Melchin Michael (15 results)

- Softcover
Seller: Revaluation Books, Exeter, United KingdomRevaluation Books
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Paperback. Condition: Brand New. 81 pages. 11.00x8.50x0.19 inches. In Stock.
Published by The Palaeontological Association, 1998
- Softcover
Seller: Eryops Books, Stephenville, TX, U.S.A.Eryops Books
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Add to basketNo Binding. Condition: Very Good. ORIGINAL 1998 Article, disbound from journal; no covers; in very good condition. Journal.
Published by The Palaeontological Association, 1998
- Softcover
Seller: Eryops Books, Stephenville, TX, U.S.A.Eryops Books
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Add to basketNo Binding. Condition: Very Good. ORIGINAL 1998 Article, disbound from journal; no covers; in very good condition. Journal.

What Does Graptolite Origination and Extinction Reveal about the Cause of the Late Ordovician Mass Extinction?
Charles E. Mitchell, H. David Sheets, Michael J. Melchin, Chris Holmden
- Softcover
Seller: Rarewaves.com USA, London, LONDO, United KingdomRarewaves.com USA
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Paperback. Condition: New. Assesses the macroevolutionary turnover of paleotropical planktic graptolites during the Late Ordovician Mass Extinction (LOME) via automated sequencing and capture-mark-recapture modeling. Graptolites exhibited a succession of turnover pulses (sensu Elizabeth Vrba) that were coincident with the main phases of the Hirnantian glaciation and during which the Diplograptina experienced declining metapopulation size, elevated extinction, zero species originations, and ultimately, complete extermination. Concurrently, the Neograptina (latest Katian temperate zone immigrants) exhibit pulses of both extinction and adaptive radiation. Thus, the LOME involved intense species selection and the wholesale alteration of the clade diversity structure of a major element of the zooplankton. The LOME is unlikely to have been a direct effect of ocean anoxia or sampling bias but rather resulted from Hirnantian climate change, which altered nutrient supplies and plankton community compositions along with ecological displacement and loss of habitat that together drove the succession of turnover pulses. This title is also available as open access on Cambridge Core.…

- Softcover
Seller: Revaluation Books, Exeter, United KingdomRevaluation Books
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Paperback. Condition: Brand New. 88 pages. 6.00x0.18x9.00 inches. In Stock.

What Does Graptolite Origination and Extinction Reveal about the Cause of the Late Ordovician Mass Extinction? (Elements of Paleontology)
Mitchell, Charles E. Charles E. Mitchell, H. David Sheets, Michael J. Melchin, Chris Holmden,
- Softcover
Seller: Chiron Media, Wallingford, United KingdomChiron Media
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paperback. Condition: New.

- Softcover
Seller: Revaluation Books, Exeter, United KingdomRevaluation Books
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Paperback. Condition: Brand New. 88 pages. 6.00x0.18x9.00 inches. In Stock.

What Does Graptolite Origination And Extinction Reveal About The Cause Of The Late Ordovician Mass Extinction?
Mitchell, Charles E.; Sheets, H. David; Melchin, Michael J.; Holmden, Chris
- Hardcover
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What Does Graptolite Origination and Extinction Reveal about the Cause of the Late Ordovician Mass Extinction?
Charles E. Mitchell, H. David Sheets, Michael J. Melchin, Chris Holmden
- Hardcover
Seller: Rarewaves.com USA, London, LONDO, United KingdomRarewaves.com USA
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Hardback. Condition: New. Assesses the macroevolutionary turnover of paleotropical planktic graptolites during the Late Ordovician Mass Extinction (LOME) via automated sequencing and capture-mark-recapture modeling. Graptolites exhibited a succession of turnover pulses (sensu Elizabeth Vrba) that were coincident with the main phases of the Hirnantian glaciation and during which the Diplograptina experienced declining metapopulation size, elevated extinction, zero species originations, and ultimately, complete extermination. Concurrently, the Neograptina (latest Katian temperate zone immigrants) exhibit pulses of both extinction and adaptive radiation. Thus, the LOME involved intense species selection and the wholesale alteration of the clade diversity structure of a major element of the zooplankton. The LOME is unlikely to have been a direct effect of ocean anoxia or sampling bias but rather resulted from Hirnantian climate change, which altered nutrient supplies and plankton community compositions along with ecological displacement and loss of habitat that together drove the succession of turnover pulses. This title is also available as open access on Cambridge Core.…

What Does Graptolite Origination And Extinction Reveal About The Cause Of The Late Ordovician Mass Extinction?
Mitchell, Charles E.; Sheets, H. David; Melchin, Michael J.; Holmden, Chris
- Hardcover
Seller: GreatBookPrices, Columbia, MD, U.S.A.GreatBookPrices
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What Does Graptolite Origination And Extinction Reveal About The Cause Of The Late Ordovician Mass Extinction?
Mitchell, Charles E.; Sheets, H. David; Melchin, Michael J.; Holmden, Chris
- Hardcover
Seller: GreatBookPricesUK, Woodford Green, United KingdomGreatBookPricesUK
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Condition: New.

What Does Graptolite Origination And Extinction Reveal About The Cause Of The Late Ordovician Mass Extinction?
Mitchell, Charles E.; Sheets, H. David; Melchin, Michael J.; Holmden, Chris
- Hardcover
Seller: GreatBookPricesUK, Woodford Green, United KingdomGreatBookPricesUK
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Condition: As New. Unread book in perfect condition.

What Does Graptolite Origination and Extinction Reveal about the Cause of the Late Ordovician Mass Extinction?
Charles E. Mitchell, H. David Sheets, Michael J. Melchin, Chris Holmden
- Softcover
Seller: Rarewaves.com UK, London, United KingdomRarewaves.com UK
Contact seller5-star sellerCondition: New
US$ 30.43
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Paperback. Condition: New. Assesses the macroevolutionary turnover of paleotropical planktic graptolites during the Late Ordovician Mass Extinction (LOME) via automated sequencing and capture-mark-recapture modeling. Graptolites exhibited a succession of turnover pulses (sensu Elizabeth Vrba) that were coincident with the main phases of the Hirnantian glaciation and during which the Diplograptina experienced declining metapopulation size, elevated extinction, zero species originations, and ultimately, complete extermination. Concurrently, the Neograptina (latest Katian temperate zone immigrants) exhibit pulses of both extinction and adaptive radiation. Thus, the LOME involved intense species selection and the wholesale alteration of the clade diversity structure of a major element of the zooplankton. The LOME is unlikely to have been a direct effect of ocean anoxia or sampling bias but rather resulted from Hirnantian climate change, which altered nutrient supplies and plankton community compositions along with ecological displacement and loss of habitat that together drove the succession of turnover pulses. This title is also available as open access on Cambridge Core.…

- Hardcover
Seller: Revaluation Books, Exeter, United KingdomRevaluation Books
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US$ 130.80
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Hardcover. Condition: Brand New. 88 pages. 6.00x0.25x9.00 inches. In Stock.

What Does Graptolite Origination and Extinction Reveal about the Cause of the Late Ordovician Mass Extinction?
Charles E. Mitchell, H. David Sheets, Michael J. Melchin, Chris Holmden
- Hardcover
Seller: Rarewaves.com UK, London, United KingdomRarewaves.com UK
Contact seller5-star sellerCondition: New
US$ 89.53
US$ 87.03 shippingShips from United Kingdom to U.S.A.Quantity: Over 20 available
Hardback. Condition: New. Assesses the macroevolutionary turnover of paleotropical planktic graptolites during the Late Ordovician Mass Extinction (LOME) via automated sequencing and capture-mark-recapture modeling. Graptolites exhibited a succession of turnover pulses (sensu Elizabeth Vrba) that were coincident with the main phases of the Hirnantian glaciation and during which the Diplograptina experienced declining metapopulation size, elevated extinction, zero species originations, and ultimately, complete extermination. Concurrently, the Neograptina (latest Katian temperate zone immigrants) exhibit pulses of both extinction and adaptive radiation. Thus, the LOME involved intense species selection and the wholesale alteration of the clade diversity structure of a major element of the zooplankton. The LOME is unlikely to have been a direct effect of ocean anoxia or sampling bias but rather resulted from Hirnantian climate change, which altered nutrient supplies and plankton community compositions along with ecological displacement and loss of habitat that together drove the succession of turnover pulses. This title is also available as open access on Cambridge Core.…