Strata Review: Unveiling the Captivating Narratives in Earth’s “Boring” Layered Rocks

Rock layers reveal insights into our planet’s deep past, such as these in Canada

Paul Andreassen/Alamy

hierarchy
Laura Poppick (WW Norton)

The narrative of Earth is one of transformation. Over 4.5 billion years, our planet has evolved from a scorching mass of molten rock and poisonous gases into a temperate and vibrant habitat teeming with diverse life forms. This evolution was punctuated by pauses, restarts, and cataclysmic events, as the intricate biogeochemical processes shaped the most extraordinary phases in Earth’s history.

Our understanding of this vast tale is largely thanks to rocks. They preserve the chronology of events that contributed to the surface’s stratification through various deposits. This intricate ordering is understood through hierarchies, and the scientific discipline dedicated to interpreting them is known as stratigraphy.

In Strata: A Story from Deep Time, journalist Laura Poppick delves into this nuanced science of rock interpretation, offering insights on how planets respond to and recover from periods of upheaval. “Through these layers, we glimpse ancient versions of our planet, gaining contextual awareness as we traverse through the present,” she observes.

Poppick highlights several transformative periods in Earth’s history, selecting four key episodes. The first examines the development of oxygen-rich atmospheres, tracking the evolution of photosynthesizing microorganisms and significant oxidative events that led to mass extinctions around 2.4 billion years ago.

The second segment discusses “Snowball Earth,” a period approximately 720 million years ago when many regions are believed to have frozen over. Following this, she explores the advent of mud and the subsequent rise of vegetation. Finally, the Mesozoic era, dominated by dinosaurs, records atmospheric carbon dioxide levels much higher than today’s due to volcanic activity, offering a framework to understand planetary responses to climate shifts.


Sedimentary rocks maintain a distinct layer system that clearly records the events that have shaped our planet’s surface.

Throughout each episode, Poppick introduces geologists working to unravel the numerous unanswered questions regarding the timing and causes of these changes. She visits significant geological sites, from Newfoundland to the Australian Outback, where one can observe the strata that articulate these narratives.

The recurring theme emphasizes the importance of paying attention to rocks. To an untrained observer, they may appear ordinary; however, Poppick reminds us that “a trained eye discerns physical and chemical indicators—proxies—that reveal the characteristics of our planet during the formation of these rocks.” She underscores the value of geologists’ expertise.

This book is a remarkable attempt to make stratigraphy engaging. At times, it falters, and Poppick’s fragmented writing style led me to lose the thread of the narrative.

Her comparisons of geological transformations to human-centric changes sometimes felt uneasy. For instance, she likens the Mesozoic greenhouse climate to modern carbon emissions, though the historical era’s temperatures were so extreme that such analogies may be misleading, even at optimistic emission projections.

Another limitation lies in the currently incomplete nature of geoscience. Some of the pivotal questions raised by Poppick—including the true cause of Snowball Earth—remain unresolved or are subject to debate among different factions. By the end, I was left with a sense of uncertainty about what can be definitively stated. Yet, that unpredictability might be intrinsic to geology itself. “Nothing is immutable in stone as our understanding of geology continues to evolve, just like the rocks,” Poppick states.

Nevertheless, the book effectively captures the grandeur of the story embedded in rocks. It does so particularly well by showing how seemingly mundane observations about rocks can lead directly to profound insights into Earth’s history. Such revelations illuminate the stratigraphic process as Poppick examines overlooked outcrops, encouraging us to perceive the rocks in our surroundings with renewed appreciation.

“Hierarchies are, in many ways, love letters from a maturing Earth,” she argues. This book abundantly reveals the reasons to uncover the secrets they hold.

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New Evidence of Ice-Rich Layered Deposits Found at Medusae Fossai by Mars Express

Over 15 years ago ESA's Mars Express spacecraft studied the Fossae Formation of Medusae and revealed mysterious deposits up to 2.5 km deep. These early observations left it unclear what the sediment was made of, but a new study provides an answer.

This image shows a height map of the surface of Mars, with the lowest land areas shown in blue and the highest land areas shown in white. Image credit: ESA.

of Formation of medusae fossa (MFF) – a huge and unusual soft rock deposit near Mars' equator – is about one-fifth the size of the continental United States and 100 times the mass of the largest explosive volcanic deposits on Earth.

It consists of several wind-carved features hundreds of kilometers in diameter and several kilometers high.

This feature, discovered at the boundary between highlands and lowlands on Mars, is probably the largest single source of dust on Mars.

Initial observations from ESA's Mars Express spacecraft show that the MFF is relatively transparent to radar and has low density, both characteristics seen in ice deposits.

But planetary scientists couldn't rule out the possibility that the terrain is actually drier, a huge accumulation of windblown dust, volcanic ash, or sediment.

“When we reexamined the MFF using new data from Mars Express's MARSIS radar, we found that the deposits were even thicker than we thought,” said Dr. Thomas Watters, a planetary researcher at the Smithsonian Institution. It's up to 3.7 kilometers thick,” said Dr. Thomas Watters, a planetary researcher at the Smithsonian Institution.

“Interestingly, the radar signal is consistent with what we would expect to see from layered ice, and is similar to the signal seen from the polar caps of Mars, which we know are very ice-rich.”

“If it were to melt, the ice trapped in the MFF would cover the entire planet in a layer of water 1.5 to 2.7 meters deep. This would be the largest amount of water ever discovered in this region of Mars. That's enough to fill Earth's Red Sea.”

“This is where the new radar data comes in. Given its depth, if the MFF is just a huge dust pile, we would expect it to be compressed under its own weight,” says the Italian National Institute of Astrophysics. said researcher Dr. Andrea Cicchetti.

“This will produce something much denser than what we're actually seeing with MARSIS.”

“And when we modeled how different materials behave without ice, nothing reproduced the properties of MFF. We need ice.”

“The new results suggest that there is instead a layer of dust and ice, topped by a protective layer of dry dust or ash hundreds of meters thick.”

In this image, the white line on Mars' surface (top) indicates the stretch of land scanned by Mars Express's MARSIS radar. The graph below shows the topography and subsurface structure of the land, with layers of dry sediment (likely dust or volcanic ash) shown in brown and layers of likely ice-rich sediment shown in blue. I am. The graph shows that the ice deposits are thousands of meters high and hundreds of kilometers wide. Once all the suspected water ice in the MFF melts, Mars will be covered by an ocean of water up to 2.7 meters deep. Image credit: CReSIS / KU / Smithsonian Institution.

“This latest analysis challenges our understanding of the MFF and raises as many questions as it answers,” said ESA Project Scientist for Mars Express and the ESA ExoMars Trace Gas Orbiter. said Dr. Colin Wilson.

“How long ago did these ice deposits form? What was Mars like at that time?”

“If confirmed to be water ice, these giant deposits could change our understanding of Mars' climate history.”

“Any ancient water reservoir would be an attractive target for human or robotic exploration.”

Result is, journal Geophysical Research Letters.

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thomas watters other. 2024. Evidence for ice-rich layered deposits in the Medusa Fossa Formation on Mars. Geophysical Research Lettersin press.

Source: www.sci.news