Pleistocene times in what is today the arid Great Basin--a vast body of water that at its highest stand was some 1,330 feet deep (modern-day Lake Tahoe in the Sierra Nevada, by the way, is 1,900 feet deep).

  • Pelecypods: Genus Pisidium Common Name--Peaclam

  • Pelecypods: Genus Pisidium Common Name--Peaclam

  • Pelecypod: Genus Anodonta Common Name--Fat Floater

  • Gastropods: Genus Physa Common Name--Obtuse Physa

  • Gastropod: Genus Stagnicola Common Name--Pondsnail

  • Gastropods: Genus Valvata Common Name--Valve Snail

  • Gastropopds: Genus Planorbis Common Name--Ram's-Horn

On-Site Images Of The Sehoo Formation, Nevada

Upper Pleistocene (24 to 13 Thousand Years Old)

Links To The Triassic Period

Explore The Geologic Interval 248 To 206 Million Years Ago

Ammonoid Links

Places In Cyberspace That Pertain To Ammonoids

Everyone's Invited To Visit My Other Web Sites

And be sure to visit My Pages, where all of the fossils pages I have created are categorized and linked.

 Images Of Prida Fm. Fossils  Images Of Prida Fm. Ammonoids  Images Of Prida Fm. Fossils In Matrix
     
On-Site Prida Fm. Images Images Of Sehoo Fm. Mollusks On-Site Sehoo Fm. Images
     
Ammonoids Geologic History Links To The Triassic Period Links To Ammonoids
     
BLM Rules For Fossil Collecting My Other Web Pages My Email Address

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