Tempskya Sp

''Tempskya'' is an extinct genus of tree fern that lived during the Cretaceous period. Fossils have been found across both the Northern and Southern hemispheres. The growth habit of ''Tempskya'' was unlike that of any living fern or any other living plant, consisting of multiple conjoined dichotomous branching stems enmeshed within roots that formed a "false trunk".

Description

The trunk of ''Tempskya'' was actually a large collection of stems surrounded by adventitious roots. The false trunks can reach up to in height and up to in diameter. Small leaves grew from various points across the height of the trunk. This is in contrast to most tree ferns, where typically large leaves grow from the top of the trunk. Thin leaves have been discovered for the first time on ''Tempskya wyomingense'' specimens; the more commonly seen fossilized leaf bases show that they covered the upper part of the trunk.

Hypothesized growth pattern

Examination of cross sections of various ''Tempskya'' specimens shows that those with the largest trunks have the smallest number of stems, and vice versa. From this, a possible growth pattern of ''Tempskya'' has been suggested: at the sporeling stage, ''Tempskya'' would consist of a single stem, which would begin to branch off distally. A "mantle" of adventitious roots would then develop around the stems to support them. Later on, many of the stems would begin to decay, while the adventitious roots would still provide support and absorb water for the grown plant. This growth pattern has also been hypothesized for ''Psaronius''.

Ecology

''Tempskya'' is thought to have grown in lowland environments close to water, like wetlands and riverbanks.

Taxonomy

The first fossils of ''Tempskya'' was originally described in 1824 as the ''Endogenites erosa'' by Stokes and Webb, who considered it to be a palm tree. The genus ''Tempskya'' was named by August Carl Joseph Corda in 1845, from specimens found in what is now the Czech Republic. The four species originally described by Corda were, in order: ''Tempskya pulchra'', ''Tempskya macrocaula'', ''Tempskya microrrhiza'', and ''Tempskya schimperi''.

''Tempskya'' is the sole member of the family Tempskyaceae. The family has been placed in the order "Filicales", which is now split into a number of orders of leptosporangiate ferns. They have been suggested to members of Cyatheales, based on morphological similarities of the petiole and spores to some members of that order.

Species

Most taxonomists divide ''Tempskya'' species into two groups, those with a simple cortex with only a parenchymatous inner cortex without sclerenchyma, while other species have an inner cortex with either discontinuous or continuous layers of sclerenchyma.

* Parenchymatous inner cortex group:
** ''Tempskya iwatensis'' Nishida, 1986 Taneichi Formation, Japan, Late Cretaceous (Santonian)
** ''Tempskya rossica'' Kidston and Gwynne Vaughan, 1911 Mugadjar, Kazakhstan, Upper Cretaceous?
** ''Tempskya uemurae'' Nishida, 2001 Taneichi Formation, Japan, Late Cretaceous (Santonian)
** ''Tempskya dernbachii'' Tidwell et Wright, 2003 emend. Martínez, Martínez and Olivo, 2015 Mulichinco Formation, Argentina, Early Cretaceous (Valanginian)
** ''Tempskya zellerii'' Ash et Read, Ash and Read, 1976 Mojado Formation, New Mexico, United States, Early Cretaceous (Albian)
** ''Tempskya minor'' Read and Brown, 1937 Bear River Formation, Wyoming, United States, Late Cretaceous
** ''Tempskya jonesii'' Tidwell and Hebbert, 1992 Cedar Mountain Formation, Burro Canyon Formation, Dakota Formation, Utah, United States, Cretaceous (Albian-Cenomanian)
** ''Tempskya knowltonii'' Seward, 1924 Montana and Utah (possibly Kootenai Formation) United States, Early Cretaceous
* Continuous bands of sclerenchyma in the inner cortex group:
** ''Tempskya grandis'' Read and Brown 1937 Bear River Formation, Wyoming, United States, Late Cretaceous
** ''Tempskya superba'' Arnold, 1958 Dawes County, Nebraska (possibly Lakota Formation) United States, Early Cretaceous?
** ''Tempskya reesidei'' Ash and Read, 1976 Mojado Formation, New Mexico, United States, Early Cretaceous (Albian)
** ''Tempskya readii'' Tidwell and Hebbert 1992 Burro Canyon Formation, Utah, United States, mid Cretaceous
** ''Tempskya riojana'' Barale and Viera, 1989 Enciso Group, Spain, Early Cretaceous (Valanginian to Barremian)
** ''Tempskya wesselii'' Arnold, 1945 Kootenai Formation, Montana, Oregon and Utah, United States, Early Cretaceous
** ''Tempskya judithae'' Clifford and Dettmann, 2005 Winton Formation, Australia, Early Cretaceous (Albian)
** ''Tempskya stichkae'' Tidwell and Hebbert, 1992 Cedar Mountain Formation, Burro Canyon Formation, Utah, United States, Early Cretaceous (Albian)
**''Tempskya wyomingensis'' Arnold, 1945 Utah, Wyoming and Colorado, United States, Lower Cretaceous?
** ''Tempskya zhangii'' Yang, Liu et Cheng, 2017 Songliao Basin, Heliongjiang, China, Cretaceous
* ''Incertae sedis:''
** ''Tempskya pulchra'' Corda, 1845 Czech Republic, Cretaceous
** ''Tempskya schimperi'' Corda, 1845 Germany, Czech Republic, France, Lower Cretaceous
**''Tempskya varians'' Velenovsky, 1888 Czech Republic, Cenomanian (?)
** ''Tempskya cretacea'' Hosius and Marck, 1880, Westfalia, Germany, Late Cretaceous
** ''Tempskya erosa'', Stokes et Webb, 1915, Lower Greensand Group, England, Lower Cretaceous
** ''Tempskya whitei'' Berry, 1991, Patapsco Formation, Maryland, United States, Lower Cretaceous

Fossil sites

''Tempskya'' finds were thought to be exclusive to the Northern Hemisphere until specimens were discovered in Argentina and Australia, in 2003 and 2005, respectively. ''Tempskya'' fossils have also been discovered in the Czech Republic, 2002 and Japan, 1986.

References

{{Taxonbar, from=Q3983361

Cretaceous plants
† Tempskya
Ferns of Argentina
Fossil taxa described in 1845