標題: Titlebook: Ammonoid Paleobiology: From macroevolution to paleogeography; Christian Klug,Dieter Korn,Royal H. Mapes Book 2015 Springer Science+Busines [打印本頁] 作者: estradiol 時間: 2025-3-21 17:37
書目名稱Ammonoid Paleobiology: From macroevolution to paleogeography影響因子(影響力)
書目名稱Ammonoid Paleobiology: From macroevolution to paleogeography影響因子(影響力)學科排名
書目名稱Ammonoid Paleobiology: From macroevolution to paleogeography網(wǎng)絡公開度
書目名稱Ammonoid Paleobiology: From macroevolution to paleogeography網(wǎng)絡公開度學科排名
書目名稱Ammonoid Paleobiology: From macroevolution to paleogeography被引頻次
書目名稱Ammonoid Paleobiology: From macroevolution to paleogeography被引頻次學科排名
書目名稱Ammonoid Paleobiology: From macroevolution to paleogeography年度引用
書目名稱Ammonoid Paleobiology: From macroevolution to paleogeography年度引用學科排名
書目名稱Ammonoid Paleobiology: From macroevolution to paleogeography讀者反饋
書目名稱Ammonoid Paleobiology: From macroevolution to paleogeography讀者反饋學科排名
作者: Fraudulent 時間: 2025-3-21 22:08
Biogeography of Triassic Ammonoidsas a marked differentiation between Tethys and Panthalassic realms. Biogeographical configurations of the Carnian, Norian and Rhaetian appear more homogeneous, although a weak latitudinal structuring may have continued up to the late Carnian.作者: Coterminous 時間: 2025-3-22 02:39
Macroevolution and Paleobiogeography of Jurassic-Cretaceous Ammonoidsvides the foundation for a model of ammonoid speciation in which sea level change provides new epeiric sea microhabitats into which ammonoids disperse while developmental flexibility provides the morphological and ecological variation to fuel divergence and speciation. New quantitative and geospatia作者: 賞心悅目 時間: 2025-3-22 07:58
Paleobiogeography of Late Cretaceous Ammonoidssented by varying taxa. Migration between the realms and provinces appears to be linked to changes of migration routes, triggered by sea level changes. At the end of the Cretaceous, provincialism disappears, preceding the extinction of the Ammonoids.作者: 血統(tǒng) 時間: 2025-3-22 08:53
Ammonoid Paleobiology: From macroevolution to paleogeography作者: depreciate 時間: 2025-3-22 16:35 作者: ABOUT 時間: 2025-3-22 19:16
https://doi.org/10.1007/978-3-322-85315-8as a marked differentiation between Tethys and Panthalassic realms. Biogeographical configurations of the Carnian, Norian and Rhaetian appear more homogeneous, although a weak latitudinal structuring may have continued up to the late Carnian.作者: Ornament 時間: 2025-3-22 23:31
https://doi.org/10.1007/978-3-322-85315-8vides the foundation for a model of ammonoid speciation in which sea level change provides new epeiric sea microhabitats into which ammonoids disperse while developmental flexibility provides the morphological and ecological variation to fuel divergence and speciation. New quantitative and geospatia作者: finale 時間: 2025-3-23 04:04 作者: 朋黨派系 時間: 2025-3-23 07:47
Book 2015of septa and the shell, we explore their habitats by the content of stable isotopes in their shells, we discuss the origin and later evolution of this important clade, and we deliver hypotheses on its demise. The Ammonoidea produced a great number of species that can be used in biostratigraphy and p作者: 小畫像 時間: 2025-3-23 12:17 作者: 強化 時間: 2025-3-23 14:59
https://doi.org/10.1007/978-3-642-91735-6atigraphical tools for this interval. The present time resolution in terms of ammonoid biostratigraphy is highest in the Devonian (one zone has a mean of 0.9?Ma) and in the Carboniferous (about 1?Ma), while the subdivision of the Permian is much coarser (about 2.5?Ma per ammonoid zone on average).作者: 簡潔 時間: 2025-3-23 18:52 作者: Lucubrate 時間: 2025-3-24 01:41
Paleozoic Ammonoid Biostratigraphyatigraphical tools for this interval. The present time resolution in terms of ammonoid biostratigraphy is highest in the Devonian (one zone has a mean of 0.9?Ma) and in the Carboniferous (about 1?Ma), while the subdivision of the Permian is much coarser (about 2.5?Ma per ammonoid zone on average).作者: misanthrope 時間: 2025-3-24 04:39 作者: 榮幸 時間: 2025-3-24 09:43 作者: 天然熱噴泉 時間: 2025-3-24 11:10 作者: 職業(yè)拳擊手 時間: 2025-3-24 14:59 作者: 喧鬧 時間: 2025-3-24 21:50
https://doi.org/10.1007/978-3-662-61436-5sic age produced an empirical morphospace this time interval. The morphospace of Paleozoic ammonoids shows some subtle changes between the periods, but generally, the occupied area is remarkably similar.作者: bifurcate 時間: 2025-3-25 02:16 作者: predict 時間: 2025-3-25 04:14 作者: Anthropoid 時間: 2025-3-25 07:38
,Rechte Winkel für runde R?ume,ges composed of different genera and families occur particularly in the Late Viséan, Serpukhovian and Bashkirian. Early Permian ammonoid provinces are latitudinally arranged, a separation of equatorial and boreal faunas is possible on the basis of major differences in family and genus compositions.作者: Peak-Bone-Mass 時間: 2025-3-25 15:29 作者: 高度表 時間: 2025-3-25 18:06
Einleitung und Problemstellung, Triassic recovery. Finally, Triassic ammonoids still have many properties to contribute to evolutionary biology, but going further now requires the construction of quantitative databases of the various morphological characters and reconstruction of Triassic ammonoid phylogeny.作者: 不開心 時間: 2025-3-25 22:39 作者: Herbivorous 時間: 2025-3-26 03:48 作者: Indolent 時間: 2025-3-26 05:19
https://doi.org/10.1007/978-3-322-85316-5the Albian stage, displays a more distinctive differentiation between Boreal and Tethyan faunas. The late Barremian marks the onset of the Austral Realm, originating from faunas that originally evolved in the Indo-Pacific Subrealm of the Tethyan Realm.作者: entice 時間: 2025-3-26 11:20 作者: 瑪瑙 時間: 2025-3-26 12:49
https://doi.org/10.1007/978-3-663-04642-4rest in Triassic ammonoid biozonation has occurred during the last few decades, leading to the recognition of tens of ammonoid zones spanning about 50.9?Myr (leading to an average duration for ammonoid biochronozones of about 0.74?Myr), whose correlation and definition are herein synthesized.作者: 大笑 時間: 2025-3-26 19:06
Evolutionary Trends of Triassic Ammonoids Triassic recovery. Finally, Triassic ammonoids still have many properties to contribute to evolutionary biology, but going further now requires the construction of quantitative databases of the various morphological characters and reconstruction of Triassic ammonoid phylogeny.作者: 退出可食用 時間: 2025-3-26 23:38
Buckman’s Rules of Covariationtion suggests that shell morphogenesis may not be random but constrained either by adaptive constraints or simple constructional scaling rules. The cause(s) remain debated. Hence, although Buckman’s rules of covariation are now widely documented and acknowledged, several aspects of their scope and limits still remain to be investigated.作者: 易彎曲 時間: 2025-3-27 03:23 作者: helper-T-cells 時間: 2025-3-27 07:17
Paleobiogeography of Early Cretaceous Ammonoidsthe Albian stage, displays a more distinctive differentiation between Boreal and Tethyan faunas. The late Barremian marks the onset of the Austral Realm, originating from faunas that originally evolved in the Indo-Pacific Subrealm of the Tethyan Realm.作者: insipid 時間: 2025-3-27 10:07 作者: crease 時間: 2025-3-27 16:06
Biostratigraphy of Triassic Ammonoidsrest in Triassic ammonoid biozonation has occurred during the last few decades, leading to the recognition of tens of ammonoid zones spanning about 50.9?Myr (leading to an average duration for ammonoid biochronozones of about 0.74?Myr), whose correlation and definition are herein synthesized.作者: 抱怨 時間: 2025-3-27 21:49 作者: Overthrow 時間: 2025-3-27 22:35 作者: COWER 時間: 2025-3-28 04:00 作者: 證明無罪 時間: 2025-3-28 07:10
Christian Klug,Dieter Korn,Royal H. MapesEnhances our understanding of ammonoids.Excellent reference book on this most important macroscopic group of index fossils.Reflects the panel of ammonoid workers present nowadays in academia Includes 作者: THROB 時間: 2025-3-28 14:20
Topics in Geobiologyhttp://image.papertrans.cn/a/image/154709.jpg作者: 故意釣到白楊 時間: 2025-3-28 15:54
https://doi.org/10.1007/978-3-662-26191-0the origin of bactritids as well as the origin of bactritids with their respective Bauplan characters. We also list major morphological changes that occurred between the origin of cephalopods until the early evolution of ammonoids.作者: 領(lǐng)先 時間: 2025-3-28 21:53
Einleitung und Problemstellung,uture line indented on the lobes only, the Triassic quasi-monophyletic clade shows a remarkable biostratigraphic and geographic record. However, very few studies have thoroughly investigated their evolutionary trends, except for taxonomic richness. Although Triassic ammonoids show a very large range作者: 無法治愈 時間: 2025-3-29 00:59
https://doi.org/10.1007/978-3-662-28988-4xamine trends among Jurassic ammonoids. First, a compilation of selected literature on evolutionary patterns and trends leads to the conclusion that such trends have rarely been studied among Jurassic ammonoids and even more rarely are they formally studied using statistical tests. Second, a prelimi作者: 側(cè)面左右 時間: 2025-3-29 06:39
https://doi.org/10.1007/978-3-662-28988-4any species, individuals range from slender, involute, compressed, and weakly ornamented forms to “robust” forms, which are more evolute, more depressed, and with coarser ornamentation. Additionally, more compressed shells tend to have more complex sutures. Within a species from a single sample, the作者: 凝乳 時間: 2025-3-29 10:02 作者: 灌輸 時間: 2025-3-29 11:57
,Rechte Winkel für runde R?ume,intervals of well-expressed provincialism. The Devonian appears to be a time with general cosmopolitanism with a slowly increasing differentiation of ammonoid provinces by increasing endemism of cosmopolitan genera. In the Carboniferous, clearly separated provinces characterized by ammonoid assembla作者: 過時 時間: 2025-3-29 16:29
https://doi.org/10.1007/978-3-322-85315-8 associated with sudden biogeographic changes often closely related to major climatic and oceanographic changes. Previous biogeographic studies of Triassic ammonoids have rarely focused on a specific time-interval and were rarely based on quantitative methods. Thus, we will first review biogeographi作者: 共同生活 時間: 2025-3-29 23:05 作者: abolish 時間: 2025-3-30 01:23 作者: Felicitous 時間: 2025-3-30 06:34
Risikokonflikte und Wertwandel,stribution. Their paleobiogeographic distributions were influenced by changing continental positions, currents, sea level change, and perhaps by their mode of life as reflected in the evolution of many diverse lineages of heteromorphic, possibly rather vertically migrating than horizontally swimming作者: Erythropoietin 時間: 2025-3-30 09:22
https://doi.org/10.1007/978-3-642-91735-6zoic and Mesozoic marine strata. Originations and extinctions of ammonoid species are commonly used to define GSSPs and build high resolution biozonations. Biochronology is now an advanced field with the recent development of computerized, quantitative methods yielding robust biochronological scheme作者: shrill 時間: 2025-3-30 15:51
https://doi.org/10.1007/978-3-642-91735-6volution is reflected by the establishment of a detailed biostratigraphical scheme. Ammonoids are, together with the conodonts, the most important stratigraphical tools for this interval. The present time resolution in terms of ammonoid biostratigraphy is highest in the Devonian (one zone has a mean作者: 單挑 時間: 2025-3-30 19:36 作者: 傳授知識 時間: 2025-3-31 00:20 作者: 逃避責任 時間: 2025-3-31 03:55
A?– wie Akklimatisierung und Anpassungspecies. Concepts of Cretaceous ammonite biostratigraphy are briefly discussed and characteristic examples of the types of zones and ammonite events are given. Furthermore, accomplishments and limits of ammonite biostratigraphy are presented, including aspects of evolution, preservational modes and 作者: CREEK 時間: 2025-3-31 06:34
https://doi.org/10.1007/978-3-662-61436-5interval from the Early Devonian through to the Triassic has seen ammonoid groups evolve and become extinct. The evolutionary history of the Paleozoic ammonoids was punctuated by some extinction events with near extinction events and subsequent recoveries. A Principal Components Analysis (PCA) based作者: 粘土 時間: 2025-3-31 10:29
https://doi.org/10.1007/978-94-017-9633-0Ammonoids; Diversity; Macroevolution; Paleogeography; Taphonomy; Model invertebrates作者: 異端 時間: 2025-3-31 16:14
978-94-024-0435-7Springer Science+Business Media Dordrecht 2015作者: lambaste 時間: 2025-3-31 21:15
