Welcome to Crimetown, a series produced by Marc Smerling and Zac Stuart-Pontier in partnership with Gimlet Media. Each season, we investigate the culture of crime in a different city. In Season 2, Crimetown heads to the heart of the Rust Belt: Detroit, Michigan. From its heyday as Motor City to its rebirth as the Brooklyn of the Midwest, Detroit’s history reflects a series of issues that strike at the heart of American identity: race, poverty, policing, loss of industry, the war on drugs, an ...
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Audioboom and John Batchelor에서 제공하는 콘텐츠입니다. 에피소드, 그래픽, 팟캐스트 설명을 포함한 모든 팟캐스트 콘텐츠는 Audioboom and John Batchelor 또는 해당 팟캐스트 플랫폼 파트너가 직접 업로드하고 제공합니다. 누군가가 귀하의 허락 없이 귀하의 저작물을 사용하고 있다고 생각되는 경우 여기에 설명된 절차를 따르실 수 있습니다 https://ko.player.fm/legal.
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HEADLINE: Life on Land Collaboration: Devonian Mycorrhizae and Silurian Deep-Sea Vents BOOK TITLE: Other Lands, A Journey Through Earth's Extinct Worlds GUEST AUTHOR NAME: Thomas Halliday 200-WORD SUMMARY: This source details the move of life onto land an
Manage episode 510944089 series 96788
Audioboom and John Batchelor에서 제공하는 콘텐츠입니다. 에피소드, 그래픽, 팟캐스트 설명을 포함한 모든 팟캐스트 콘텐츠는 Audioboom and John Batchelor 또는 해당 팟캐스트 플랫폼 파트너가 직접 업로드하고 제공합니다. 누군가가 귀하의 허락 없이 귀하의 저작물을 사용하고 있다고 생각되는 경우 여기에 설명된 절차를 따르실 수 있습니다 https://ko.player.fm/legal.
HEADLINE: Life on Land Collaboration: Devonian Mycorrhizae and Silurian Deep-Sea Vents
BOOK TITLE: Other Lands, A Journey Through Earth's Extinct Worlds
GUEST AUTHOR NAME: Thomas Halliday
200-WORD SUMMARY: This source details the move of life onto land and the origins of ecosystems. In the Devonian(407 million years ago), life thrived through collaboration, notably the crucial partnership of Mycorrhizae (fungi and roots). This collaboration was essential for plants to develop roots and extract mineral resources from rocks, while the fungi gained energy from plant photosynthesis. Evidence from Rynie, Scotland—a Yellowstone-like ecosystem with hot springs—shows detailed preservation of these interactions. The largest organism on land at this time was Prototaxites, a lichen structure that grew up to 9 meters tall. Arthropods, such as the freshwater shrimp Rhyniella, were among the first animals to inhabit the land. The conversation shifts to the Silurian (435 million years ago) and the deep ocean. The site of Yaman-Kassie is the earliest known fossilized hydrothermal vent with organisms living on it. These deep-sea vents support life via a chemical-based food chain independent of light. Halliday references the major hypothesis that life itself originated at similar deep alkaline vents, based on replicable chemistry that naturally creates the necessary hydrogen ion gradients. The segment concludes with the Ordovician mass extinction (444 million years ago), the first of the "big five" mass extinctions, which was caused by global cooling followed by rapid warming, stressing marine life with a high rate of climate change.
BOOK TITLE: Other Lands, A Journey Through Earth's Extinct Worlds
GUEST AUTHOR NAME: Thomas Halliday
200-WORD SUMMARY: This source details the move of life onto land and the origins of ecosystems. In the Devonian(407 million years ago), life thrived through collaboration, notably the crucial partnership of Mycorrhizae (fungi and roots). This collaboration was essential for plants to develop roots and extract mineral resources from rocks, while the fungi gained energy from plant photosynthesis. Evidence from Rynie, Scotland—a Yellowstone-like ecosystem with hot springs—shows detailed preservation of these interactions. The largest organism on land at this time was Prototaxites, a lichen structure that grew up to 9 meters tall. Arthropods, such as the freshwater shrimp Rhyniella, were among the first animals to inhabit the land. The conversation shifts to the Silurian (435 million years ago) and the deep ocean. The site of Yaman-Kassie is the earliest known fossilized hydrothermal vent with organisms living on it. These deep-sea vents support life via a chemical-based food chain independent of light. Halliday references the major hypothesis that life itself originated at similar deep alkaline vents, based on replicable chemistry that naturally creates the necessary hydrogen ion gradients. The segment concludes with the Ordovician mass extinction (444 million years ago), the first of the "big five" mass extinctions, which was caused by global cooling followed by rapid warming, stressing marine life with a high rate of climate change.
51575 에피소드
Manage episode 510944089 series 96788
Audioboom and John Batchelor에서 제공하는 콘텐츠입니다. 에피소드, 그래픽, 팟캐스트 설명을 포함한 모든 팟캐스트 콘텐츠는 Audioboom and John Batchelor 또는 해당 팟캐스트 플랫폼 파트너가 직접 업로드하고 제공합니다. 누군가가 귀하의 허락 없이 귀하의 저작물을 사용하고 있다고 생각되는 경우 여기에 설명된 절차를 따르실 수 있습니다 https://ko.player.fm/legal.
HEADLINE: Life on Land Collaboration: Devonian Mycorrhizae and Silurian Deep-Sea Vents
BOOK TITLE: Other Lands, A Journey Through Earth's Extinct Worlds
GUEST AUTHOR NAME: Thomas Halliday
200-WORD SUMMARY: This source details the move of life onto land and the origins of ecosystems. In the Devonian(407 million years ago), life thrived through collaboration, notably the crucial partnership of Mycorrhizae (fungi and roots). This collaboration was essential for plants to develop roots and extract mineral resources from rocks, while the fungi gained energy from plant photosynthesis. Evidence from Rynie, Scotland—a Yellowstone-like ecosystem with hot springs—shows detailed preservation of these interactions. The largest organism on land at this time was Prototaxites, a lichen structure that grew up to 9 meters tall. Arthropods, such as the freshwater shrimp Rhyniella, were among the first animals to inhabit the land. The conversation shifts to the Silurian (435 million years ago) and the deep ocean. The site of Yaman-Kassie is the earliest known fossilized hydrothermal vent with organisms living on it. These deep-sea vents support life via a chemical-based food chain independent of light. Halliday references the major hypothesis that life itself originated at similar deep alkaline vents, based on replicable chemistry that naturally creates the necessary hydrogen ion gradients. The segment concludes with the Ordovician mass extinction (444 million years ago), the first of the "big five" mass extinctions, which was caused by global cooling followed by rapid warming, stressing marine life with a high rate of climate change.
BOOK TITLE: Other Lands, A Journey Through Earth's Extinct Worlds
GUEST AUTHOR NAME: Thomas Halliday
200-WORD SUMMARY: This source details the move of life onto land and the origins of ecosystems. In the Devonian(407 million years ago), life thrived through collaboration, notably the crucial partnership of Mycorrhizae (fungi and roots). This collaboration was essential for plants to develop roots and extract mineral resources from rocks, while the fungi gained energy from plant photosynthesis. Evidence from Rynie, Scotland—a Yellowstone-like ecosystem with hot springs—shows detailed preservation of these interactions. The largest organism on land at this time was Prototaxites, a lichen structure that grew up to 9 meters tall. Arthropods, such as the freshwater shrimp Rhyniella, were among the first animals to inhabit the land. The conversation shifts to the Silurian (435 million years ago) and the deep ocean. The site of Yaman-Kassie is the earliest known fossilized hydrothermal vent with organisms living on it. These deep-sea vents support life via a chemical-based food chain independent of light. Halliday references the major hypothesis that life itself originated at similar deep alkaline vents, based on replicable chemistry that naturally creates the necessary hydrogen ion gradients. The segment concludes with the Ordovician mass extinction (444 million years ago), the first of the "big five" mass extinctions, which was caused by global cooling followed by rapid warming, stressing marine life with a high rate of climate change.
51575 에피소드
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