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The Earth Story

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This is the blog homepage of the Facebook group "The Earth Story" (Click here to visit our Facebook group). “The Earth Story” are group of volunteers with backgrounds throughout the Earth Sciences. We cover all Earth sciences - oceanography, climatology, geology, geophysics and much, much more. Our articles combine the latest research, stunning photography, and basic knowledge of geosciences, and are written for everyone!
We hope you find us to be a unique home for learning about the Earth sciences, and we hope you enjoy!
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Mesozoic Monthly: Aspidorhynchus

As we all seek out responsible ways to enjoy our summer months while the world continues to respond to COVID-19, many of us are embracing the therapeutic effects of the great outdoors. One popular activity, especially in and around the Three Rivers, is fishing. Some modern fishes look positively primeval, as if they were hooked straight out of the Age of Dinosaurs and reeled into the present day. For July’s edition of Mesozoic Monthly, our star is Aspidorhynchus, one of the weird and wonderful fishes that inhabited the oceans of the Mesozoic Era.

Let’s start with a quick lesson on fish, for context. There are two main groups of bony fishes. One group, the class Sarcopterygii, are called the lobe-finned fishes because they have fleshy, limb-like fins that they use to paddle through the water like oars. The first vertebrates to go on land were sarcopterygians, and the descendants of these adventurous fish eventually evolved into amphibians, reptiles, and mammals – including us! Despite their prolific limbed descendants, sarcopterygians make up only a small fraction of fishes today. The vast majority of fish belong to the other class: Actinopterygii, or the ray-finned fishes. These fishes have delicate ray-like bones supporting thinly webbed fins instead of the meaty fins of the sarcopterygians. Actinopterygians are so successful that they dominate both freshwater and saltwater ecosystems, thrive in a variety of habitats, and fill various ecological niches. Such diverse lifestyles mean that actinopterygians come in many shapes and sizes. Nemo (a clownfish) is an actinopterygian. So is the barracuda that ate his mother, the catfish in the Monongahela River, and the unfortunate goldfish you won at the carnival as a kid. Most fossil fishes, like Aspidorhynchus for example, are also actinopterygians.

Aspidorhynchus is an extinct member of the order Holostei, nested, in diagrams of relatedness, within the class Actinopterygii. The only members of the Holostei today are gars and bowfins. Superficially, Aspidorhynchus looks like a gar, but it is more closely related to bowfins. Its name means “shield snout,” in reference to its pointy, swordfish-like upper jaw. Unlike swordfish, which lack teeth as adults, this snout was filled with many sharp teeth. The limited flexibility of its skull restricted its diet to tiny fish, two inches (5 centimeters) in diameter at the largest. Aspidorhynchus was not very large itself, its slender body only growing to approximately two feet (60 centimeters) in length. It was covered with ganoid scales, which are hard, diamond-shaped scales made with a shiny compound called ganoin. Only a few types of modern fishes have ganoid scales, including gar, sturgeon, and paddlefish.

Jurassic feeding frenzy: the pterosaur (flying reptile) Rhamphorhynchus and the predatory fish Aspidorhynchus attack a school of smaller fish. Usually, the baitfish were the only casualties here, but once in a while, everybody lost (see below!). Art by RavePaleoArt on DeviantArt, reproduced with permission.

Although species of Aspidorhynchus lived in the Jurassic and Cretaceous periods, we know that it encountered the same struggles as some modern fish due to several remarkable fossils. Just like swordfish, the pointy snout of Aspidorhynchus frequently got it into trouble by impaling other animals! The abundance of fossil evidence for this was provided by the unique conditions of the habitat preserved in the famous Solnhofen Limestone of Germany. In the Late Jurassic, this area was an isolated series of lagoons that accumulated a bottom layer of anoxic brine, which is extra-salty, low-oxygen water where oxygen-dependent (aerobic) life cannot survive. Despite this, the surface still teemed with life: fishes and marine reptiles dominated the water, small non-avian dinosaurs scurried along the shore, and pterosaurs (flying reptiles) and archaic birds flew overhead. The fish-eating pterosaur Rhamphorhynchus seems to have been a fairly frequent victim of the snout of Aspidorhynchus, with multiple fossils documenting unfortunate collisions in which the fish’s snout pierced and became entangled in the wing membrane of the pterosaur. (For a summary of pterosaur wings, check out the March edition of Mesozoic Monthly, on Nemicolopterus.) It’s obvious from the size of the animals that neither was trying to eat the other, but somehow, they became stuck together. As the two animals struggled to survive, they slowly drifted downward into the anoxic brine, where they suffocated and settled onto the bottom of the lagoon. If any other animals had tried to eat or otherwise disturb the corpses, they would have died in the brine as well, so the fossils of the Solnhofen Limestone are typically pristine and undisturbed by scavengers.

Three views of the most famous (and probably the most beautiful) Aspidorhynchus vs. Rhamphorhynchus fossil from the Upper Jurassic Solnhofen Limestone of southern Germany. Avid fisherman Matt Lamanna, the head of Vertebrate Paleontology at Carnegie Museum of Natural History (CMNH), jokes that the Aspidorhynchus looks angry, as if it’s mad about getting its snout stuck in the Rhamphorhynchus and dooming them both. Sorry Matt, this is just a quirk of preservation – the compression of the Aspidorhynchus skull during fossilization gave it the appearance of having grouchy eyebrows that weren’t there in life. You can learn more about this specimen in a paper by Frey and Tischlinger (2012). And if you want to see real fossils of both of these animals in person (albeit preserved separately), come visit the Solnhofen case in CMNH’s Dinosaurs in Their Time exhibition.

Because Aspidorhynchus lived only during the Mesozoic, there’s no chance that a modern-day angler will ever hook one. But should you find yourself fishing in one of Pennsylvania’s rivers or lakes this summer, and manage to land a gar or bowfin, pause for a moment and reflect on the ancient legacy of these fishes – a heritage that dates to the Age of Dinosaurs.

Lindsay Kastroll is a volunteer and paleontology student working in the Section of Vertebrate Paleontology at Carnegie Museum of Natural History. Museum staff, volunteers, and interns are encouraged to blog about their unique experiences and knowledge gained from working at the museum.

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Solnhofen Plattenkalk - rare and beautiful.

For large parts of the Jurassic about 155 million years ago, areas of western Europe were covered by warm, shallow seas. Associated with these is one of the most valuable fossil sites known on Earth. The Solnhofen Plattenkalk or Solnhofen Limestone in Bavaria, Germany, is a Late Jurassic ‘Konservat- Largerstätte’ that preserves a rare and unique assemblage of fossil biota.

During the Late Jurassic the area occupied by the Solnhofen Plattenkalk was an archipelago at the edge of the Tethys Ocean. Extensive coral and sponge reef systems created numerous protected lagoons with limited recharge from the open ocean. As salinity in the lagoons rose high enough for the resulting brine to be toxic to life and since the deepest waters were anoxic, many ordinary scavengers were absent. In this environment of soft, fine sediments the remains of animals living around the lagoons are exceptionally well preserved.

The fossil assemblages are highly diverse, with jellyfish, worms, ammonites, bivalves, prawns, shrimp, lobsters, barnacles, crinoids, echinoids and fish all preserved. Horseshoe crab fossils are also preserved and often found at the distal end of their own tracks, formed as they walked to their demise.

Although there is great diversity from the marine species there is also an abundance of terrestrial life preserved. Fossils of insects, plants, small dinosaurs, lizards, crocodilians, and pterosaurs are all found. The fossils from the Solnhofen Plattenkalk are not numerous, but they are exceptional, including delicate dragonfly wings and over 600 identifiable species of dinosaur. This Konservat-Largerstätte gives an unprecedented view of a complete Jurassic ecosystem.

Does anyone have any kind of fossils of their own? Add some pics into the comments below, we would love to see them.

~ JM

Photo Credit: https://www.paleodirect.com/pgset2/f064.htm For more information: Fossilmuseum.net - http://www.fossilmuseum.net/Fossil_Sites/solnhofen/Solnhofen_Lagerstatt.htm The Solnhofen Limestone of Germany - http://www.ucmp.berkeley.edu/mesozoic/jurassic/solnhofen.html Solnhofen Limestone - http://www.britannica.com/EBchecked/topic/553476/Solnhofen-Limestone Munnecke, A., Westphal, H., & KÖLBL‐EBERT, M. A. R. T. I. N. A. (2008). Diagenesis of plattenkalk: examples from the Solnhofen area (Upper Jurassic, southern Germany). Sedimentology, 55(6), 1931-1946.

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Lithographic limestone

Most of us know that rocks and minerals have played a role as the star material in many art forms, including jewellery making, sculpture, pottery, as well as their use as pigments. But did you know that they are also used behind the scenes?

Lithography is an oil-based printmaking technique that relies on the immiscibility of water and oil. It originated during the 18th century as a way to cheaply print theatrical works. The technique derives its name from the lithographic limestone that was originally used as the etching surface. After the image is chemically "burned" into the stone surface, it creates alternate hydrophillic (water-attractant) and hydrophobic (water-repellent) areas. The hydrophobic areas are what the oil-based ink "sticks" to. After inking, the image is printed with the aid of a press.

Nowadays, mass printing uses polymer-coated metal plates (as part of the offset lithography process), however some fine artists still insist on using limestone to create artworks. The first image shows the limestone slab with the individual layers required to produce a composite image (each would be inked with a different colour), while the second shows an amazingly complex print created with this process.

Lithographic limestone is a hard, homogenous, fine-grained, defect-free type of stone used in the creation of lithographic prints. In geology, lithographic texture refers to a grain size > 1/250 mm.

This type of limestone is formed in shallow, hypersaline, stagnant, anoxic conditions which prevent the sediments from becoming disturbed by benthic (sea-floor dwelling) organisms, growths of microbial mats (algae and bacteria), as well as wave action, allowing it to remain homogenous.

The first quarries of lithographic limestone were found in Solnhofen, and for many years, were the only source of this material until similar rocks were discovered and quarried near Montdardier in France. Solnhofen is also very famous for the high quality fossils it preserves (see the past article by TES linked below). Both deposits were Jurassic in origin, although the French limestone was deposited earlier (200-1800 mya) than the German (155 mya). The USA also began quarrying lithographic limestone around the same time (1868) as its European counterparts. Sadly, once metal plate printing came into effect c. 1918, the quarries were shut down or used for the production of crushed rock.

  • YK

Past articles: Solnhofen Limestone – http://on.fb.me/13LTAdi

Image credit: Lithographic Stone for Anchor Manilla Tropical Gum and Moseleys Air Mail envelopes. Finished label shown. © Edinburgh City of Print, 2009 (http://commons.wikimedia.org/wiki/File:Lithographic_stone_for_Anchor_Manilla_Tropical_Gum.jpg). Used under creative commons licensing. “The Custer Fight” by George Marion Russell, 1903 (http://commons.wikimedia.org/wiki/File:Charles_Marion_Russell_-The_Custer_Fight%281903%29.jpg). Used under public domain license.

Further reading: More on lithography - http://www.britannica.com/EBchecked/topic/343748/lithography A pictorial demonstration of the lithographic process - http://entertainment.howstuffworks.com/arts/artwork/stone-lithography.htm The tectonic setting of lithographic limestone (warning: a lot of geology jargon)-http://www.academia.edu/402877/Tectonic_and_Climatic_setting_of_Lithographic_Limestone_Basins

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A Final Journey Set In Stone

Something unfortunate happened to a horseshoe crab some 150 million years ago. A harsh storm washed it into a toxic lagoon, where it scrambled around and eventually died. What it left behind was remarkable - a perfectly fossilized story of its final, brief journey, capturing the longest, complete death track ever found.

The horseshoe crab, Mesolimulus walchi, was discovered in Solnhofen, Germany, along with many other beautifully fossilized animals. The soft carbonate mud preserved insects, sea jellies, and dinosaurs with great detail. M. walchi was likely a juvenile at the time of its death, measuring 12.7cm long by 6.9cm wide. The toxic lagoon that it was dropped into was highly salty and anoxic (no oxygen).

According to Dean Lomax of the Doncaster Museum & Art Gallery in the U.K. and Christopher Racay of the Wyoming Dinosaur Center, the disturbed surface at the beginning of its trail shows that the horseshoe crab sank to the bottom of the lagoon on its back and struggled to turn upright. It then began its mortichnia, meaning death track or last walk, meandering and making a few turns before becoming distressed. It then began to asphyxiate, leaving behind less uniform, deeper and more erratic imprints as it tried to escape. At the end of the 9.7 meter fossilized trail we find the complete specimen of the crab.

Lomax and Racay dismiss the hypothesis that it was dropped in the lagoon by a flying predator, such as a pterosaur, due to the lack of any predation marks. Lomax writes in the journal Ichnos, “Trackways and trace makers preserved together in the fossil record are rare and such specimens allow unique insights into behavior and ecology.” So our little arthropod friend did not die in vain: its story was set in stone and survived millions of years as one of the most amazing specimens of its kind.

~ SW

Photo credit: Ghedoghedo http://bit.ly/1udDEqt

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Saccocoma tenella

This fossil is one of the most common creatures found in the Jurassic aged Solnhofen limestone, the famous deposits in Germany where the earliest feathered dinosaur fossils were located.

This guy is much tinier and was a free-floating crinoid. Crinoids are some of the most common fossils found in the Paleozoic, but most of them were attached to the ocean floor. These crinoids had no stalk, no connection to the ground. They probably still were filter feeders, taking nutrition from small particles floating in the water, but scientists are still working to understand the details of their motion. Their arms curl up on death, but were most likely extended during life and used to both direct plankton in towards it mouth and maintain its position in the water.

Really cool looking, not as well known fossil from one of the most famous units in the world.

-JBB

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About 130,000 unique and rare fossils from western Europe were purchased by Andrew Carnegie in 1903 from Baron de Bayet, executive secretary to King Leopold II (at turn of last century) Belgium. 

Examples of fossils on exhibit in our core exhibition Dinosaurs in Their Time are from Lyme Regis (England), Holzmaden (Germany), and Solnhofen (Germany). 

The fossils were collected from famous paleontology sites in Europe and United States more than a century ago.

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These fossils were found in a quarry in Solnhofen, Germany, which was once a series of shallow, tropical lagoons. The environmental conditions at Solnhofen resulted in remarkably preserved fossils of Late Jurassic plants, invertebrates, fish, reptiles, and bird species like these fossils on display in Dinosaurs in Their Time.

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Solnhofen Plattenkalk - rare and beautiful.

For large parts of the Jurassic about 155 million years ago, areas of western Europe were covered by warm, shallow seas. Associated with these is one of the most valuable fossil sites known on Earth. The Solnhofen Plattenkalk or Solnhofen Limestone in Bavaria, Germany, is a Late Jurassic ‘Konservat- Largerstätte’ that preserves a rare and unique assemblage of fossil biota.

During the Late Jurassic the area occupied by the Solnhofen Plattenkalk was an archipelago at the edge of the Tethys Ocean. Extensive coral and sponge reef systems created numerous protected lagoons with limited recharge from the open ocean. As salinity in the lagoons rose high enough for the resulting brine to be toxic to life and since the deepest waters were anoxic, many ordinary scavengers were absent. In this environment of soft, fine sediments the remains of animals living around the lagoons are exceptionally well preserved.

The fossil assemblages are highly diverse, with jellyfish, worms, ammonites, bivalves, prawns, shrimp, lobsters, barnacles, crinoids, echinoids and fish all preserved. Horseshoe crab fossils are also preserved and often found at the distal end of their own tracks, formed as they walked to their demise.

Although there is great diversity from the marine species there is also an abundance of terrestrial life preserved. Fossils of insects, plants, small dinosaurs, lizards, crocodilians, and pterosaurs are all found. The fossils from the Solnhofen Plattenkalk are not numerous, but they are exceptional, including delicate dragonfly wings and over 600 identifiable species of dinosaur. This Konservat-Largerstätte gives an unprecedented view of a complete Jurassic ecosystem.

Does anyone have any kind of fossils of their own? Add some pics into the comments below, we would love to see them.

~ JM

Photo Credit: https://www.paleodirect.com/pgset2/f064.htm For more information: Fossilmuseum.net - http://www.fossilmuseum.net/Fossil_Sites/solnhofen/Solnhofen_Lagerstatt.htm The Solnhofen Limestone of Germany - http://www.ucmp.berkeley.edu/mesozoic/jurassic/solnhofen.html Solnhofen Limestone - http://www.britannica.com/EBchecked/topic/553476/Solnhofen-Limestone Munnecke, A., Westphal, H., & KÖLBL‐EBERT, M. A. R. T. I. N. A. (2008). Diagenesis of plattenkalk: examples from the Solnhofen area (Upper Jurassic, southern Germany). Sedimentology, 55(6), 1931-1946.

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Fossil squid While we are all familiar with some of the hard shells of these ancient creatures from the fossil record such as ammonites and belemnites, finding one with its soft parts preserved as well as this is almost as rare as hen's teeth. When they dies and sank to the bottom of the sea or were washed onto an ancient shore by the waves, any passing carnivore would take a bite or two, and they were finished off by the usual bacteria that promote decay. This specimen, nearly 30 cm long died in an ancient anoxic lagoon by a Jurassic shore in what is now Germany some 150 million years ago. The lack of oxygen allowed preservation of the soft parts in what is now famed as one of the premier fossil sites in the world, the Solnhoffen lithographic limestone (so called because pictures were etched onto its surface for printing). This formation is renowned for the discovery of the first specimen of archaeopteryx, complete with its feathers, that sparked off a still ongoing debate about the evolution of birds from dinosaurs. Loz Image credit: LGF Foundation

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A Final Journey Set In Stone Something unfortunate happened to a horseshoe crab some 150 million years ago. A harsh storm washed it into a toxic lagoon, where it scrambled around and eventually died. What it left behind was remarkable - a perfectly fossilized story of its final, brief journey, capturing the longest, complete death track ever found. The horseshoe crab, Mesolimulus walchi, was discovered in Solnhofen, Germany, along with many other beautifully fossilized animals. The soft carbonate mud preserved insects, sea jellies, and dinosaurs with great detail. M. walchi was likely a juvenile at the time of its death, measuring 12.7cm long by 6.9cm wide. The toxic lagoon that it was dropped into was highly salty and anoxic (no oxygen). According to Dean Lomax of the Doncaster Museum & Art Gallery in the U.K. and Christopher Racay of the Wyoming Dinosaur Center, the disturbed surface at the beginning of its trail shows that the horseshoe crab sank to the bottom of the lagoon on its back and struggled to turn upright. It then began its mortichnia, meaning death track or last walk, meandering and making a few turns before becoming distressed. It then began to asphyxiate, leaving behind less uniform, deeper and more erratic imprints as it tried to escape. At the end of the 9.7 meter fossilized trail we find the complete specimen of the crab. Lomax and Racay dismiss the hypothesis that it was dropped in the lagoon by a flying predator, such as a pterosaur, due to the lack of any predation marks. Lomax writes in the journal Ichnos, “Trackways and trace makers preserved together in the fossil record are rare and such specimens allow unique insights into behavior and ecology.” So our little arthropod friend did not die in vain: its story was set in stone and survived millions of years as one of the most amazing specimens of its kind. ~ SW For more info: http://www.sci-news.com/paleontology/article00554.html (Original paywalled article) http://www.tandfonline.com/doi/abs/10.1080/10420940.2012.702704#preview Photo credit: Ghedoghedo http://bit.ly/1udDEqt

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Saccocoma tenella This fossil is one of the most common creatures found in the Jurassic aged Solnhofen limestone, the famous deposits in Germany where the earliest feathered dinosaur fossils were located. This guy is much tinier and was a free-floating crinoid. Crinoids are some of the most common fossils found in the Paleozoic, but most of them were attached to the ocean floor. These crinoids had no stalk, no connection to the ground. They probably still were filter feeders, taking nutrition from small particles floating in the water, but scientists are still working to understand the details of their motion. Their arms curl up on death, but were most likely extended during life and used to both direct plankton in towards it mouth and maintain its position in the water. Really cool looking, not as well known fossil from one of the most famous units in the world. -JBB Image credit: https://www.flickr.com/photos/worf/215445272 Read more: http://link.springer.com/article/10.1007%2Fs00015-011-0059-z http://www.palass-pubs.org/palaeontology/pdf/Vol37/Pages%20121-129.pdf http://www.ucmp.berkeley.edu/mesozoic/jurassic/solnhofen.html

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