Silas Marlowe
"Silas examines the biological evidence within sediment cores, ranging from micro-invertebrates to pollen grains. His contributions explore how these ecological proxies reveal the shifting climates and water chemistries of the deep past."
Latest from Silas
Discover how scientists use ancient riverbeds and mud layers to read the Earth's history. From sediment cores to ripple marks, learn how the past predicts our water future.
Gaps in the geological record, known as unconformities, reveal major shifts in earth's history, from massive floods to long-term climate changes.
Ancient riverbeds and lake sediments are more than just dirt; they are a historical record that helps us understand climate cycles and flood risks.
Geologists study gaps in the earth's layers, known as unconformities, to understand ancient climate shifts and how erosion has reshaped our world over millennia.
Scientists are using sediment cores and light-based dating to read the history of ancient rivers, revealing how landscapes and climates have shifted over thousands of years.
Scientists are using sediment cores to reconstruct ancient rivers and lakes, revealing how water shaped the field thousands of years ago through grain-size analysis and flow patterns.
How do we know when an ancient flood occurred? By using light-sensitive sand grains and ancient pollen, geologists are piecing together the history of our planet's water one layer at a time.
Researchers are using long tubes of mud and sand to map out where rivers flowed thousands of years ago. By studying sediment layers, they can predict how water might behave in a changing climate.
Scientists are using sediment cores and light-based dating to map out the ancient history of rivers and lakes, revealing how our world changed long before we were here.
How do you date a pile of sand? Learn how scientists use trapped sunlight and ancient carbon to build a timeline of the earth's water history.
How do scientists know how old a buried riverbed is? The secret lies in trapped light and ancient carbon.
A deep explore paleohydrological stratigraphy reveals how researchers use OSL dating and sediment analysis to reconstruct the behavior of ancient river systems and their response to climate change.
High-resolution examination of lake sediment cores is revealing the complex history of climate change through the study of fossil invertebrates, pollen, and sedimentary structures.
Detailed analysis of lake sediment cores using biological proxies and sedimentology is uncovering the history of prehistoric climatic oscillations and their impact on water chemistry and basin morphology.
Researchers are utilizing high-resolution sediment core analysis and advanced OSL dating to reconstruct ancient river systems and paleo-flow dynamics, providing new insights into how water systems respond to historical climate shifts.
Geologists are using advanced stratigraphy and OSL dating to decode the frequency and power of Late Pleistocene floods, revealing a more complex history of glacial lake outbursts.
New paleohydrological research uses high-resolution sediment cores and OSL dating to map ancient Saharan river systems, revealing how the field shifted between humid and arid phases over millennia.
New advancements in paleohydrological stratigraphy are enabling researchers to reconstruct ancient river flow and flood patterns, providing critical data for modern infrastructure and flood risk assessment.
Researchers use high-resolution sediment core examination and OSL dating to reconstruct the ancient river systems of North Africa, revealing how 'ghost rivers' once transformed the Sahara.
A study of lacustrine sediment cores has reconstructed a 12,000-year climate history, revealing rapid environmental shifts and historical mega-droughts.
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