Identifying Hypotheses and Beliefs

Origin of Earth's Water

Liquid water covers approximately $71\%$ of Earth's surface, yet the origin of this water remains a subject of scientific debate. Scientists have proposed two main models to explain how Earth acquired its water.

*Model 1*
Earth's water was delivered during the late stage of planetary accretion by carbonaceous chondrites (meteorites originating from the outer asteroid belt). Carbonaceous chondrites are rich in water and organic compounds. The deuterium-to-hydrogen ($D/H$) ratio of these meteorites is approximately $1.4 \times 10^{-4}$, which closely matches the $D/H$ ratio of Earth’s modern oceans ($1.56 \times 10^{-4}$). Proponents of Model 1 argue that because asteroids formed closer to the Sun, they were more likely to intersect Earth's orbit during its final formation phases.

*Model 2*
Earth's water was delivered during the Late Heavy Bombardment, roughly $3.9$ billion years ago, by icy comets originating from the outer solar system. Comets contain up to $80\%$ water ice. Proponents of Model 2 argue that the extreme gravitational perturbations caused by the migration of giant planets scattered comets inward, resulting in frequent impacts on Earth. Although many comets have $D/H$ ratios of approximately $3.0 \times 10^{-4}$ (twice that of Earth's oceans), proponents argue that a subset of comets from the Kuiper Belt has $D/H$ ratios matching Earth's oceans and that comet impacts delivered the vast majority of Earth's volatile elements.

Based on the provided models, is the following statement true or false?

According to Model 2, gravitational perturbations caused by the migration of giant planets scattered comets inward, leading to frequent impacts that delivered Earth's water.

Ancient Lunar Magnetic Field Models

The Moon currently lacks a global magnetic field, but magnetized crustal rocks indicate it possessed one between $4.25$ and $3.56\text{ billion years ago}$ ($\text{Ga}$). Two models are proposed to explain this ancient lunar dynamo:

*Model 1 (Thermal-Compositional Dynamo)*
This model proposes that the lunar dynamo was driven by thermal and compositional convection within a liquid metallic core. As the core cooled, solid iron crystallized at the center, releasing lighter elements (such as sulfur) into the remaining liquid outer core. The buoyant rise of these lighter elements, combined with heat loss, drove fluid convection that maintained a continuous, stable magnetic field of approximately $100\text{ }\mu\text{T}$ for nearly $700\text{ million years}$, ending only when core crystallization was complete.

*Model 2 (Mechanical Impact Dynamo)*
This model proposes that the lunar dynamo was not continuously active but was periodically restarted by massive basin-forming impacts. A giant impactor would transfer immense angular momentum to the Moon’s mantle, temporarily altering its rotation rate relative to the liquid core. This differential rotation at the core-mantle boundary generated shear and turbulence in the liquid core, initiating a dynamo. Each dynamo event lasted only $10\text{ to }20\text{ million years}$ before friction synchronized the rotation of the mantle and core, extinguishing the magnetic field until the next major impact.

Statement: According to Model 2, a lunar crustal rock that crystallized continuously over a $50\text{-million-year}$ period of impact quiescence (a time with no large impacts) would record a strong, steadily active global magnetic field throughout its entire formation.

Three models are proposed to explain the formation of hematite ($\text{Fe}_2\text{O}_3$) spherules, commonly called "blueberries," discovered in the Meridiani Planum region of Mars.

*Model 1*
Spherules formed in situ within porous basaltic volcanic rock. Upwelling volcanic fluids heated to temperatures between $150^\circ\text{C}$ and $250^\circ\text{C}$ circulated through underground aquifers. These fluids, neutral in pH and rich in dissolved iron, encountered sudden pressure drops, causing hematite to precipitate symmetrically in all directions within spherical pore spaces (vesicles). Because the vesicles were free of mineral grains, the resulting spherules consist of pure, crystalline hematite with no internal sedimentary inclusions.

*Model 2*
Spherules formed as chemical concretions in a shallow, highly acidic ($pH < 3.0$), hypersaline surface lake. Liquid water containing dissolved $\text{Fe}^{3+}$ ions seeped downward through porous quartz sandstone. The acidic water reacted with localized, alkaline carbonate minerals within the sandstone, raising the pH and causing hematite to precipitate outward from nucleation centers. Consequently, these spherules grew around and enveloped surrounding quartz sand grains, resulting in a concentric internal structure containing micro-grains of quartz.

*Model 3*
Spherules are impact spherules created during a hypervelocity meteorite impact on the Martian surface. The impact vaporized iron-rich basaltic target rocks and the iron-nickel meteorite itself, ejecting a plume of vapor and molten droplets into the upper atmosphere. As the droplets fell back toward the surface, they cooled and solidified into spherical shapes. The spherules accumulated as a distinct, widespread air-fall layer on top of preexisting rock units, rather than growing within them.

Match each description of a spherule's formation mechanism or physical constraint to the specific model that proposes it.

Passage

Two biologists present competing hypotheses regarding the evolutionary origin of hydrogenosomes, double-membraned organelles found in certain anaerobic eukaryotes that produce molecular hydrogen ($H_2$).

Biologist 1
Hydrogenosomes evolved directly from an ancestral anaerobic endosymbiotic bacterium that was distinct from the aerobic $\alpha$-proteobacterium that gave rise to mitochondria. This ancestral endosymbiont belonged to an anaerobic lineage of bacteria that possessed hydrogenase enzymes. Over evolutionary time, this bacterium transferred most of its genome to the host nucleus, leaving an organelle specialized for anaerobic ATP production. Consequently, hydrogenosomes and mitochondria represent completely independent endosymbiotic events.

Biologist 2
Hydrogenosomes and mitochondria share a common endosymbiotic ancestor: a facultatively anaerobic $\alpha$-proteobacterium. Depending on the environmental pressures faced by the host eukaryotic lineage, this single ancestral organelle diverged. In aerobic environments, it evolved into mitochondria, retaining the electron transport chain. In strictly anaerobic environments, it lost the electron transport chain and evolved into hydrogenosomes. Thus, hydrogenosomes are highly modified mitochondria rather than the product of a separate endosymbiotic event.

Based on Biologist 1's hypothesis, if a newly discovered anaerobic eukaryote is found to contain hydrogenosomes that still retain a small genome, the genes in this organellar genome would be expected to share the greatest sequence similarity with the genes of which of the following groups?

Martian Methane Origins

Methane ($\text{CH}_4$) has been detected in the Martian atmosphere, sparking debate over its origin. Because methane is rapidly destroyed by solar ultraviolet radiation, its presence requires an active source. Two scientists present hypotheses regarding the source of Martian methane.

Scientist 1
Martian methane is biogenic, produced by subsurface methanogenic microbes. These microbes reside deep underground where liquid water is stable, utilizing carbon dioxide ($\text{CO}_2$) and hydrogen ($\text{H}_2$) to produce $\text{CH}_4$ as a metabolic byproduct. Scientist 1 points out that the detected methane exhibits seasonal fluctuations, peaking during the Martian summer when warmer temperatures increase microbial metabolic activity. Furthermore, carbon isotope analysis shows a depletion of carbon-13 ($^{13}\text{C}$) relative to carbon-12 ($^{12}\text{C}$) in atmospheric methane samples, which is a classic signature of biological processing.

Scientist 2
Martian methane is abiogenic, produced by serpentinization, a geological process in which water reacts with olivine-rich rocks in the presence of carbon dioxide. This reaction occurs deep within the Martian crust where geothermal heat warms the rocks. Scientist 2 argues that the seasonal fluctuations are caused by the seasonal release of methane trapped in clathrate hydrates (water ice cages) as the surface temperature warms, rather than biological activity. According to Scientist 2, abiotic reactions can produce similar carbon isotope signatures in environments with highly localized hydrogeochemical pathways, meaning the carbon-13 depletion is not exclusive to biological sources.

Based on the viewpoints of the two scientists, which of the following assumptions is implicit in Scientist 1's argument but disputed by Scientist 2?

Two scientists present competing hypotheses regarding the origin of Earth's water.

Scientist 1
Earth's water originated primarily from volcanic outgassing. As the early Earth cooled, water vapor released from molten rock in the mantle condensed to form the oceans. This water was present within the planet's building blocks during its initial formation.

Scientist 2
Earth's water was delivered primarily by icy comets and carbonaceous meteorites that bombarded the planet after its crust had solidified. The isotopic ratio of hydrogen in Earth's oceans matches that of outer solar system comets, suggesting an extraterrestrial origin.

According to Scientist 1, Earth's water was originally introduced to the surface through which of the following processes?

Warm Jupiters are giant exoplanets with orbits between $0.1\text{ AU}$ and $1.0\text{ AU}$. Astronomers propose three models to explain their origin:

* Model 1 (In-Situ Formation): Warm Jupiters form at their current orbital distances. Because this region contains little mass in typical protoplanetary disks, Model 1 assumes that the local disk surface density must have been at least 100 times greater than the minimum mass solar nebula. Under this hypothesis, dust grains coagulated rapidly to form a $10\ M_\oplus$ core, which then triggered runaway gas accretion from the local gas reservoir. This entire process must be completed within 1–2 million years, before the stellar wind disperses the gas.
* Model 2 (Disk Migration): Warm Jupiters form beyond the 'ice line' ($>3\text{ AU}$), where water ice can condense, providing abundant solid material to build a massive core. The planet then migrates inward because of tidal torque from the gas disk (Type II migration). This migration is driven by the exchange of angular momentum between the planet and the gas disk. Model 2 assumes that migration ceases when the planet reaches the inner edge of the gas disk or when the gas disk is photodissipated by the host star.
* Model 3 (High-Eccentricity Tidal Migration): Like Model 2, Model 3 assumes Jovian planets must form beyond the ice line ($>3\text{ AU}$) to acquire enough solid ice and dust for core growth. However, after formation, the planet is perturbed into a highly eccentric orbit ($e > 0.9$) by the gravitational influence of a distant companion star or planet. During periastron (closest approach to the host star), the intense tidal forces stretch and compress the planet, dissipating orbital energy as heat within the planet. This process, known as tidal circularization, slowly shrinks and circularizes the orbit over hundreds of millions of years. Model 3 assumes that the gas disk is completely gone before the gravitational perturbations trigger this high-eccentricity phase.

Based on the models described, is the following statement true or false?

'Model 2 and Model 3 both hypothesize that the initial formation of a gas giant's core requires a region of the protoplanetary disk where temperatures are low enough for water ice to condense, whereas Model 1 assumes that core formation can occur in much warmer regions closer to the star provided there is an exceptionally high density of dust.'

Three students propose hypotheses to explain why a copper coin turns green over time:

* Student 1 believes that the green color is copper carbonate formed when copper reacts with carbon dioxide and water vapor in the air.
* Student 2 believes that the green color is copper chloride formed when copper reacts with airborne chlorine from coastal salt spray.
* Student 3 believes that the green color is copper oxide formed when copper reacts only with gaseous oxygen in dry air.

Match each chemical requirement for the coin turning green to the student who proposes it.

Hydrangea plants can produce flowers that are either pink or blue. Two students propose different hypotheses to explain the primary factor that determines this flower color.

Student 1
The color change of hydrangea flowers is determined directly by the pH of the surrounding soil. When the soil is acidic (pH less than $6.0$), the hydrogen ion concentration directly alters the chemical structure of the pigment anthocyanin within the flower petals, causing it to reflect blue light. In alkaline soil (pH greater than $7.0$), the pigment's structure remains unchanged, and the flowers appear pink.

Student 2
The color change of hydrangea flowers is determined directly by the absorption of aluminum ions ($\text{Al}^{3+}$) from the soil, which form a chemical complex with the pigment anthocyanin to produce the blue color. Soil pH is only an indirect factor: acidic soil makes aluminum ions soluble and available for the plant to absorb, while alkaline soil binds aluminum ions in insoluble compounds, preventing absorption and resulting in pink flowers.

Based on Student 2's hypothesis, which of the following is the direct cause of the blue color in hydrangea flowers?

Three models are proposed to explain the thermal energy source and fracturing mechanism responsible for the cryovolcanic plumes observed at the south pole of Saturn's moon, Enceladus.

Model 1
The parallel fractures (tiger stripes) are open conduits connected to a localized subsurface reservoir of liquid water. Saturn's gravitational pull exerts varying tidal forces on Enceladus along its eccentric orbit. This tidal flexing causes the walls of the fractures to rub against one another. Frictional heating along these sliding faults melts the surrounding ice, generating the heat that keeps the vents open and drives the vapor plumes.

Model 2
The thermal energy source is radiogenic decay within the silicate core, which maintains a global subsurface ocean. As the moon slowly cools, the outer ice shell thickens. Because ice is less dense than liquid water, this freezing process expands the shell, generating intense hydrostatic pressure within the underlying ocean. Once the pressure exceeds the tensile strength of the ice shell, fracturing occurs, violently venting pressurized water into space.

Model 3
Cold water from the subsurface ocean migrates downward, circulating through a porous, fractured silicate core. An exothermic chemical reaction known as serpentinization occurs between the water and olivine-rich rocks in the core, raising the water temperature. This reaction also releases gases, primarily $H_2$. The resulting warm, buoyant, gas-rich fluids rise rapidly, melting conduits through the overlying ice shell to erupt as plumes.

Based on the models provided, match each key hypothesis regarding the primary energy source or fracturing mechanism on Enceladus to the corresponding model.

Two students discuss the cause of the glowing blue waves observed in some coastal waters at night.

Student 1: The glow is produced entirely by bioluminescent dinoflagellates (microscopic organisms) that emit light when physically disturbed by wave motion or predators. The temperature of the water has no direct effect on their light production.

Student 2: The glow is caused by phosphorescent minerals dissolved in the water that absorb sunlight during the day and re-emit it at night. This process is highly dependent on water temperature, with warmer water causing a brighter glow.

According to Student 1's hypothesis, the glowing waves are directly caused by which of the following?

Archean Haze Models

During the Archean Eon (approximately $4.0$ to $2.5$ billion years ago), Earth's atmosphere was rich in methane ($CH_4$) and carbon dioxide ($CO_2$) but lacked oxygen ($O_2$). Solar ultraviolet (UV) radiation drove photochemical reactions in this atmosphere, producing a hydrocarbon haze. Proponents of three models debate the characteristics and climate impacts of this Archean haze.

Model 1 (Organic Haze Model)
Proponents of Model 1 propose that the haze was composed of complex organic polymers formed at high altitudes (above $40\text{ km}$) where solar UV flux was greatest. These polymer particles grew as fluffy, fractal aggregates (non-spherical shapes). Proponents believe that because of their high fractal dimension, the aggregates scattered incoming solar radiation poorly but allowed thermal infrared radiation from Earth's surface to pass through. Thus, the haze did not cause global cooling (an "anti-greenhouse" effect), allowing $CH_4$ and $CO_2$ in the lower atmosphere to maintain liquid surface water.

Model 2 (Sulfate-Shielded Haze Model)
Proponents of Model 2 argue that volcanic emissions of sulfur dioxide ($SO_2$) reacted with atmospheric water vapor, forming sulfate ($H_2SO_4$) aerosols in the lower atmosphere (below $15\text{ km}$). These polar sulfate droplets coated the organic polymers, causing the aggregate structures to collapse into compact, smooth spheres. Proponents believe that these spherical particles highly efficiently scattered incoming solar radiation back into space, creating a strong anti-greenhouse cooling effect. Proponents assume that surface liquid water was maintained only because the cooling was offset by extremely high concentrations of greenhouse gases ($CO_2$ and $H_2S$) trapped in the lower troposphere.

Model 3 (Biogenic Carbonate Haze Model)
Proponents of Model 3 suggest that windblown biogenic carbonate dust ($CaCO_3$) from early microbial mats served as the primary nucleation sites for organic haze throughout the entire atmospheric column. These composite dust-organic particles had a carbonate core and an organic shell. Proponents believe that this unique structure allowed the haze to actively absorb outgoing thermal infrared radiation, directly contributing to greenhouse warming. Proponents assume that a biological feedback loop existed: cooler surface temperatures reduced microbial activity, decreasing carbonate dust emission and haze density, which subsequently mitigated cooling.

Based on the descriptions of Model 2 and Model 3, the proponents of these two models would most likely disagree on which of the following questions regarding the Archean atmospheric haze?

The Fermi Bubbles are two massive structures of high-energy gamma-ray and X-ray emission extending approximately $25{}000\text{ light-years}$ above and below the center of the Milky Way galaxy. Astronomers have proposed three models to explain the origin of these bubbles.

*Model 1*
The bubbles were inflated by a pair of highly collimated plasma jets ejected perpendicular to the galactic plane. These jets were powered by a single, rapid accretion event onto Sagittarius $\text{A}^*$ ($\text{Sgr A}^*$), the supermassive black hole at the galactic center. This event occurred $3\text{ to }6\text{ million years}$ ago and lasted for less than $100{}000\text{ years}$. The bubbles are relatively young structures formed by this brief, explosive release of magnetic and kinetic energy.

*Model 2*
The bubbles are the result of a sustained galactic wind driven by a period of intense starburst activity near the galactic center. Over the past $10\text{ million years}$, thousands of massive stars underwent core-collapse supernovae, releasing kinetic energy and stellar winds. This cumulative energy pushed gas out of the galactic disk, slowly inflating the bubbles over millions of years. Consequently, the gas within the bubbles should contain high concentrations of heavy elements synthesized during these supernovae.

*Model 3*
The bubbles were formed by a series of periodic, discrete energy injections over the last $5\text{ million years}$. These injections occurred when individual stars passed too close to $\text{Sgr A}^*$ and were torn apart by tidal forces, a process known as a Tidal Disruption Event (TDE). The accretion of this stellar debris onto $\text{Sgr A}^*$ generated recurring, episodic outflows. Rather than a single massive event or steady stellar winds, the current volume of the bubbles is the cumulative result of these individual stellar destruction episodes.

Based on the passage, match each of the three models with the statement that best represents its underlying hypothesis or key belief.

Two students propose hypotheses to explain the primary energy source for deep-sea hydrothermal vent ecosystems.

Student 1
The primary energy source for these ecosystems is geothermal heat emitted directly from the vents. Organisms in these environments have adapted to absorb this heat energy directly to power their metabolic processes.

Student 2
The primary energy source is chemical energy from dissolved compounds, such as hydrogen sulfide ($H_2S$), present in the vent fluids. Specialized bacteria use chemosynthesis to convert these chemicals into organic matter, which forms the base of the food web.

Based on these hypotheses, evaluate the truth of the following statement: Student 2 believes that geothermal heat is absorbed directly by organisms as their primary energy source.

The Younger Dryas was a period of abrupt cooling that occurred approximately 12,900 years ago. Two scientists propose different hypotheses regarding the primary trigger of this cooling event.

Scientist 1
The Younger Dryas cooling was triggered by the sudden release of a massive volume of freshwater from Lake Agassiz into the North Atlantic Ocean. This freshwater influx reduced the salinity and density of the surface waters, disrupting the Atlantic Meridional Overturning Circulation (AMOC). Because the AMOC transports warm tropical water northward, its slowdown immediately cooled the North Atlantic region, initiating global climate feedbacks.

Scientist 2
The Younger Dryas cooling was triggered by the impact or airburst of a disintegrating comet over North America. This impact event ignited widespread wildfires, releasing immense quantities of soot, ash, and dust into the atmosphere. This atmospheric shroud blocked incoming solar radiation, causing immediate global cooling (an 'impact winter'). The physical disruption also destabilized ice sheets, leading to freshwater runoff, which was a secondary effect rather than the primary cause of the cooling.

Based on the passage, match each concept on the left with the corresponding hypothesis or description on the right.

Titan, Saturn's largest moon, has liquid methane ($CH_4$) and ethane ($C_2H_6$) lakes on its surface. Since atmospheric methane is continuously destroyed by solar photolysis, it must be replenished from the moon's interior to maintain these lakes. Two models are proposed to explain this replenishment mechanism.

Model 1 (Clathrate Outgassing)
Titan's methane is stored in the crust within methane clathrate hydrates (water ice cages trapping methane molecules). Thermal anomalies caused by episodic runaway convection in Titan's rocky core warm the ice crust. This warming destabilizes the clathrate hydrates, releasing methane gas that rises through fractures to the surface and atmosphere. This process occurs in discrete outgassing events every few hundred million years, meaning lake levels fluctuate significantly over geologic time.

Model 2 (Cryovolcanic Eruptions)
Titan's interior contains a deep liquid water-ammonia ocean beneath a convective ice shell. Methane is dissolved directly in this sub-surface ocean. When pressure builds due to partial freezing of the ocean, cryovolcanic plumes of liquid water, ammonia, and dissolved methane erupt onto the surface. This cryovolcanism is a continuous process driven by tidal heating from Saturn, ensuring a steady, constant supply of methane to the surface lakes and atmosphere.

Which of the following beliefs is held by the proponents of Model 1 but NOT by the proponents of Model 2 regarding the replenishment of Titan's methane lakes?

Two scientists present competing viewpoints on the origin of Earth's oceans.

Scientist 1
Earth’s liquid water originated primarily from volcanic outgassing during the planet's early history. As Earth cooled, water vapor released from molten rock condensed and fell as rain, filling the ocean basins. This water was entirely native to the materials that formed early Earth.

Scientist 2
Earth’s liquid water was delivered by comets and water-rich asteroids during the Late Heavy Bombardment, billions of years ago. The heat of early Earth would have vaporized and lost any original water. Therefore, Earth's oceans could only have formed from these external cosmic impacts.

Based on Scientist 1's viewpoint, which of the following statements best describes the origin of Earth's oceans?

Although the Martian atmosphere is composed primarily of carbon dioxide ($CO_2$), planetary missions have detected trace amounts of methane ($CH_4$). Because atmospheric methane is rapidly destroyed by solar ultraviolet radiation, its persistent presence suggests an ongoing source of replenishment. Scientists have proposed two models to explain the origin and release of methane on Mars.

Model 1 (Biogenic Hypothesis)
Martian methane is produced by subsurface methanogenic archaea residing in deep liquid-water aquifers. These micro-organisms consume carbon dioxide and hydrogen gas ($H_2$) to sustain their metabolism, releasing methane as a byproduct. Proponents of Model 1 believe that subsurface biological activity is directly influenced by seasonal temperature cycles. During the Martian summer, localized subsurface warming increases microbial metabolic rates and causes thermal expansion of the aquifers, forcing accumulated methane gas upward through seasonal fractures in the overlying cryosphere.

Model 2 (Abiogenic Hypothesis)
Martian methane is produced abiotically through serpentinization, a reaction between water and ultramafic rocks rich in the mineral olivine ($(Mg,Fe)_2SiO_4$) within the Martian crust. This reaction occurs at high temperatures and pressures deep underground, yielding hydrogen gas ($H_2$) as a byproduct. The hydrogen subsequently reacts with dissolved carbon dioxide ($CO_2$) via a mineral-catalyzed Fischer-Tropsch-type synthesis to form methane. Proponents of Model 2 believe that because geothermal heat is stable, methane production occurs at a constant rate. Its release into the atmosphere is regulated solely by episodic tectonic fracturing that opens pathways from the deep crust to the surface, completely independent of seasonal variations in surface temperature.

Which of the following assumptions is implicitly required by Model 1's hypothesis regarding the seasonal variation of Martian atmospheric methane, but is NOT required by Model 2?

Two students discuss the sudden decline of the yellow trout lily population in a local forest.

Student 1: The decline is due to a decrease in soil pH (increased acidity) resulting from acid rain. This acidity prevents the lilies from absorbing essential nutrients, causing them to wither and die.

Student 2: The decline is caused by an increase in the population of the red-backed salamander. These salamanders compact the soil around the lily bulbs, preventing water from reaching the roots.

Based on the explanations, determine whether the following statement is true or false:

Student 2 believes that the wildflower decline is caused by chemical changes in the soil.

Silica-rich deposits discovered on Mars have led to competing models regarding their origin. Three scientists propose different mechanisms for how these deposits formed:

Scientist 1
The deposits formed through acid-sulfate leaching. Acidic groundwater ($pH < 3$) containing dissolved sulfate ions flowed through subterranean basaltic rocks. The acidic fluid selectively dissolved and removed elements such as magnesium ($Mg$), iron ($Fe$), and calcium ($Ca$), leaving behind a highly concentrated, insoluble silica residue ($SiO_2 > 90\%$). This process occurred under ambient, low-temperature subterranean conditions.

Scientist 2
The deposits resulted from solfataric alteration. High-temperature volcanic gases ($>200^\circ\text{C}$), specifically sulfur dioxide ($SO_2$) and hydrogen chloride ($HCl$), mixed with water vapor and rose through crustal fractures. This acidic steam reacted with the surrounding rock, vaporizing volatile metals and carrying them away, leaving amorphous silica crusts at the surface outlets (fumaroles).

Scientist 3
The deposits precipitated directly from a surface water body. A highly alkaline, silica-saturated lake filled the crater. As the lake water evaporated under cold, dry conditions, the concentration of dissolved silica exceeded saturation limits. This caused the silica to precipitate out of the solution alongside evaporite minerals like gypsum.

Match each specific geological mechanism to the scientist whose model proposes that mechanism.