Translation of "phanerozoic" to Portuguese language:
Examples (External sources, not reviewed)
| Alexander V. Markov, and Andrey V. Korotayev (2007) Phanerozoic marine biodiversity follows a hyperbolic trend Palaeoworld 16(4) pp. | Alexander V. Markov, Andrey V. Korotayev Phanerozoic marine biodiversity follows a hyperbolic trend Palaeoworld 16 4 (2007) pp. |
| This is because many Precambrian rocks have been heavily metamorphosed, obscuring their origins, while others have been destroyed by erosion, or remain deeply buried beneath Phanerozoic strata. | Isso ocorre porque muitas rochas Pré cambrianas foram fortemente metamorfoseadas, obscurecendo suas origens, enquanto outras foram destruídos pela erosão ou permanecem profundamente enterrados sob estratos do Fanerozóico. |
| Geographical data from Sinop Geological formation non folded covers the Phanerozoic and Quaternary basin of the Upper Xingu Relief and altitude Residual Northern Plateau and Mato Grosso Plateau Parecis. | Dados geográficos de Sinop Formação Geológica coberturas não dobradas do Fanerozoico e Bacia Quaternária do Alto Xingu Relevo e altitude Planalto Residual Norte de Mato Grosso e Planalto do Parecis. |
| Classically, the boundary between the Proterozoic and the Phanerozoic eons was set at the base of the Cambrian Period when the first fossils of animals including trilobites and archeocyathids appeared. | Tradicionalmente, a fronteira entre o Proterozoico e o Fanerozoico foi colocada na base do Câmbrico, quando os primeiros fósseis de trilobites e Archaeocyatha apareceram. |
| The Precambrian (or Pre Cambrian sometimes abbreviated pЄ) is the largest span of time in Earth's history before the current Phanerozoic Eon, and is a Supereon divided into several eons of the geologic time scale. | O Pré cambriano (ou Pré Câmbrico) é o grande período de tempo na história da Terra antes do atual Éon Fanerozóico, e é um Superéon dividido em vários éons da escala de tempo geológico. |
| The Precambrian is so named because it precedes the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the classical name for Wales, where rocks from this age were first studied. | O Pré cambriano é assim chamado porque precede o Cambriano, o primeiro período do Éon Fanerozóico, que é nomeado após Cambria, o nome clássico para o País de Gales, onde as rochas dessa idade foram estudadas pela primeira vez. |
| Further, the conventional view that all the phyla arose in the Cambrian is flawed while the phyla may have diversified in this time period, representatives of the crown groups of many phyla do not appear until much later in the Phanerozoic. | Further, the conventional view that all the phyla arose in the Cambrian is flawed whilst the phyla may have diversified in this time period, representatives of the crown groups of many phyla do not appear until much later in the Phanerozoic. |
| However, animals are not affected when similar oceanographic conditions occur in the Phanerozoic there is no convincing correlation between oxygen levels and evolution, so oxygen may have been no more a prerequisite to complex life than liquid water or primary productivity. | However, animals are not affected when similar oceanographic conditions occur in the Phanerozoic there is no convincing correlation between oxygen levels and evolution, so oxygen may have been no more a prerequisite to complex life than liquid water or primary productivity. |
| Most geologists and paleontologists would probably set the Proterozoic Phanerozoic boundary either at the classic point where the first trilobites and reef building animals (archaeocyatha) such as corals and others appear at the first appearance of a complex feeding burrow called Treptichnus pedum or at the first appearance of a group of small, generally disarticulated, armored forms termed 'the small shelly fauna'. | A maioria dos geólogos e paleontólogos provavelmente consideraria que a fronteira Fanerozoico Proterozoico ocorre no ponto clássico em que surgem as primeiras trilobites e Archaeocyatha com a primeira aparição de complexas tocas de alimentação ( Trichophycus pedum ) ou com a primeira aparição de um grupo de pequenas e geralmente desarticuladas formas couraçadas designadas 'pequena fauna conquífera'. |
