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## Hotspot
### Text
HotspotPanoramaOverlayTextImage_1C79E4BE_0EAF_CBEE_41AC_E4D71691A7D1.text = DESCUBRA A JAZIDA PALEONTOLÓGICA |
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### Popup Image
### Title
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## Popup
### Body
htmlText_B6C06D5E_AF67_D4D4_41C0_C917A3BB388A.html = A CAMADA DAS PEGADAS |
THE FOOTPRINTS LAYER
A camada onde se encontram preservadas as pegadas, é constituída por calcário margoso e está numa posição sub-horizontal. A sua superfície é irregular devido à passagem de vários dinossauros, provocando um distúrbio da camada sedimentar, pelo movimento destes animais, indicando assim uma atividade de pisoteamento pelos dinossauros, denominada de “dinoturbação”. As pegadas estão dispostas regularmente, segundo uma direção preferencial (sensivelmente de norte para sul). Estas pegadas foram feitas por dinossáurios saurópodes, provavelmente por diplodocídeos ou titanossaurídeos, estes últimos, muito comuns no Cretácico.
The layer where the footprints are preserved, consists of marly limestone and is in a sub-horizontal position. Its surface is irregular due to the passage of several dinosaurs, causing a disturbance of the sedimentary layer by the movement of these animals, thus indicating a trampling activity by dinosaurs, called "dinoturbation". The tracks are arranged regularly, according to a preferential direction (roughly from north to south). These tracks were made by sauropod dinosaurs, probably by diplodocids or titanosaurids, the latter very common in the Cretaceous.
JAZIDA PALEONTOLÓGICA DA PRAIA DA PAREDE |
PALEONTOLOGICAL SITE OF PRAIA DA PAREDE
Na Praia da Parede (São Pedro do Estoril) são visíveis, na zona intermareal (entre marés), várias pegadas de dinossauros saurópodes, impressas numa camada localizada junto ao mar, numa área frequentemente coberta por areia. Esta camada de calcário fossilífero (com fósseis) foi formada no final do Cretácico Inferior, num ambiente marinho de maré de baixa energia, num baixio, aberto a condições marinhas. Nas diferentes camadas da Praia da Parede foram encontrados diversos fósseis de animais marinhos (peixes, búzios e bivalves) que ali viviam há cerca de 100 - 105 milhões de anos. Alguns destes animais já estão extintos, como é o caso dos bivalves rudistas, outros, como é o caso dos pectinídeos, grupo a que pertencem as atuais vieiras, ainda subsistem.
At Praia da Parede (São Pedro do Estoril), several sauropod dinosaur tracks are visible in the intertidal zone (between tides), imprinted on a layer located near the sea, in an area often covered by sand. This layer of fossiliferous limestone (with fossils) was formed at the end of the Lower Cretaceous, in a low-energy tidal environment, in a shallow, open to marine conditions. In the different layers of Praia da Parede several fossils have been found of marine animals (fish, whelks and bivalves) that lived there about 100 - 105 million years ago. Some of these animals are already extinct, such as the ruddy bivalves, while others, such as the pectinids, the group to which the current scallops belong, still survive.
OS DINOSSÁURIOS DA PRAIA DA PAREDE |
THE PRAIA DA PAREDE DINOSAURS
Os saurópodes eram o grupo dos famosos e gigantescos dinossáurios herbívoros, de caudas e pescoços longos e flexíveis e a cabeça pequena. Foram os maiores animais que alguma vez pisaram a Terra. As mandíbulas apresentavam dentes tubulares e lisos. O corpo era maciço e sustentado pelas quatro patas, que funcionavam como se fossem autênticos pilares. Sendo tão grandes, estes animais necessitavam de ingerir muito alimento; comparativamente, ocupavam o lugar que os elefantes ocupam nas faunas atuais. Tal como estes, ou por certo ainda mais, devem ter devastado grandes áreas de floresta. Os pescoços compridos davam-lhes a vantagem de chegar às folhas das partes mais altas das árvores, inacessíveis a outros dinossáurios herbívoros. Como grupo foram bastante bem-sucedidos e viveram em quase todas as massas de terra emersas do planeta desde o Jurássico Inferior até ao final do Cretácico.
The sauropods were the group of the famous, gigantic, herbivorous dinosaurs, with long, flexible tails and necks and small head. They were the largest animals that ever walked the Earth. Their jaws had smooth, tubular teeth. The body was massive and supported by four legs, which worked as if they were authentic pillars. Being so large, these animals needed to ingest a lot of food; comparatively, they occupied the place that elephants occupy in today's faunas. Like them, or certainly even more, they must have devastated large areas of forest. Their long necks gave them the advantage of reaching the leaves on the highest parts of the trees, inaccessible to other herbivorous dinosaurs. As a group they were quite successful and lived on almost every emersed land mass on the planet from the Lower Jurassic to the end of the Cretaceous.