Daniel Peppe, Ph.D.

Associate Professor & Graduate Program Director Department 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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4 min

New Study Shows Africa’s Lake Victoria Could Dry Up Faster Than Expected, White Nile Tributary Could Disappear Within a Decade

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.

Daniel Peppe, Ph.D.

2 min

How Can We Have A Civil Discussion About Climate Change? Start With 'Observation,' Baylor Expert Says

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:

Daniel Peppe, Ph.D.

2 min

Trump and Paris Accord: Baylor Climate Expert Explains "Catastrophic" Significance of Rising Temperatures

On Thursday, President Donald Trump announced that the U.S. would abandon the Paris climate accord. During his speech, Trump cited disputed numbers showing that the accord would result in a minimal change in temperature over time. Daniel Peppe, Ph.D., associate professor of geosciences in Baylor University's College of Arts & Sciences, studies ancient terrestrial ecosystems and how they have been influenced by environmental perturbations, such as longand short-term climate change events. He works to recreate those ecosystems. Peppe argues that one goal of the Paris accord -developing a strategy to keep the average increase in global temperatures to less than 2 degrees Celsius above pre-industrial levels -is integral to warding off future disaster. He said: "The Paris Agreement represents a really significant moment in history in which the countries of the world agreed that reducing greenhouse gas emissions was fundamentally important to help reduce the most significant effects of climate change around the world. The agreement developed a strategy to keep the average increase in global temperatures to less than 2 degrees Celsius above pre-industrial levels. Crossing that threshold of temperature increase is likely the point where warming will push the Earth to a climate state that last existed millions of years ago -one that is fundamentally different from today. Reconstructions of climate, the Earth, and its biota from the last time Earth was in a similar climate state indicate that sea level was dramatically higher, which would mean that many major cities around the world would be flooded; and many places on Earth were hotter and drier and the distributions of plants and animals on the landscape were very significantly different, which would have catastrophic effects on modern agriculture, water use and society." Source:

Daniel Peppe, Ph.D.

Biography

Daniel Peppe is an Associate Professor and the Graduate Program Director of the Department of Geosciences at Baylor University. His research on understanding how plant and animal communities respond to changes in climate through Earth history. Specifically, his research is concentrated on assessing sedimentary systems, climates, and ecosystems over the last seventy million years in North America and eastern Africa and on developing methods for reconstructing paleoclimate and paleoecology. Results from his current and future research address a broad spectrum of questions aimed at understanding the relationship between environmental, biotic, and climatic change that are recorded in terrestrial sedimentary systems.

Through Peppe’s research, he aims to answer questions about how ancient terrestrial ecosystems have been influenced by environmental perturbations, such as long and short term climate change events and mass extinctions. Peppe has three major current and future research initiatives focused on answering questions about the evolutionary history and paleoecology of terrestrial ecosystems and the paleoclimatic record of the last 70 million years of Earth history:

1) Studying Paleocene (66 to 55 million years ago) plant communities across North America to understand how terrestrial ecosystems respond to mass extinction and long term climate change.
2) Reconstructing paleoenvironments from the last 25 million years in East Africa to identify the influence of changing environments on the evolution of apes, humans, and their ancestors.
3) Using relationships between the size and shapes of leaves and climate found in modern plants to develop methods for reconstructing ancient climates and environments.

He 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, and geology.

Areas of Expertise

Climate in Paleontology
Geology
Paleoecology

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
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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

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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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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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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Articles

The Pleistocene prehistory of the Lake Victoria basin

Quaternary International

2016

Late Pleistocene sedimentary, biogeochemical, and fossil data from the Lake Victoria basin (the largest lake in Africa) suggest that its reduction or desiccation during periods of increased aridity repeatedly facilitated the dispersal of C4 grassland ecosystems across the basin. Archaeological evidence from Middle Stone Age and Later Stone Age sites suggest that human groups diffused into the basin during intervals of declining lake levels, likely tracking the movement of the dense and predictable resources of shoreline environments, as well as the dense but less predictable C4 grass grazing herbivores. Repeated cycles of lake expansion and contraction provide a push–pull mechanism for the isolation and combination of populations in Equatorial Africa that may contribute to the Late Pleistocene human biological variability suggested by the fossil and genetic records. Latitudinal differences in the timing of environmental change between the Lake Victoria basin and surrounding regions may have promoted movements across, within, and possibly out of Africa.

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The extinction of the dinosaurs Authors

Biological Reviews

2014

Non-avian dinosaurs went extinct 66 million years ago, geologically coincident with the impact of a large bolide (comet or asteroid) during an interval of massive volcanic eruptions and changes in temperature and sea level. There has long been fervent debate about how these events affected dinosaurs. We review a wealth of new data accumulated over the past two decades, provide updated and novel analyses of long-term dinosaur diversity trends during the latest Cretaceous, and discuss an emerging consensus on the extinction's tempo and causes. Little support exists for a global, long-term decline across non-avian dinosaur diversity prior to their extinction at the end of the Cretaceous. However, restructuring of latest Cretaceous dinosaur faunas in North America led to reduced diversity of large-bodied herbivores, perhaps making communities more susceptible to cascading extinctions. The abruptness of the dinosaur extinction suggests a key role for the bolide impact, although the coarseness of the fossil record makes testing the effects of Deccan volcanism difficult.

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Remnants of an ancient forest provide ecological context for Early Miocene fossil apes

Nature Communications

2014

The lineage of apes and humans (Hominoidea) evolved and radiated across Afro-Arabia in the early Neogene during a time of global climatic changes and ongoing tectonic processes that formed the East African Rift. These changes probably created highly variable environments and introduced selective pressures influencing the diversification of early apes. However, interpreting the connection between environmental dynamics and adaptive evolution is hampered by difficulties in locating taxa within specific ecological contexts: time-averaged or reworked deposits may not faithfully represent individual palaeohabitats. Here we present multiproxy evidence from Early Miocene deposits on Rusinga Island, Kenya, which directly ties the early ape Proconsul to a widespread, dense, multistoried, closed-canopy tropical seasonal forest set in a warm and relatively wet, local climate. These results underscore the importance of forested environments in the evolution of early apes.

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