Vertebrate land invasion - wikipedia Vertebrate land invasion It has been suggested that this article be merged with Evolution of tetrapods. ( Discuss ) Proposed since June 2016. This article has multiple issues. Please help improve it or discuss these issues on the talk page. ( Learn how and when to remove these template messages ) This article needs more links to other articles to help integrate it into the encyclopedia. Please help improve this article by adding links that are relevant to the context within the existing text. ( April 2015 ) This article includes a list of references, but its sources remain unclear because it has insufficient inline citations. Please help to improve this article by introducing more precise citations. ( May 2015 ) This article may be too technical for most readers to understand. Please help improve it to make it understandable to non-experts, without removing the technical details. The talk page may contain suggestions. ( May 2015 ) The aquatic to terrestrial transition of vertebrate organisms occurred in the late Devonian era and was an important step in the evolutionary history of modern land vertebrates. The transition allowed animals to escape competitive pressure from the water and explore niche opportunities on land. Fossils from this period have allowed scientists to identify some of the species that existed during this transition, such as Tiktaalik and Acanthostega. Many of these species were also the first to develop adaptations suited to terrestrial over aquatic life, such as neck mobility and hindlimb locomotion. The late Devonian vertebrate transition was not the only terrestrial invasion in evolutionary history. The vertebrate transition was preceded by the plant and invertebrate terrestrial invasion. These invasions allowed for the appropriate niche development that would ultimately facilitate the vertebrate invasion. Furthermore, the late Devonian event is only significant in that it was the first land invasion by vertebrate organisms, and that it resulted in an explosion of vertebrate biodiversity due to the many different niches that these species were able to exploit. However, aquatic species have continued to develop adaptations suited to terrestrial life ( and vice versa ) from the late Devonian to the Holocene. Contents 1 Overview of transition 2 Evolutionary timeline 3 Driving factors 3.1 Evolutionary pushes 3.2 Evolutionary pulls 4 Barriers to transition 4.1 Sensory systems 4.2 Homeostasis 4.3 Anatomy 4.4 Behaviour 5 Notable adaptations 5.1 Placement of eyes on head 5.2 Head and neck mobility 5.3 Fused sacrum 5.4 Lost adaptations 6 Future invasions 7 References Overview of transition The vertebrate species that were important to the initial water to land transition can be qualified as being one of five groups : Sarcopterygian fishes, prototetrapods, aquatic tetrapods, true tetrapods, and terrestrial tetrapods. Many morphological changes occurred throughout this transition. Mechanical support structures changed from fins to limbs, the method of locomotion changed from swimming to walking, respiratory structures changed from gills to lungs, feeding mechanisms changed from suction feeding to biting, and mode of reproduction changed from larval development to metamorphosis. Evolutionary timeline Lungfish appeared approximately 400 million years ago. It is a species that endured rapid evolution during the Devonian era, which became known as the dipnoan renaissance. The Acanthostega species, known as the fish with legs, is considered a tetrapod by structural findings but is postulated to have perhaps never left the aquatic environment. Its legs are not well - suited to support its weight. The bones of its forearm, the radius and ulna, are very thin at the wrist and also unable to support it on land. It also lacks a sacrum and strong ligaments at the hip, which would be integral to supporting the animal against gravity. In this sense, the species is considered a tetrapod but not one that has adapted well enough to walk on land. Furthermore, its gill bars have a supportive brace characterized for use as an underwater ear because it can pick up noise vibrations through the water. Tetrapods that adapted to terrestrial living adapted these gill bones to pick up sounds through air, and they later became the middle ear bones seen in mammalian tetrapods. Ichthyostega, on the other hand, is considered to be a fully terrestrial tetrapod that perhaps depended on water for its aquatic young. Comparisons between the skeletal features of Acanthostega and Ichthyostega reveal that they had different habits. Acanthostega is likely exclusive to an aquatic environment, while Ichthyostega is progressed in the aquatic to terrestrial transition by living dominantly on the shores. An evolutionary timeline of the late Devonian vertebrate terrestrial invasion demonstrates the changes that took place. A group of fish from the Givetian stage began developing limbs, and eventually evolved into aquatic tetrapods in the Famennian stage. Pederpes, Westlothiana, Protogyrinus, and Crassigyrinus descended from these species into the carboniferous period and were the first land vertebrates. A particularly important transitional species is one known as Tiktaalik. It has a fin, but interestingly the fin has bones within it that are similar to mammalian tetrapods. It has an upper arm bone, a lower arm bone, forearm bones, a wrist, and fingerlike projections. Essentially, it is a fin that can support the animal. Similarly, it also has a neck that allows independent head movement from the body. Its ribs are also able to support the body in gravity. Its skeletal features exhibit its ability as a fish that can live in shallow water and also venture onto land. Driving factors It took many millions of years for vertebrates to transition out of water onto land. During this time, both the competitive pressures that would push species out of the water and the niche occupation incentives that would pull species onto land were slowly building. The culmination of these driving factors are what ultimately facilitated the vertebrate transition. Evolutionary pushes Scientists believe that a long period of time where biotic and abiotic factors in the aquatic environment were unfavourable to a subset of aquatic organisms is what initiated their transition to shallower waters. Some of these push factors are environmental hypoxia, unfavourable aquatic temperatures, and increased salinity. Other constantly present factors such as predation, competition, waterborne diseases and parasites also contributed to the transition. A theory put forth by Joseph Barrell possibly helps explain what may have initiated these push factors to become relevant in the late Devonian. The extensive oxidized sediments that were present in Europe and North America during the late Devonian are evidence of severe droughts during this time. These droughts would cause small ponds and lakes to dry out, forcing certain aquatic organisms to move on land to find other bodies of water. Natural selection on these organisms eventually led to the evolution of the first terrestrial vertebrates. Evolutionary pulls The pull factors were secondary to the push factors, and only became significant once the pressures to leave the aquatic environment became significant. These were largely the niches and opportunities that were available for exploitation in the terrestrial environment, and include higher environmental oxygen partial pressures, favourable temperatures, and the lack of competitors and predators on land. The plants and invertebrates that had preceded the vertebrate invasion also provided opportunities in the form of abundant prey and lack of predators. Barriers to transition There were many challenges that the first land vertebrates faced. These challenges allowed for rapid natural selection and niche domination, resulting in an adaptive radiation that produced many different vertebrate land species in a relatively short period of time. Sensory systems Depending on the water depth at which a species lives, the visual perception of many aquatic species is better suited to darker environments than those on land. Similarly, hearing in aquatic organisms is better optimized for sounds underwater, where the speed and amplitude of sound is greater than in air. Homeostasis Homeostasis was almost definitely a challenge for land invading vertebrates. Gas exchange and water balance are highly different in water and in air. Homeostasis mechanisms suitable for a terrestrial environment may have been necessary to develop before these organisms invaded land. Anatomy The primary anatomical barrier is the development of lungs for proper gas exchange, however other anatomical barriers also exist. The stressors of the musculoskeletal system are different in air than they are in water, and the muscles and bones must be strong enough to withstand the increased effects of gravity on land. Behaviour Many behaviours, such as reproduction, are specifically optimized to a wet environment. Navigation and locomotion are also highly different in aquatic environments compared to terrestrial environments. Notable adaptations Placement of eyes on head The ancestral species of tetrapods that lived entirely in water had tall and narrow skulls with eyes facing sideways and forwards to maximize visibility for predators and prey in the aquatic environment. As the ancestors of early tetrapods started inhabiting shallower waters, these species had flatter skulls with eyes at the tops of their heads, which made it possible to spot food above them. Once the tetrapods transitioned onto land, the lineages evolved to have tall and narrow skulls with eyes facing sideways and forwards again. This allowed them to navigate through the terrestrial environment and look for predators and prey. Head and neck mobility Fish do not have necks, so the head is directly connected to the shoulders. In contrast, land animals use necks to move their heads so they can look down to see the food on the ground. The greater the mobility of the neck, the more visibility the land animal has. As lineages moved from completely aquatic environments to shallower waters and land, they gradually evolved vertebral columns that increased neck mobility. The first neck vertebra that evolved permitted the animals to have flexion and extension of the head so that they can see up and down. The second neck vertebra evolved to allow rotation of the neck for moving the head left and right. As tetrapod species continued to evolve on land, adaptations included seven or more vertebrae, allowing increasing neck mobility. Fused sacrum The sacrum connects the pelvis and hindlimbs and is useful for motion on land. The aquatic ancestors of tetrapods did not have a sacrum, so it was speculated to have evolved for locomotive function exclusive to terrestrial environments. However, the Acanthostega species is one of the earliest lineages to have a sacrum, even though it is a fully aquatic species. Once species moved onto land, the trait was adapted for terrestrial locomotion support, which is evidenced by additional vertebrae fusing similarly to permit additional support. This is an example of exaptation, where a trait performs a function that did not arise through natural selection for its current use. Lost adaptations As the lineages evolved to adapt to terrestrial environments, many lost traits that were better suited for the aquatic environment. Many lost their gills, which were only useful for obtaining oxygen in water. Their tail fins became smaller. They lost the lateral line system, a network of canals along the skull and jaw that are sensitive to vibration, which does not work outside of an aquatic environment. Future invasions For successful land invasion, the species had several pre-adaptations like air - breathing and limb - based locomotion. Aspects such as reproduction and swallowing, however, have bound these species to the aquatic environment. These pre-adaptations have allowed vertebrates to venture onto land hundreds of times, but were not able to accomplish the same degree of prolific radiation into diverse terrestrial species. To understand the potential of future invasions, studies must evaluate the models of evolutionary steps taken in past invasions. The commonalities to current and future invasions may then be elucidated to predict the effects of environmental changes. References ^ Jump up to : `` Tiktaalik roseae : Q&A Session with Neil Shubin ''. Tiktaalik.uchicago.edu. April 2006. Retrieved 7 April 2015. ^ Jump up to : Clack, Jennifer A. ( 2012 ). Gaining ground : the origin and evolution of tetrapods ( 2nd ed. ). Bloomington : Indiana University Press. ISBN 978 - 0 - 253 - 35675 - 8. ^ Jump up to : Ashley - Ross, M.A. ; Hsieh, S.T. ; Gibb, A.C. ; Blob, R.W. ( 9 May 2013 ). `` Vertebrate Land Invasions - Past, Present, and Future : An Introduction to the Symposium ''. Integrative and Comparative Biology. 53 ( 2 ) : 192 -- 196. PMID 23660589. doi : 10.1093 / icb / ict048. ^ Jump up to : Long, JA ; Gordon, MS ( September -- October 2004 ). `` The Greatest Step in Vertebrate History : A Paleobiological Review of the Fish ‐ Tetrapod Transition ''. Physiological and Biochemical Zoology. 77 ( 5 ) : 700 -- 719. PMID 15547790. doi : 10.1086 / 425183. ^ Jump up to : `` The origin of tetrapods ''. Evolution.berkeley.edu. Retrieved 7 April 2015. 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Question: when did amphibians begin to colonize land as the first terrestrial vertebrates
Answer: the late Devonian era