The Chemnitz petrified forest is a

petrified forest Petrified wood, also known as petrified tree (from Ancient Greek meaning 'rock' or 'stone'; literally 'wood turned into stone'), is the name given to a special type of ''fossilized wood'', the fossilized remains of terrestrial vegetation. ''P ...

Chemnitz Chemnitz (; from 1953 to 1990: Karl-Marx-Stadt , ) is the third-largest city in the German state of Saxony after Leipzig and Dresden. It is the 28th largest city of Germany as well as the fourth largest city in the area of former East Germany a ...

, Germany. Most of the trunks are exhibited in the Museum of Natural History in Chemnitz inside of Kulturkaufhaus Tietz , including slices of trunks with polished edges. A small collection can be seen also on Zeißstraße (Hilbersdorf, 1911). From April 4, 2008, to Fall 2011, an excavation in Hilbersdorf was held to find and research more trunks. Their researchers discovered, amongst others, ''

Arthropitys bistriata ''Arthropitys'' is an extinct genus of calamitacean equisetale. The petrified fossils of ''Arthropitys bistriata'', the type species, can be found at Chemnitz petrified forest, Chemnitz, Germany. History Petrified trunks of tree ferns, seed ...

'', a type of

Calamites ''Calamites'' is a genus of extinct arborescent (tree-like) horsetails to which the modern horsetails (genus ''Equisetum'') are closely related. Unlike their herbaceous modern cousins, these plants were medium-sized trees, growing to heights o ...

, giant horsetails that are ancestors of modern

horsetails ''Equisetum'' (; horsetail, snake grass, puzzlegrass) is the only living genus in Equisetaceae, a family of ferns, which reproduce by spores rather than seeds. ''Equisetum'' is a "living fossil", the only living genus of the entire subclass Eq ...

, found on this location with never seen multiple branches. Many more plants and animals from this excavation are still in an ongoing research. This exceptional find received the 2010 Fossil of the Year award of the German Paleontological Society. It was integrated into the permanent exhibition.

History

Georgius Agricola (1494-1555) described petrified trees in the Chemnitz area first at 1546. Versteinerter Wald Chemnitz 2009

Petrified In geology, petrifaction or petrification () is the process by which organic material becomes a fossil through the replacement of the original material and the filling of the original pore spaces with minerals. Petrified wood typifies this proce ...

trunks of

tree ferns The tree ferns are arborescent (tree-like) ferns that grow with a trunk elevating the fronds above ground level, making them trees. Many extant tree ferns are members of the order Cyatheales, to which belong the families Cyatheaceae (scaly tree ...

seed ferns A seed is an embryonic plant enclosed in a protective outer covering, along with a food reserve. The formation of the seed is a part of the process of reproduction in seed plants, the spermatophytes, including the gymnosperm and angiosperm pl ...

conifers Conifers are a group of cone-bearing seed plants, a subset of gymnosperms. Scientifically, they make up the division Pinophyta (), also known as Coniferophyta () or Coniferae. The division contains a single extant class, Pinopsida. All extan ...

as well as

Cordaitales Cordaitales are an extinct order of gymnosperms, known from the early Carboniferous to the late Permian. Many Cordaitales had elongated strap-like leaves, resembling some modern-day conifers of the Araucariaceae and Podocarpaceae. They had cone ...

and different species of

. The primeval plants were repeatedly discovered from the 17th century ongoing till today and mostly at Hilbersdorf, today a district of Chemnitz. In the mid-18th century, gemstone prospector David Frenzel (1691-1772) found numerous examples of this wood in the hills in and around Chemnitz. One of his 1751 finds is one of the few petrified wood specimens still possessing its roots (Megadeudron saxonicum). This petrified wood was transported to Dresden (Zwinger, for exhibition in the Roayal Saxon Museum). Later a collector, the Hilbersdorf contractor Güldner, bequeathed some of the petrified logs to King Albert Museum in Chemnitz. The first director of the Museum, Johann Traugott Sterzel (1841-1914), took over the investigation of the findings. The Sterzeleanum in the museum (the petrified forest display) is dedicated to him.

Creation of the petrified forest

The petrified forest was formed in connection with the eruption of the Zeisigwald

volcano A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are ...

in the lower

Permian The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleoz ...

and dates back about 291 million years.Senckenberg Gesellschaft für Naturforschung ''Chemnitzer Wald ist 291 Millionen Jahre alt''
/ref> The trees were uprooted or snapped off by the eruption and the amount of

tephra Tephra is fragmental material produced by a volcanic eruption regardless of composition, fragment size, or emplacement mechanism. Volcanologists also refer to airborne fragments as pyroclasts. Once clasts have fallen to the ground, they rem ...

, much like the trees caught in the

1980 eruption of Mount St. Helens On March 27, 1980, a series of volcanic explosions and pyroclastic flows began at Mount St. Helens in Skamania County, Washington, United States. A series of phreatic blasts occurred from the summit and escalated until a major explosive eru ...

. The trunks were then covered with hot

. In the following of years, the

silicic acid Silicon dioxide, also known as silica, is an oxide of silicon with the chemical formula , most commonly found in nature as quartz and in various living organisms. In many parts of the world, silica is the major constituent of sand. Silica is one ...

included in the tephra ensured the fossilization of Permian plants, preserving them until today.

Fauna

The

varanopid Varanopidae is an extinct family of amniotes that resembled monitor lizards and may have filled a similar niche, hence the name. Typically, they are considered synapsids that evolved from an ''Archaeothyris''-like synapsid in the Late Carbonifero ...

Ascendonanus ''Ascendonanus'' (meaning "climbing dwarf") is an extinct genus of varanopid amniote from the Early Permian of Germany. It is one of the earliest specialized arboreal (tree-living) tetrapods currently known and outwardly resembled a small lizard ...

'' As well as reptiles, amphibians, gastropods and arthropods, including the

trigonotarbid The order Trigonotarbida is a group of extinct arachnids whose fossil record extends from the late Silurian to the early Permian (Pridoli epoch, Pridoli to Sakmarian).Dunlop, J. A., Penney, D. & Jekel, D. 2020A summary list of fossil spiders and ...

'' Permotarbus'' and scorpion ''

Opsieobuthus ''Opsieobuthus'' is an extinct genus of centromachid scorpion. The type species ''O. pottsvillensis'' was named from the late Carboniferous of Clay City, Indiana. A second species ?''O. tungeri'' was tentatively assigned to the genus from the ...

'' are known from the forest.

References

External links

* {{coord, 50, 49, 51, N, 12, 55, 22, E, type:landmark, display=title Petrified forests Paleontology in Germany History of Chemnitz Culture in Chemnitz

History

Creation of the petrified forest

Fauna

References

Further reading

External links