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It seems like you pasted the wrong paragraph partition. The third paragraph seems to start with "However, ... end" with "...more common than they are today" not "...such compounds". This may lead to different interpretation in question 4.

Thank you. Fixed the issue.
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But in the mock, it shows as follows (attached image)
I too was confused between A and B for question 4.

Edit: It doesn't matter, as the highlighted question isn't questioning the hypothesis that gases couldn't have led to the origin of life.
The geologists say that the gases weren't concentrated enough in the 'atmosphere'. The passage accepts this.
But then pivots to a different location where the gases are concentrated and supports that the gases led to the origin of life -the author says that the gases were far more concentrated in the Lost City 'waters'.
“Billions of years ago, could vents like Lost City have produced the needed organics?” -This is not doubting; it’s suggesting: maybe the chemistry happened in vents, not the atmosphere.
Then comes support for that hypothesis:
  • “Lost City fluids contain organic compounds.”
  • “Early Earth probably had peridotite seafloor (so Lost-City-like vents were common).”

In a way, this question/new hypothesis is trying to make the earlier hypothesis - 'gases could lead to the origin of life' work.

This wasn't easy at all!
Hope this helps.
user1937
­Scientists have discovered a remarkable undersea field of hot springs and gigantic chimneys, unlike anything seen before, and named it Lost City. Geologist Deborah Kelley led an expedition to analyze Lost City, obtaining results that have prompted reconsideration of how life on Earth first emerged and of where extraterrestrial life might also exist.

Around most hydrothermal vents, the seawater is extremely acidic and reaches temperatures over 400 degrees Celsius. But at Lost City, the water is alkaline and no hotter than 90 degrees Celsius. And unlike other hydrothermal vents, those at Lost City are situated on seafloor consisting mainly of rock called peridotite. Seawater reacts with the peridotite, producing energy-rich gases such as hydrogen and methane. Some scientists speculate that these gases could have fostered the emergence of life on Earth. A famous experiment conducted in 1952 showed that sparks discharging through energy-rich gases produce many organic compounds, including amino acids, which are components of all living things.

However, geologists later concluded that these gases were probably not concentrated enough in Earth's early atmosphere to form such compounds. But the gases are far more concentrated in the Lost City waters. Billions of years ago, could vents resembling those at Lost City have produced the organic compounds required for life? Hydrothermal fluids at Lost City contain certain organic compounds. And on early Earth, peridotite probably comprised most of the seafloor, making conditions like those at Lost City far more common than they are today.

Lost City also teems with microbes such as methanogens, which metabolize hydrogen and generate methane. Each step in the geothermal process that generates methane is replicated in the biochemical pathways of these methanogens. This suggests that on early Earth, the methanogens' primordial ancestors at sites like Lost City may have simply co-opted each of the geochemical steps for themselves, producing the first biochemical pathways, which their descendents have inherited.

The Lost City findings also suggest that extraterrestrial life could exist on any planet or moon containing peridotite and liquid water. Evidence of these components is strongest on Mars and on Jupiter's moon Europa, and researchers have detected methane in the Martian atmosphere. Whether the methane comes from microbes or chemical reactions remains uncertain.

1. To support the hypothesis that hydrogen and methane fostered the emergence of life on Earth, the passage mentions the

(A) concentrations of these gases in Earth's early atmosphere
(B) discharge of sparks through gases around hydrothermal vents
(C) likely composition of the early Earth's seafloor
(D) temperature and alkalinity of the seawater on ancient Earth
(E) chemical reactions of seawater with energy-rich gases



2. The passage indicates that most current hydrothermal vents

(A) teem with methanogens and similar microbes
(B) are not found on undersea beds of peridotite
(C) have natural chimneys that vent acidic seawater
(D) produce organic compounds such as amino acids
(E) generate hydrogen and methane at high temperatures



3. The passage most clearly implies that some of the microbes at Lost City may

(A) use methane generated by geothermal reactions to support their metabolic processes
(B) descend from extraterrestrial life-forms that originated billions of years ago
(C) consume certain organic compounds found in hydrothermal fluids within natural chimneys
(D) be able to withstand the acidic seawater and extreme temperatures found around most other hydrothermal vents
(E) have biochemical pathways that first appeared among primordial life forms billions of years ago



4. The question asked in the third paragraph (see highlighted text in red) serves mainly to

(A) suggest a hypothesis that the other sentences in the third paragraph help support
(B) raise doubts about a hypothesis stated explicitly in the second paragraph
(C) rhetorically imply that the main conclusion of the passage as a whole needs additional support
(D) indirectly help explain the presence of the geothermal process discussed in the fourth paragraph
(E) indicate the issue that most strongly motivated Kelley to lead her expedition to analyze Lost City­


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Screenshot 2025-10-05 113604.png
Screenshot 2025-10-05 113604.png [ 130.13 KiB | Viewed 1516 times ]

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user1937
­Scientists have discovered a remarkable undersea field of hot springs and gigantic chimneys, unlike anything seen before, and named it Lost City. Geologist Deborah Kelley led an expedition to analyze Lost City, obtaining results that have prompted reconsideration of how life on Earth first emerged and of where extraterrestrial life might also exist.

Around most hydrothermal vents, the seawater is extremely acidic and reaches temperatures over 400 degrees Celsius. But at Lost City, the water is alkaline and no hotter than 90 degrees Celsius. And unlike other hydrothermal vents, those at Lost City are situated on seafloor consisting mainly of rock called peridotite. Seawater reacts with the peridotite, producing energy-rich gases such as hydrogen and methane. Some scientists speculate that these gases could have fostered the emergence of life on Earth. A famous experiment conducted in 1952 showed that sparks discharging through energy-rich gases produce many organic compounds, including amino acids, which are components of all living things. However, geologists later concluded that these gases were probably not concentrated enough in Earth's early atmosphere to form such compounds.

But the gases are far more concentrated in the Lost City waters. Billions of years ago, could vents resembling those at Lost City have produced the organic compounds required for life? Hydrothermal fluids at Lost City contain certain organic compounds. And on early Earth, peridotite probably comprised most of the seafloor, making conditions like those at Lost City far more common than they are today.

Lost City also teems with microbes such as methanogens, which metabolize hydrogen and generate methane. Each step in the geothermal process that generates methane is replicated in the biochemical pathways of these methanogens. This suggests that on early Earth, the methanogens' primordial ancestors at sites like Lost City may have simply co-opted each of the geochemical steps for themselves, producing the first biochemical pathways, which their descendants have inherited.

The Lost City findings also suggest that extraterrestrial life could exist on any planet or moon containing peridotite and liquid water. Evidence of these components is strongest on Mars and on Jupiter's moon Europa, and researchers have detected methane in the Martian atmosphere. Whether the methane comes from microbes or chemical reactions remains uncertain.

1. To support the hypothesis that hydrogen and methane fostered the emergence of life on Earth, the passage mentions the

(A) concentrations of these gases in Earth's early atmosphere
(B) discharge of sparks through gases around hydrothermal vents
(C) likely composition of the early Earth's seafloor
(D) temperature and alkalinity of the seawater on ancient Earth
(E) chemical reactions of seawater with energy-rich gases



2. The passage indicates that most current hydrothermal vents

(A) teem with methanogens and similar microbes
(B) are not found on undersea beds of peridotite
(C) have natural chimneys that vent acidic seawater
(D) produce organic compounds such as amino acids
(E) generate hydrogen and methane at high temperatures



3. The passage most clearly implies that some of the microbes at Lost City may

(A) use methane generated by geothermal reactions to support their metabolic processes
(B) descend from extraterrestrial life-forms that originated billions of years ago
(C) consume certain organic compounds found in hydrothermal fluids within natural chimneys
(D) be able to withstand the acidic seawater and extreme temperatures found around most other hydrothermal vents
(E) have biochemical pathways that first appeared among primordial life forms billions of years ago



4. The question asked in the third paragraph (see highlighted text in red) serves mainly to

(A) suggest a hypothesis that the other sentences in the third paragraph help support
(B) raise doubts about a hypothesis stated explicitly in the second paragraph
(C) rhetorically imply that the main conclusion of the passage as a whole needs additional support
(D) indirectly help explain the presence of the geothermal process discussed in the fourth paragraph
(E) indicate the issue that most strongly motivated Kelley to lead her expedition to analyze Lost City­


Discussed this passage and questions here:

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