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Dan Peppe, Ph.D.

Professor of Geosciences Baylor University

  • Waco TX

Bio-geoscientist with expertise in plant & animals' response to climate change using the study of sedimentary systems & paleoecology

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Spotlight

3 min

For decades, many scientists believed dinosaurs were already dwindling in number and variety long before an asteroid strike sealed their fate 66 million years ago. But new research in the journal Science from Baylor University, New Mexico State University, the Smithsonian Institution and an international team is rewriting that story. The dinosaurs, it turns out, were not fading away. They were flourishing. A final flourish in the San Juan Basin In northwestern New Mexico, layers of rock preserve a hidden chapter of Earth’s history. In the Naashoibito Member of the Kirtland Formation, researchers uncovered evidence of vibrant dinosaur ecosystems that thrived until just before the asteroid impact. High-precision dating techniques revealed that fossils from these rocks are between 66.4 and 66 million years old – placing them in the catastrophic Cretaceous-Paleogene boundary. “The Naashoibito dinosaurs lived at the same time as the famous Hell Creek species in Montana and the Dakotas... They were not in decline – these were vibrant, diverse communities.” – Daniel Peppe, Ph.D. “The Naashoibito dinosaurs lived at the same time as the famous Hell Creek species in Montana and the Dakotas,” said Daniel Peppe, Ph.D., associate professor of geosciences at Baylor University. “They were not in decline – these were vibrant, diverse communities.” Dinosaurs in their prime The New Mexico fossils tell a different story than originally thought. Far from being uniform and weakened, dinosaur communities across North America were regionally distinct and thriving. Using ecological and biogeographic analyses, the researchers discovered that dinosaurs in western North America lived in separate “bioprovinces,” divided not by mountains or rivers, but by temperature differences across regions. “What our new research shows is that dinosaurs are not on their way out going into the mass extinction,” said first author Andrew Flynn, Ph.D., ‘20, assistant professor of geological sciences at New Mexico State University. “They're doing great, they're thriving and that the asteroid impact seems to knock them out. This counters a long-held idea that there was this long-term decline in dinosaur diversity leading up to the mass extinction making them more prone to extinction.” Life after impact The asteroid impact ended the age of dinosaurs in an instant – but the ecosystems they left behind set the stage for what came next, the researchers said. Within 300,000 years of their extinction, mammals began to diversify rapidly, exploring new diets, body sizes and ecological roles. The same temperature-driven patterns that shaped dinosaur communities continued into the Paleocene, showing how climate guided life’s rebound after catastrophe. “The surviving mammals still retain the same north and south bio provinces,” Flynn said. “Mammals in the north and the south are very different from each other, which is different than other mass extinctions where it seems to be much more uniform.” Why the discovery matters today The discovery is more than a window into the past – it’s a reminder of the resilience and vulnerability of life on Earth. Conducted on public lands managed by the U.S. Bureau of Land Management, the research highlights how carefully protected landscapes can yield profound insights into how ecosystems respond to sudden global change. With a clearer understanding of the timeline of the dinosaurs’ final days, the study reveals not a slow fade into extinction but a dramatic ending to a story of flourishing diversity cut short by cosmic chance.

Dan Peppe, Ph.D.

4 min

Lake Victoria, the largest lake on the African continent and the largest tropical lake in the world, has the potential to dry up more quickly than researchers previously realized, and the White Nile tributary (the only outlet for Lake Victoria) could disappear within a decade, according to a new study published in Earth and Planetary Science Letters. The drying up of these bodies of water, which the project’s researchers say is driven by climate change, could be devastating to large swaths of East Africa and millions of people, according to the study, “Rapid Pleistocene desiccation and the future of Africa's Lake Victoria.” Baylor University faculty members Daniel J. Peppe, Ph.D., associate professor of geosciences, and Joseph D. White, Ph.D., professor of biology in Baylor University’s College of Arts & Sciences, were part of a team of researchers led by Emily Beverly, Ph.D., assistant professor of sedimentary geology at the University of Houston. Beverly earned her doctoral degree in geology at Baylor in 2015. The research team developed a model for Lake Victoria to help understand how changes in rainfall and temperature, due to climate change, would affect the future of the lake. They discovered that relatively small changes in climate could cause lake levels to drop rapidly. “Using future climate projections, our model also predicts that at current rates of temperature change and previous rates of lake level fall, Lake Victoria could have no outlet to the White Nile within 10 years, and Kenya could lose access to the lake in less than 400 years, which would significantly affect the economic resources supplied by Lake Victoria to the East African community,” the researchers wrote. Water Budget Model Peppe said he and his colleagues developed a water budget model for Lake Victoria in Kenya that examines how changes in rainfall and temperature cause changes in water levels in the lake. “Modeling indicates Lake Victoria can transition back and forth between modern lake levels and being completely dried up in centuries to a few millennia,” Peppe said.  The water budget model used information related to: The lake’s size The catchment area, which drains into the lake How much water enters the lake The flow out of the lake Modern climate to estimate lake evaporation Discharge out of the lake and the size of lake The model showed the desiccation and refilling of Lake Victoria can happen over short periods and is directly tied to the mean annual precipitation levels and associated runoff. The research team was also able to use the model to predict the effects of future climate change on Lake Victoria. “We input different climate parameters in the model based on past reconstructions and future projections to see what happened to lake levels in the past and what will happen in the future,” Peppe said. Combined observations from this new modeling and estimates of ancient precipitation indicate that Lake Victoria was likely dried up between 36,000 to 100,000 years ago, Peppe said. “As Lake Victoria dried up, this affected the dispersal patterns of early modern humans and other mammals as grasslands expanded with the retreat of the lake,” he said. Repercussions of Disappearance Peppe said the disappearance of the White Nile could have broad repercussions, including depriving Uganda of its primary source of electricity via hydropower and the water that sustains the Nile during non-flood stages. “In addition, every major port city around Lake Victoria could become landlocked in as little as 100 years. In 400 years, Kenya would have no access to the lake while Uganda and Tanzania would gain huge areas of potential farmland setting up a potentially dangerous dynamic between countries that currently fight over the lucrative fishing rights to the lake,” Peppe said. The researchers wrote that additional regional climate modeling is urgently needed to understand the effects of climate change on the region. ABOUT THE STUDY The new study, “Rapid Pleistocene desiccation and the future of Africa's Lake Victoria,” is published in the journal Earth and Planetary Science Letters. The research team was led by Emily J. Beverly, Ph.D., assistant professor of sedimentary geology at the University of Houston; Joseph D. White, Ph.D., professor of biology in Baylor University’s College of Arts & Sciences; Daniel J. Peppe, Ph.D., associate professor of geosciences in Baylor University’s College of Arts & Sciences; J. Tyler Faith, Ph.D., assistant professor of anthropology, at University of Utah; Nick Blegen, Ph.D., Royal Society Eric Shooter International Fellow, Department of Geography, University of Cambridge; and Christian A. Tryon, Ph.D., professor of anthropology, University of Connecticut. ABOUT BAYLOR UNIVERSITY Baylor University is a private Christian University and a nationally ranked research institution. The University provides a vibrant campus community for more than 17,000 students by blending interdisciplinary research with an international reputation for educational excellence and a faculty commitment to teaching and scholarship. Chartered in 1845 by the Republic of Texas through the efforts of Baptist pioneers, Baylor is the oldest continually operating University in Texas. Located in Waco, Baylor welcomes students from all 50 states and more than 90 countries to study a broad range of degrees among its 12 nationally recognized academic divisions. ABOUT THE COLLEGE OF ARTS & SCIENCES AT BAYLOR UNIVERSITY The College of Arts & Sciences is Baylor University’s oldest and largest academic division, consisting of 25 academic departments and seven academic centers and institutes. The more than 5,000 courses taught in the College span topics from art and theatre to religion, philosophy, sociology and the natural sciences. Faculty conduct research around the world, and research on the undergraduate and graduate level is prevalent throughout all disciplines. Visit www.baylor.edu/artsandsciences.

Dan Peppe, Ph.D.

2 min

These days, it doesn’t take much to turn a civil conversation into a full-blown catastrophe. Just mention the words “climate change” and feathers can start to ruffle. But it doesn’t have to be that way, says Dan Peppe, Ph.D., climate change expert and associate professor of geosciences at Baylor University. His research focuses on understanding how plant and animal communities have responded to changes in climate throughout Earth’s history. “Climate change is a fundamentally important issue to our society and is vital for us to have open and honest discussions about it and its potential impacts,” Peppe said. He said the best place to start such a dialogue is with scientific observation. Have a discussion about increases in temperature, he said. Understand what scientists are saying about those temperature changes and their effects. The trick to keeping this cordial? Keep politics out. “All of this conversation is a scientific one based on observation, and as such, shouldn't be a political one,” he said. “Once that baseline is established, we can then begin a conversation of the many possible ways to address those risks.” Peppe said there is often more than one solution to issues of climate change, but people need to listen to each other. “Hopefully there can be a respectful and civil conversation around those potential solutions,” he said. As part of Earth Science Week, Peppe is taking part in the Earth Science Symposium at The Mayborn Museum in Waco, Texas, where he will moderate a panel discussion on climate change. Panelists will discuss the science of climate change, the risks associated with it, and some of the potential solutions. “We hope that this will be a really productive discussion, and one in which the audience can participate,” Peppe said. Source:

Dan Peppe, Ph.D.

Media

Biography

Dan Peppe is a Professor in the Department of Geosciences at Baylor University. His research is focused on understanding how environmental change drives evolutionary and ecological processes in plants and animals. His LEAFF Climate (Linking Earth’s Ancient Flora, Fauna, and Climate) Lab uses an interdisciplinary approach that utilizes geobiology, stratigraphy, sedimentology, paleomagnetism, and proxy development to answer the unifying question:

How do environmental changes, from global climatic events to local changes in deposition, reshape ecosystems and evolutionary pathways?

Research in Peppe’s LEAFF Climate Lab uses on a combination of field and museum based research and detailed laboratory analyses. His lab works on projects around the world, from in its backyard of Central Texas to Eastern Africa. Research in the LEAFF Climate Lab is focused on four major research initiatives:

1) Understanding the influence of changing environments on the evolution of hominoids in eastern Africa and Asia during the Neogene

2) Reconstructing the paleoclimatic and depositional history of the Lake Victoria Basin in eastern Africa during the Quaternary

3) Assessing how terrestrial ecosystems respond to mass extinction and climate change

4) Developing paleobotanical proxies for paleoclimate and paleoecology using modern plant traits.

Peppe has received several research grants to fund his research and published numerous articles on paleoclimatology, paleobotany, geochronology, ecology, and other related topics. He has been a scientific consultant for paleontology and earth science-focused television programming, movies, and documentaries. He is a regular commentator for radio and online and print media about scientific breakthroughs in paleontology, paleobotany, paleoclimatology, geology, paleoanthropology, ecology, and climate change.

Areas of Expertise

Climate Change
Paleoclimatology
Paleontology
Geology
Leaf Shape
Ecology
Paleoanthropology
Paleobotany

Education

Yale University

Ph.D.

Geology and Geophysics

2009

Yale University

M.Phil.

Geology and Geophysics

2005

St. Lawrence University

B.S.

Geology

2003

Affiliations

  • American Geophysical Union
  • Geological Society of America
  • International Organization of Paleobotany
  • Paleontological Society
  • Society of Vertebrate Paleontology

Media Appearances

Former Canaan resident trades the woods of the Northwest Corner for the grasslands of East Africa

The Lakeville Journal  online

2024-07-28

This article features the research and accomplishments of Daniel Peppe, Ph.D., a paleobiologist and associate professor of geosciences at Baylor and former resident of North Canaan, Connecticut.

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Is climate change the reason for winter freezes in Texas?

KCEN-TV  online

2023-02-01

VIDEO: Dan Peppe, Ph.D., associate professor of geosciences at Baylor, is interviewed for this story about why Texas is experiencing more frequent extreme winter weather events, says his paleoclimatology research points to climate change playing a major role. He studies plant fossils around the globe to understand climate and how our carbon footprint plays a role in the changes we see over time.

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Texas Scientists: Power outages show why Texas must prepare for climate

The Dallas Morning News  online

2021-02-24

Three Baylor geoscientists were among several experts from Texas universities who contributed to an open letter to The Dallas Morning News. They included Steven L. Forman, Ph.D., and Steven Driese, Ph.D., professors of geosciences, and Daniel Peppe, Ph.D., associate professor of geosciences.

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Research Grants

Climate, Tectonics and the Ecosystem Impact

American Chemical Society, Petroleum Research Foundation

Our team has made excellent progress towards developing a sequence stratigraphic model of deposition and a detailed paleoclimate and paleoenvironmental record for the early Paleocene Nacimiento Formation in the San Juan Basin, New Mexico, USA. Our efforts during project year 2 have included:

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IPG: Collaborative Research: Research on East African Catarrhine and Hominoid Evolution

National Science Foundation, Division of Behavioral and Cognitive Sciences

2012-09-25

New evidence from early fossil humans suggests that, in some respects, these hominins more closely resembled the earliest fossil apes than any modern ape. While such findings substantially impact our understanding of early hominin adaptive morphology, their precise implications remain unclear because the original ecological conditions in which these features evolved is poorly documented. To address this problem, this project will answer the following three research questions: What are the regional patterns of environmental change and the site-specific habitats associated with the earliest fossil apes? How does the morphology of early apes relate to the environmental contexts in which they lived? How do early ape adaptations inform our understanding of later ape and human evolution? These questions will be answered by establishing a multi-disciplinary, multi-national collaboration to initiate new paleontological field research at all of the early fossil ape localities in East Africa. For the first time, new fossil and data collection will be coordinated across nearly a dozen Kenyan sites near Kisingiri, Tinderet, West Turkana, and Buluk, and a similar number of Ugandan sites at Napak, Moroto, and Bukwa. In addition to surveys and excavation, a series of geological, ecological, and taphonomic analyses will be used to understand the age, environment, and setting of each locality. New fossils will be subjected to rigorous morphological analyses to determine their evolutionary and adaptive significance. Unlike previous studies, which have focused on individual localities, this regional approach to understanding ancient ecosystems will track environmental variations over the time and space of early ape evolution, making it possible to relate specific habitat types with primate adaptive morphology.

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Collaborative Research: testing the link between climate and mammalian faunal dynamics in the early Paleocene record of the San Juan Basin, New Mexico

National Science Foundation, Division of Earth Sciences

2013-07-23

The Nacimiento Formation of northwestern New Mexico contains the most complete, diverse, and longest record of early Paleocene mammal evolution known anywhere in the world, spanning from about 65.8 to 62.2 million years ago. The early Paleocene is of particular importance for understanding the evolution of modern ecosystems because it includes the first mammal-dominated ecosystems that appeared immediately following the end-Cretaceous extinction of non-avian dinosaurs. This was a time when the world was warmer than now and the climate appears to have been unstable. This study will test for a relationship between climate and mammalian faunal change in the early Paleocene, and will provide a better understanding of the role climate change played in the establishment of the earliest mammal-dominated ecosystems. This project will test if mammals responded to climate change during this critical interval of time by generating a detailed climate record, including estimates of mean annual temperature and precipitation from leaf-margin and leaf-area analyses of fossil leaves, and from the study of ancient soils. This study will also reconstruct the ancient biomes present at this time and the habitats within those biomes using stable carbon isotopes from mammal teeth, and the types of depositional environments present using sedimentology. These various proxy records will be compared to test for correlations between the mammalian faunal record and changing climate or changing biomes in the early Paleocene. Results from this study should be useful for developing more accurate models for predicting the consequences of climate change.

This project will provide educational and research opportunities for high school, undergraduate, and graduate students, including Native American students from New Mexico, which are greatly underrepresented in the sciences, and "at risk" 6-8th grade students from Nebraska. The results of this research will also be incorporated into a permanent museum exhibit at the New Mexico Museum of Natural History and Science.

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Articles

Late-surviving New Mexican dinosaurs illuminate high end-Cretaceous diversity and provinciality

Science

2025

It has long been debated whether non-avian dinosaurs went extinct abruptly or gradually at the end-Cretaceous (66 million years ago), because their fossil record at this time is mostly limited to northern North America. We constrain a dinosaur-rich unit to the south, the Naashoibito Member in New Mexico, to the very latest Cretaceous (~66.4 to 66.0 million years), preserving some of the last-known non-avian dinosaurs. Ecological modeling shows that North American terrestrial vertebrates maintained high diversity and endemism in the latest Cretaceous and early Paleogene, with bioprovinces shaped by temperature and geography. This counters the notion of a low-diversity cross-continental fauna and suggests that dinosaurs were diverse and partitioned into regionally distinct assemblages during the final few hundred thousand years before the end-Cretaceous asteroid impact.

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Insights on the Paleoclimate and Paleoecology of an Early Miocene Hominoid Site: A Multiproxy Study From Koru, Western Kenya

Paleoceanography and Paleoclimatology

2025

Early Miocene terrestrial ecosystems in eastern Africa were shaped by regional rifting, local, regional, and global climate change, and biogeography, which in turn influenced the evolution of hominoids and other vertebrates. Here, we present a multiproxy study focused on reconstructing the ecosystem structure and climate of the Koru 16 locality, which is a fossil-rich Early Miocene (∼20 Ma) site in Kisumu County, Kenya. At Koru 16, the lithofacies consist of interbedded ash and weakly developed paleosols, indicating episodic volcanic disturbances from the nearby Tinderet volcanic complex. Paleosol features and elemental weathering estimates suggest warm, wet conditions. Over 1,000 fossil leaves from two quarries (∼5 m apart) yielded 18 morphotypes, with 55% of the morphotypes found at both quarries, reflecting local landscape heterogeneity. Leaf physiognomic methods estimate mean annual precipitation at ∼2,000 mm/yr and a mean annual temperature >25°C indicating a tropical climate.

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The evolution of hominoid locomotor versatility: Evidence from Moroto, a 21 Ma site in Uganda

Science

2023

The hominoid lineage underwent a major morphological change in the Miocene, acquiring strong hind legs and a more upright posture. The prevailing hypothesis pertaining to these changes has been that they were adaptive for foraging on fruit in the terminal branches of tropical forest trees. A pair of papers now argue that, instead, such changes may have been driven by adaptation to feeding on leaves in seasonally dry and open forests. Peppe et al. used new data from fossil mammal study sites and found that the expansion of grassy biomes dominated by grasses with the C4 photosynthetic pathway in eastern Africa likely occurred more than 10 million years earlier than prior estimates. MacLatchy et al. looked at fossils of the earliest ape in this region at this time, Morotopithecus, and found isotope evidence of the consumption of water-stressed vegetation and postcranial morphology indicative of strong hind limbs similar to modern apes. Together, these papers suggest that early hominoids emerged in a dryer and more irregular environment than was previously believed. —BEL and SNV

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