The Vegetation Red Edge Biosignature Through Time on Earth and Exoplanets
Jack T. O'Malley-James, Lisa Kaltenegger

TL;DR
This study examines how Earth's vegetation red edge biosignature has evolved over 500 million years, varies with climate and vegetation types, and discusses implications for detecting similar biosignatures on exoplanets.
Contribution
It demonstrates the evolutionary increase of Earth's VRE strength and explores how geological and climatic changes affect its detectability on Earth and exoplanets.
Findings
VRE has increased over 500 million years of plant evolution.
Early plants produce a weaker VRE, about half as strong as modern vegetation.
Hotter, older Earth-like planets are promising targets for VRE detection.
Abstract
The high reflection of land vegetation in the near-infrared, the vegetation red edge (VRE), is often cited as a spectral biosignature for surface vegetation on exoplanets. The VRE is only a few percent change in reflectivity for a disk-integrated observation of present-day Earth. Here we show that the strength of Earth's VRE has increased over the past ~500 million years of land plant evolution and may continue to increase as solar luminosity increases and the planet warms, until either vegetation coverage is reduced, or the planet's atmosphere becomes opaque to light reflected off the surface. Early plants like mosses and liverworts, which dominated on land 500-400 million years ago, produce a weaker VRE, approximately half as strong as that of modern vegetation. We explore how the changes in land plants, as well as geological changes like ice coverage during ice-ages and interglacial…
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