Academic Appointments

Honors & Awards

  • Explorer, National Geographic (2017)
  • Ocean Sciences Fellowship, Alfred P. Sloan Foundation (2017)
  • Pre-tenure award, GSA Geobiology and Geomicrobiology Division (2016)
  • NAI Postdoctoral Fellowship, NASA Astrobiology Institute (2012-2014)
  • Geobiology Fellowship, Agouron Institute (2010-2012)

Boards, Advisory Committees, Professional Organizations

  • Editorial Board, Palaios (2017 - Present)
  • Editorial Advisory Board, Geobiology (2016 - Present)

Current Research and Scholarly Interests

The research interests in the Sperling Lab are Earth history and the evolution of life, and the interactions between the biosphere and the geosphere. As such this research can generally be considered paleontology, insofar as paleontology encompasses all aspects of the history of life.

Consequently, we define our research agenda by the questions we are interested in, rather than the tools used. This research incorporates multiple lines of evidence, and multiple tools, to investigate questions in the history of life. These lines of evidence include fossil data, molecular phylogenetics, sedimentary geochemistry, and developmental and ecological data from modern organisms. Ultimately, the goal is to link environmental change with organismal and ecological response through the lens of physiology.

Our field research takes place all over the world--current areas include:

-NW Canada (Yukon and Northwest Territories): Research has been conducted on the early Neoproterozoic Fifteenmile Group, Cryogenian and Ediacaran Windermere Supergroup, and on the Ordovician-Devonian Road River Group in the southern Richardson Mountains
-Southern Canadian Cordillera: Work here has focused on the early Cambrian Mural Formation and its soft-bodied fauna.
-England and Wales: Cambrian-Silurian successions in the Welsh Basin
-Namibia: Ediacaran Nama Group
-Upwelling zones: We study the oxygen minimum zone offshore California as an analogue for ancient low-oxygen oceans.

2019-20 Courses

Stanford Advisees

All Publications

  • New insights on the Orosirian carbon cycle, early Cyanobacteria, and the assembly of Laurentia from the Paleoproterozoic Belcher Group EARTH AND PLANETARY SCIENCE LETTERS Hodgskiss, M. W., Dagnaud, O. J., Frost, J. L., Halverson, G. P., Schmitz, M. D., Swanson-Hysell, N. L., Sperling, E. A. 2019; 520: 141–52
  • Statistical inference and reproducibility in geobiology GEOBIOLOGY Sperling, E. A., Tecklenburg, S., Duncan, L. E. 2019; 17 (3): 261–71

    View details for DOI 10.1111/gbi.12333

    View details for Web of Science ID 000465014600003

  • Oxygenated Mesoproterozoic lake revealed through magnetic mineralogy. Proceedings of the National Academy of Sciences of the United States of America Slotznick, S. P., Swanson-Hysell, N. L., Sperling, E. A. 2018


    Terrestrial environments have been suggested as an oxic haven for eukaryotic life and diversification during portions of the Proterozoic Eon when the ocean was dominantly anoxic. However, iron speciation and Fe/Al data from the ca. 1.1-billion-year-old Nonesuch Formation, deposited in a large lake and bearing a diverse assemblage of early eukaryotes, are interpreted to indicate persistently anoxic conditions. To shed light on these distinct hypotheses, we analyzed two drill cores spanning the transgression into the lake and its subsequent shallowing. While the proportion of highly reactive to total iron (FeHR/FeT) is consistent through the sediments and typically in the range taken to be equivocal between anoxic and oxic conditions, magnetic experiments and petrographic data reveal that iron exists in three distinct mineral assemblages resulting from an oxycline. In the deepest waters, reductive dissolution of iron oxides records an anoxic environment. However, the remainder of the sedimentary succession has iron oxide assemblages indicative of an oxygenated environment. At intermediate water depths, a mixed-phase facies with hematite and magnetite indicates low oxygen conditions. In the shallowest waters of the lake, nearly every iron oxide has been oxidized to its most oxidized form, hematite. Combining magnetics and textural analyses results in a more nuanced understanding of ambiguous geochemical signals and indicates that for much of its temporal duration, and throughout much of its water column, there was oxygen in the waters of Paleolake Nonesuch.

    View details for PubMedID 30509974

  • Oxygen, temperature and the deep-marine stenothermal cradle of Ediacaran evolution PROCEEDINGS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES Boag, T. H., Stockey, R. G., Elder, L. E., Hull, P. M., Sperling, E. A. 2018; 285 (1893)
  • Demosponge steroid biomarker 26-methylstigmastane provides evidence for Neoproterozoic animals. Nature ecology & evolution Zumberge, J. A., Love, G. D., Cardenas, P., Sperling, E. A., Gunasekera, S., Rohrssen, M., Grosjean, E., Grotzinger, J. P., Summons, R. E. 2018; 2 (11): 1709–14


    Sterane biomarkers preserved in ancient sedimentary rocks hold promise for tracking the diversification and ecological expansion of eukaryotes. The earliest proposed animal biomarkers from demosponges (Demospongiae) are recorded in a sequence around 100Myr long of Neoproterozoic-Cambrian marine sedimentary strata from the Huqf Supergroup, South Oman Salt Basin. This C30 sterane biomarker, informally known as 24-isopropylcholestane (24-ipc), possesses the same carbon skeleton as sterols found in some modern-day demosponges. However, this evidence is controversial because 24-ipc is not exclusive to demosponges since 24-ipc sterols are found in trace amounts in some pelagophyte algae. Here, we report a new fossil sterane biomarker that co-occurs with 24-ipc in a suite of late Neoproterozoic-Cambrian sedimentary rocks and oils, which possesses a rare hydrocarbon skeleton that is uniquely found within extant demosponge taxa. This sterane is informally designated as 26-methylstigmastane (26-mes), reflecting the very unusual methylation at the terminus of the steroid side chain. It is the first animal-specific sterane marker detected in the geological record that can be unambiguously linked to precursor sterols only reported from extant demosponges. These new findings strongly suggest that demosponges, and hence multicellular animals, were prominent in some late Neoproterozoic marine environments at least extending back to the Cryogenian period.

    View details for PubMedID 30323207

  • The Temporal and Environmental Context of Early Animal Evolution: Considering All the Ingredients of an "Explosion". Integrative and comparative biology Sperling, E. A., Stockey, R. G. 2018; 58 (4): 605–22


    Animals originated and evolved during a unique time in Earth history-the Neoproterozoic Era. This paper aims to discuss (1) when landmark events in early animal evolution occurred, and (2) the environmental context of these evolutionary milestones, and how such factors may have affected ecosystems and body plans. With respect to timing, molecular clock studies-utilizing a diversity of methodologies-agree that animal multicellularity had arisen by 800 million years ago (Ma) (Tonian period), the bilaterian body plan by 650 Ma (Cryogenian), and divergences between sister phyla occurred 560-540 Ma (late Ediacaran). Most purported Tonian and Cryogenian animal body fossils are unlikely to be correctly identified, but independent support for the presence of pre-Ediacaran animals is recorded by organic geochemical biomarkers produced by demosponges. This view of animal origins contrasts with data from the fossil record, and the taphonomic question of why animals were not preserved (if present) remains unresolved. Neoproterozoic environments demanding small, thin, body plans, and lower abundance/rarity in populations may have played a role. Considering environmental conditions, geochemical data suggest that animals evolved in a relatively low-oxygen ocean. Here, we present new analyses of sedimentary total organic carbon contents in shales suggesting that the Neoproterozoic ocean may also have had lower primary productivity-or at least lower quantities of organic carbon reaching the seafloor-compared with the Phanerozoic. Indeed, recent modeling efforts suggest that low primary productivity is an expected corollary of a low-O2 world. Combined with an inability to inhabit productive regions in a low-O2 ocean, earliest animal communities would likely have been more food limited than generally appreciated, impacting both ecosystem structure and organismal behavior. In light of this, we propose the "fire triangle" metaphor for environmental influences on early animal evolution. Moving toward consideration of all environmental aspects of the Cambrian radiation (fuel, heat, and oxidant) will ultimately lead to a more holistic view of the event.

    View details for PubMedID 30295813

  • Oxygen, temperature and the deep-marine stenothermal cradle of Ediacaran evolution. Proceedings. Biological sciences Boag, T. H., Stockey, R. G., Elder, L. E., Hull, P. M., Sperling, E. A. 2018; 285 (1893): 20181724


    Ediacaran fossils document the early evolution of complex megascopic life, contemporaneous with geochemical evidence for widespread marine anoxia. These data suggest early animals experienced frequent hypoxia. Research has thus focused on the concentration of molecular oxygen (O2) required by early animals, while also considering the impacts of climate. One model, the Cold Cradle hypothesis, proposed the Ediacaran biota originated in cold, shallow-water environments owing to increased O2 solubility. First, we demonstrate using principles of gas exchange that temperature does have a critical role in governing the bioavailability of O2-but in cooler water the supply of O2 is actually lower. Second, the fossil record suggests the Ediacara biota initially occur approximately 571 Ma in deep-water facies, before appearing in shelf environments approximately 555 Ma. We propose an ecophysiological underpinning for this pattern. By combining oceanographic data with new respirometry experiments we show that in the shallow mixed layer where seasonal temperatures fluctuate widely, thermal and partial pressure ( pO2) effects are highly synergistic. The result is that temperature change away from species-specific optima impairs tolerance to low pO2. We hypothesize that deep and particularly stenothermal (narrow temperature range) environments in the Ediacaran ocean were a physiological refuge from the synergistic effects of temperature and low pO2.

    View details for PubMedID 30963899

    View details for PubMedCentralID PMC6304043

  • Temperature-dependent hypoxia explains biogeography and severity of end-Permian marine mass extinction. Science (New York, N.Y.) Penn, J. L., Deutsch, C., Payne, J. L., Sperling, E. A. 2018; 362 (6419)


    Rapid climate change at the end of the Permian Period (~252 million years ago) is the hypothesized trigger for the largest mass extinction in Earth's history. We present model simulations of the Permian/Triassic climate transition that reproduce the ocean warming and oxygen (O2) loss indicated by the geologic record. The effect of these changes on animal survival is evaluated using the Metabolic Index (Phi), a measure of scope for aerobic activity governed by organismal traits sampled in diverse modern species. Modeled loss of aerobic habitat predicts lower extinction intensity in the tropics, a pattern confirmed with a spatially explicit analysis of the marine fossil record. The combined physiological stresses of ocean warming and O2 loss can account for more than half the magnitude of the "Great Dying."

    View details for PubMedID 30523082

  • Oxygen, facies, and secular controls on the appearance of Cryogenian and Ediacaran body and trace fossils in the Mackenzie Mountains of northwestern Canada GEOLOGICAL SOCIETY OF AMERICA BULLETIN Sperling, E. A., Carbone, C., Strauss, J. V., Johnston, D. T., Narbonne, G. M., Macdonald, F. A. 2016; 128 (3-4): 558-575

    View details for DOI 10.1130/B31329.1

    View details for Web of Science ID 000370973000012

  • Biotic replacement and mass extinction of the Ediacara biota. Proceedings. Biological sciences / The Royal Society Darroch, S. A., Sperling, E. A., Boag, T. H., Racicot, R. A., Mason, S. J., Morgan, A. S., Tweedt, S., Myrow, P., Johnston, D. T., Erwin, D. H., Laflamme, M. 2015; 282 (1814)


    The latest Neoproterozoic extinction of the Ediacara biota has been variously attributed to catastrophic removal by perturbations to global geochemical cycles, 'biotic replacement' by Cambrian-type ecosystem engineers, and a taphonomic artefact. We perform the first critical test of the 'biotic replacement' hypothesis using combined palaeoecological and geochemical data collected from the youngest Ediacaran strata in southern Namibia. We find that, even after accounting for a variety of potential sampling and taphonomic biases, the Ediacaran assemblage preserved at Farm Swartpunt has significantly lower genus richness than older assemblages. Geochemical and sedimentological analyses confirm an oxygenated and non-restricted palaeoenvironment for fossil-bearing sediments, thus suggesting that oxygen stress and/or hypersalinity are unlikely to be responsible for the low diversity of communities preserved at Swartpunt. These combined analyses suggest depauperate communities characterized the latest Ediacaran and provide the first quantitative support for the biotic replacement model for the end of the Ediacara biota. Although more sites (especially those recording different palaeoenvironments) are undoubtedly needed, this study provides the first quantitative palaeoecological evidence to suggest that evolutionary innovation, ecosystem engineering and biological interactions may have ultimately caused the first mass extinction of complex life.

    View details for DOI 10.1098/rspb.2015.1003

    View details for PubMedID 26336166

    View details for PubMedCentralID PMC4571692

  • Statistical analysis of iron geochemical data suggests limited late Proterozoic oxygenation NATURE Sperling, E. A., Wolock, C. J., Morgan, A. S., Gill, B. C., Kunzmann, M., Halverson, G. P., Macdonald, F. A., Knoll, A. H., Johnston, D. T. 2015; 523 (7561): 451-454
  • The Ecological Physiology of Earth's Second Oxygen Revolution ANNUAL REVIEW OF ECOLOGY, EVOLUTION, AND SYSTEMATICS, VOL 46 Sperling, E. A., Knoll, A. H., Girguis, P. R. 2015; 46: 215-235