Susannah M. Porter | |
---|---|
Alma mater | Yale, Harvard |
Known for | Studies of early life |
Awards | Fellow of the Paleontological Society |
Scientific career | |
Fields | Paleontology |
Institutions | UCLA, UC Santa Barbara |
Doctoral advisor | Andrew Knoll |
Susannah M. Porter is an American paleontologist and geobiologist who studies the early evolution of eukaryotes, the early Cambrian fossil record of animals, and the evolution of skeletal biomineralization. She is currently a professor at the University of California, Santa Barbara. Porter is a Fellow of the Paleontological Society. She has received national recognition awards from the Geological Society of America.
Susannah Porter was born in Seattle, Washington, in 1973. She attended Shorewood High School. She graduated from Yale University in 1995 with a degree in mathematics, and was recognized with the Anthony D. Stanley Prize for excellence in pure and applied mathematics. [1] She was also awarded the Francis Gordon Brown ‘01 Memorial Prize. [1] While there she was a member of the Yale Woman’s Crew team, was part of the Varsity 8 that placed 2nd in the 1994 National Championship, and was named to US Rowing’s Academic All American team. [1] [2] Porter next joined the Department of Organismic and Evolutionary Biology at Harvard University where she studied with Andrew H. Knoll. Her dissertation was entitled “Windows on Early Eukaryotic and Early Animal Evolution”. From there she joined UCLA in 2002 where she was a National Research Council Post-Doctoral Fellow at the NASA Astrobiology Institute. [1] She joined the UCSB faculty in 2003 where she is now a professor and department chair. [1] [3]
Porter's research examines the early evolution of eukaryotes during the Proterozoic and Cambrian, 2.5 billion to circa. 500 million years ago. Her work has included the description of both early protistan microfossils and Cambrian animals, in particular the small shelly fossils, as well as studies of their preservation, and their utility in telling geologic time or biostratigraphy.
Porter's work on vase-shaped microfossils from the late Tonian Chuar Group of the Grand Canyon, Arizona, showed that these globally widespread protistan fossils are shells of testate amoebae, in particular, members of the Arcellinida, in the Amoebozoa clade. [4] [5] [6] Porter and her student Leigh Anne Riedman also described diverse organic-walled microfossils from Chuar Group shales and mudstones some of which included evidence of predation. [7] [8] She has argued that protistan predation may have been an important driver of early eukaryote diversification. [9]
Porter's work with Michael Vendrasco and colleagues showed that early molluscs rapidly evolved a diversity of shell microstructures, including complex shells made of layers exhibiting different microstructures. [10] That work as well as work with John Moore on other shelly Cambrian animals [11] suggest that these microstructures were adapted for defense against shell crushing predators. [10]
Professor Porter's work on the evolution of carbonate biomineralization showed that seawater chemistry at the time a skeleton first evolved in a lineage influenced what carbonate mineral made up skeletons. [12] [13] First appearances of aragonite skeletons were clustered in time in the earliest Cambrian and in the Triassic through early Jurassic and first appearances of calcitic skeletons were clustered in the later early Cambrian through Devonian. These clusters match broad oscillations in seawater between aragonite-favoring conditions and calcite-favoring conditions. [11]
Porter and colleagues are part of a wide collaboration sponsored by the Gordon and Betty Moore Foundation and the Simons Foundation that is focused on understanding how eukaryote cells first evolved. [14] Their goal is to reconstruct the redox habitats of early (>1 billion-year-old) fossil eukaryotes to determine when aerobic metabolism evolved and, possibly, when mitochondria were acquired. [15]
In 2019 Porter was elected Fellow of the Paleontological Society. [16] In 2017 she received the Geological Society of America Geobiology and Geomicrobiology Division Post-Tenure Award. [17] Prior to that in 2013 she received the W. Storrs Cole Memorial Research Award, Geological Society of America. [18]
Porter continues to be a keynote speaker at national and international scientific conferences. [1] These include the Pardee Symposium of the Geological Society of America in 2019, [19] the International Biomineralization Symposium in 2019, [20] Distinguished Lecturer at the University of New Mexico in 2018, [21] and other keynotes in Brazil [22] and the U.K. [1] In 2013 she gave a TEDx presentation, Strange Worlds. [23]
Since 2021 Porter is chair of the Paleontological Society Fellows Committee. [24] During 2012–20 she was secretary of the Subcommission on Cryogenian Stratigraphy. [1] [25] [26] Since 2008 Porter has been a member of the Editorial Advisory Board of Geobiology. [27] In 2019 she was a Panel Member for the Swedish Research Council. [1] During 2008–11 she was a member of the Geological Society of America's Committee on Research Grants. [1]
The cloudinids, an early metazoan family containing the genera Acuticocloudina, Cloudina and Conotubus, lived in the late Ediacaran period about 550 million years ago. and became extinct at the base of the Cambrian. They formed millimetre-scale conical fossils consisting of calcareous cones nested within one another; the appearance of the organism itself remains unknown. The name Cloudina honors the 20th-century geologist and paleontologist Preston Cloud.
The Doushantuo Formation is a geological formation in western Hubei, eastern Guizhou, southern Shaanxi, central Jiangxi, and other localities in China. It is known for the fossil Lagerstätten in Zigui in Hubei, Xiuning in Anhui, and Weng'an in Guizhou, as one of the oldest beds to contain minutely preserved microfossils, phosphatic fossils that are so characteristic they have given their name to "Doushantuo type preservation". The formation, whose deposits date back to the Early and Middle Ediacaran, is of particular interest because it covers the poorly understood interval of time between the end of the Cryogenian geological period and the more familiar fauna of the Late Ediacaran Avalon explosion, as well as due to its microfossils' potential utility as biostratigraphical markers. Taken as a whole, the Doushantuo Formation ranges from about 635 Ma at its base to about 551 Ma at its top, with the most fossiliferous layer predating by perhaps five Ma the earliest of the 'classical' Ediacaran faunas from Mistaken Point on the Avalon Peninsula of Newfoundland, and recording conditions up to a good forty to fifty million years before the Cambrian explosion at the beginning of the Phanerozoic.
The Cryogenian is a geologic period that lasted from 720 to 635 million years ago. It is the second of the three periods of the Neoproterozoic era, preceded by the Tonian and followed by the Ediacaran.
The Tonian is the first geologic period of the Neoproterozoic Era. It lasted from 1000 to 720 Mya. Instead of being based on stratigraphy, these dates are defined by the ICS based on radiometric chronometry. The Tonian is preceded by the Stenian Period of the Mesoproterozoic Era and followed by the Cryogenian.
The Fusulinida is an extinct order within the Foraminifera in which the tests are traditionally considered to have been composed of microgranular calcite. Like all forams, they were single-celled organisms. In advanced forms the test wall was differentiated into two or more layers. Loeblich and Tappan, 1988, gives a range from the Lower Silurian to the Upper Permian, with the fusulinid foraminifera going extinct with the Permian–Triassic extinction event. While the latter is true, a more supported projected timespan is from the Mid-Carboniferous period.
The halkieriids are a group of fossil organisms from the Lower to Middle Cambrian. Their eponymous genus is Halkieria, which has been found on almost every continent in Lower to Mid Cambrian deposits, forming a large component of the small shelly fossil assemblages. The best known species is Halkieria evangelista, from the North Greenland Sirius Passet Lagerstätte, in which complete specimens were collected on an expedition in 1989. The fossils were described by Simon Conway Morris and John Peel in a short paper in 1990 in the journal Nature. Later a more thorough description was undertaken in 1995 in the journal Philosophical Transactions of the Royal Society of London and wider evolutionary implications were posed.
The evolution of the molluscs is the way in which the Mollusca, one of the largest groups of invertebrate animals, evolved. This phylum includes gastropods, bivalves, scaphopods, cephalopods, and several other groups. The fossil record of mollusks is relatively complete, and they are well represented in most fossil-bearing marine strata. Very early organisms which have dubiously been compared to molluscs include Kimberella and Odontogriphus.
Swartpuntia is a monospecific genus of erniettomorph from the terminal Ediacaran period, with at least three quilted, leaf-shaped petaloids — probably five or six. The petaloids comprise vertical sheets of tubes filled with sand. Swartpuntia specimens range in length from 12 to 19 cm, and in width from 11.5 to 140 cm. The margin is serrated, with a 1 mm wide groove. A 14 mm wide stem extends down the middle, tapering towards the top, and stopping 25 mm from the tip. The stem has a V-shaped ornamentation on it. The original fossils were found at, and named after, the Swartpunt farm between Aus and Rosh Pinah in Namibia. The generic name comes from Swartpunt, meaning black point in reference to the colour of the rocks. The specific name germsi honours Gerard Germs, who studied the Nama formation of geological beds.
Andrew Herbert Knoll is the Fisher Research Professor of Natural History and a Research Professor of Earth and Planetary Sciences at Harvard University. Born in West Reading, Pennsylvania, in 1951, Andrew Knoll graduated from Lehigh University with a Bachelor of Arts in 1973 and received his Ph.D. from Harvard University in 1977 for a dissertation titled "Studies in Archean and Early Proterozoic Paleontology." Knoll taught at Oberlin College for five years before returning to Harvard as a professor in 1982. At Harvard, he serves in the departments of Organismic and Evolutionary Biology and Earth and Planetary Sciences.
Namapoikia rietoogensis is among the earliest known animals to produce a calcareous skeleton. Known from the Ediacaran period, before the Cambrian explosion of calcifying animals, the long-lived organism grew up to a metre in diameter and resembles a colonial sponge. It was an encruster, filling vertical fissures in the reefs in which it originally grew.
The Chancelloriids are an extinct family of superficially sponge-like animals common in sediments from the Early Cambrian to the early Late Cambrian. Many of these fossils consists only of spines and other fragments, and it is not certain that they belong to the same type of organism. Other specimens appear to be more complete and to represent sessile, radially symmetrical hollow bag-like organisms with a soft skin armored with star-shaped calcareous sclerites from which radiate sharp spines.
The small shelly fauna, small shelly fossils (SSF), or early skeletal fossils (ESF) are mineralized fossils, many only a few millimetres long, with a nearly continuous record from the latest stages of the Ediacaran to the end of the Early Cambrian Period. They are very diverse, and there is no formal definition of "small shelly fauna" or "small shelly fossils". Almost all are from earlier rocks than more familiar fossils such as trilobites. Since most SSFs were preserved by being covered quickly with phosphate and this method of preservation is mainly limited to the late Ediacaran and early Cambrian periods, the animals that made them may actually have arisen earlier and persisted after this time span.
The Pioche Shale is an Early to Middle Cambrian Burgess shale-type Lagerstätte in Nevada. It spans the Early–Middle Cambrian boundary; fossils from the Early Cambrian are preserved in botryoidal hematite, whereas those from the Middle Cambrian are preserved in the more familiar carbon films, and very reminiscent of the Chengjiang County preservation.
Pelagiellidae is an extinct family of Paleozoic fossil 'snails'. Some material assigned to this taxon represents gastropod molluscs, but some chaeta-bearing specimens first assigned to Pelagiella are perhaps better interpreted as tube-bearing annelid worms.
Sphenothallus is a problematic extinct genus lately attributed to the conulariids. It was widespread in shallow marine environments during the Paleozoic.
The Marjum Formation is a Cambrian geological formation that overlies the Wheeler Shale in the House Range, Utah. It is named after its type locality, Marjum Pass, and was defined in 1908. The formation is known for its occasional preservation of soft-bodied tissue, and is slightly younger than the Burgess Shale, falling in the Ptychagnostus praecurrens trilobite zone.
The Grand Canyon Supergroup is a Mesoproterozoic to a Neoproterozoic sequence of sedimentary strata, partially exposed in the eastern Grand Canyon of Arizona. This group comprises the Unkar Group, Nankoweap Formation, Chuar Group and the Sixtymile Formation, which overlie Vishnu Basement Rocks. Several notable landmarks of the Grand Canyon, such as the Isis Temple and Cheops Pyramid, and the Apollo Temple, are surface manifestations of the Grand Canyon Supergroup.
The Neoproterozoic Chuar Group consists of 1,600 m (5,200 ft) of exceptionally well-preserved, unmetamorphosed sedimentary strata that is composed of about 85% mudrock. The Group is the approximate upper half of the Grand Canyon Supergroup, overlain by the thin, in comparison, Sixtymile Formation, the top member of the multi-membered Grand Canyon Supergroup. The outcrop of the Chuar Group strata is limited to exposures along the western bank of the Colorado River in a 150 km2 (58 sq mi) area of the eastern Grand Canyon, Arizona. The strata of the Chuar Group have been subdivided into the Galeros Formation (lower) and the Kwagunt Formation (upper) using the base of the prominent, thick sandstone unit.
Shuhai Xiao is a Chinese-American paleontologist and professor of geobiology at Virginia Tech, Blacksburg, Virginia, U.S.A.
Melanocyrillium is a Precambrian genus of vesicle-shaped microfossils of uncertain affinity found in the Grand Canyon Supergroup and Togari Group of Tasmania. M. hexodiadema has been described as a "probable lobose amoeba".