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Other plants that colonised the sea, such as [[salt marsh]] plants, [[mangrove]]s, and [[marine algae]], have more diverse evolutionary lineages. In spite of their low species diversity, seagrasses have succeeded in colonising the continental shelves of all continents except Antarctica.<ref>{{Cite journal|doi = 10.1641/0006-3568(2006)56[987:AGCFSE]2.0.CO;2|issn = 0006-3568|year = 2006|volume = 56|page = 987|title = A Global Crisis for Seagrass Ecosystems|last1 = Orth|first1 = Robert J.|last2 = Carruthers|first2 = TIM J. B.|last3 = Dennison|first3 = William C.|last4 = Duarte|first4 = Carlos M.|last5 = Fourqurean|first5 = James W.|last6 = Heck|first6 = Kenneth L.|last7 = Hughes|first7 = A. Randall|last8 = Kendrick|first8 = Gary A.|last9 = Kenworthy|first9 = W. Judson|last10 = Olyarnik|first10 = Suzanne|last11 = Short|first11 = Frederick T.|last12 = Waycott|first12 = Michelle|last13 = Williams|first13 = Susan L.|journal = BioScience|issue = 12}}</ref>
Other plants that colonised the sea, such as [[salt marsh]] plants, [[mangrove]]s, and [[marine algae]], have more diverse evolutionary lineages. In spite of their low species diversity, seagrasses have succeeded in colonising the continental shelves of all continents except Antarctica.<ref>{{Cite journal|doi = 10.1641/0006-3568(2006)56[987:AGCFSE]2.0.CO;2|issn = 0006-3568|year = 2006|volume = 56|page = 987|title = A Global Crisis for Seagrass Ecosystems|last1 = Orth|first1 = Robert J.|last2 = Carruthers|first2 = TIM J. B.|last3 = Dennison|first3 = William C.|last4 = Duarte|first4 = Carlos M.|last5 = Fourqurean|first5 = James W.|last6 = Heck|first6 = Kenneth L.|last7 = Hughes|first7 = A. Randall|last8 = Kendrick|first8 = Gary A.|last9 = Kenworthy|first9 = W. Judson|last10 = Olyarnik|first10 = Suzanne|last11 = Short|first11 = Frederick T.|last12 = Waycott|first12 = Michelle|last13 = Williams|first13 = Susan L.|journal = BioScience|issue = 12}}</ref>

Around 140 million years ago, seagrasses evolved from early monocotyledonous land plants, which succeeded in conquering the marine environment. Today, they are a polyphyletic group of marine angiosperms with around 60 species in five families (Zosteraceae, Hydrocharitaceae, Posidoniaceae, Cymodoceaceae, and Ruppiaceae), which belong to the order Alismatales according to the [[Angiosperm Phylogeny Group]] IV System.<ref>{{cite journal |doi = 10.1111/boj.12385|title = An update of the Angiosperm Phylogeny Group classification for the orders and families of flowering plants: APG IV|journal = Botanical Journal of the Linnean Society|year = 2016|volume = 181|pages = 1–20}}</ref> The genus Ruppia, which occurs in brackish water, is not regarded as a “real” seagrass by all authors and has been shifted to the Cymodoceaceae by some authors.<ref>{{Cite book|url=https://books.google.com/books?id=sEfKwaRHQj4C&q=In+time+and+with+water.the+systematics+of+alismatid+monocotyledons&pg=PA118|title=Early Events in Monocot Evolution|isbn=9781107244603|last1=Wilkin|first1=Paul|last2=Mayo|first2=Simon J.|date=30 May 2013}}</ref> The APG IV System and The Plant List Webpage<ref>The Plant List (2020). Ruppia. Available online at: http://www.theplantlist.org/1.1/browse/A/Ruppiaceae/Ruppia/ (accessed September 22, 2020).</ref> do not share this family assignment.<ref name=Pfeifer2020>{{cite journal |doi = 10.3389/fpls.2020.588754|title = The Cell Wall of Seagrasses: Fascinating, Peculiar and a Blank Canvas for Future Research|year = 2020|last1 = Pfeifer|first1 = Lukas|last2 = Classen|first2 = Birgit|journal = Frontiers in Plant Science|volume = 11|page = 588754|pmid = 33193541|pmc = 7644952}}</ref>

Seagrasses form important coastal ecosystems.<ref>Hemminga, M. A., and Duarte, C. M. eds (2000). “Seagrasses in the human environment,” in Seagrass Ecology (Cambridge: Cambridge University Press), 248–291.</ref> The worldwide endangering of these sea meadows, which provide food and habitat for many marine species, prompts the need for protection and understanding of these valuable resources. Recently, sequencing of the genomes of Zostera marina and Zostera muelleri allowed better understanding angiosperm adaption to the sea.<ref name=Lee2016>{{cite journal |doi = 10.1104/pp.16.00868|title = The Genome of a Southern Hemisphere Seagrass Species (Zostera muelleri)|year = 2016|last1 = Lee|first1 = Hueytyng|last2 = Golicz|first2 = Agnieszka A.|last3 = Bayer|first3 = Philipp E.|last4 = Jiao|first4 = Yuannian|last5 = Tang|first5 = Haibao|last6 = Paterson|first6 = Andrew H.|last7 = Sablok|first7 = Gaurav|last8 = Krishnaraj|first8 = Rahul R.|last9 = Chan|first9 = Chon-Kit Kenneth|last10 = Batley|first10 = Jacqueline|last11 = Kendrick|first11 = Gary A.|last12 = Larkum|first12 = Anthony W.D.|last13 = Ralph|first13 = Peter J.|last14 = Edwards|first14 = David|journal = Plant Physiology|volume = 172|issue = 1|pages = 272–283|pmid = 27373688|pmc = 5074622}}</ref><ref name=Olsen2016>{{cite journal |doi = 10.1038/nature16548|title = The genome of the seagrass Zostera marina reveals angiosperm adaptation to the sea|year = 2016|last1 = Olsen|first1 = Jeanine L.|last2 = Rouzé|first2 = Pierre|last3 = Verhelst|first3 = Bram|last4 = Lin|first4 = Yao-Cheng|last5 = Bayer|first5 = Till|last6 = Collen|first6 = Jonas|last7 = Dattolo|first7 = Emanuela|last8 = De Paoli|first8 = Emanuele|last9 = Dittami|first9 = Simon|last10 = Maumus|first10 = Florian|last11 = Michel|first11 = Gurvan|last12 = Kersting|first12 = Anna|last13 = Lauritano|first13 = Chiara|last14 = Lohaus|first14 = Rolf|last15 = Töpel|first15 = Mats|last16 = Tonon|first16 = Thierry|last17 = Vanneste|first17 = Kevin|last18 = Amirebrahimi|first18 = Mojgan|last19 = Brakel|first19 = Janina|last20 = Boström|first20 = Christoffer|last21 = Chovatia|first21 = Mansi|last22 = Grimwood|first22 = Jane|last23 = Jenkins|first23 = Jerry W.|last24 = Jueterbock|first24 = Alexander|last25 = Mraz|first25 = Amy|last26 = Stam|first26 = Wytze T.|last27 = Tice|first27 = Hope|last28 = Bornberg-Bauer|first28 = Erich|last29 = Green|first29 = Pamela J.|last30 = Pearson|first30 = Gareth A.|journal = Nature|volume = 530|issue = 7590|pages = 331–335|pmid = 26814964|bibcode = 2016Natur.530..331O|s2cid = 3713147|display-authors = 1}}</ref> During the evolutionary step back to the ocean, different genes have been lost (e.g., stomatal genes) or have been reduced (e.g., genes involved in the synthesis of terpenoids) and others have been regained, such as in genes involved in sulfation.<ref name=Olsen2016 /><ref name=Pfeifer2020 />

Genome information further revealed that adaption to the marine habitat was accomplished by severe changes of cell wall composition.<ref name=Lee2016 /><ref name=Olsen2016 /> On the other hand, the cell walls of seagrasses are poorly understood. Beside ancestral traits of land plants, one would anticipate a habitat-driven adaption process to the new environment, which is characterized by multiple abiotic (high amounts of salt) and biotic (different seagrass grazers and bacterial colonization) stressors.<ref name=Pfeifer2020 /> The cell walls of seagrasses seem to be fascinating combinations of features known from both angiosperm land plants and marine macroalgae with new structural elements.<ref name=Pfeifer2020 />


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Revision as of 08:42, 11 March 2021

Zostera marina is the most abundant seagrass species in the Northern Hemisphere

Seagrasses are the only flowering plants which grow in marine environments. There are about 60 species of fully marine seagrasses which belong to four families (Posidoniaceae, Zosteraceae, Hydrocharitaceae and Cymodoceaceae), all in the order Alismatales (in the class of monocotyledons).[1] Seagrasses evolved from terrestrial plants which recolonised the ocean 70 to 100 million years ago.

The name seagrass stems from the many species with long and narrow leaves, which grow by rhizome extension and often spread across large "meadows" resembling grassland; many species superficially resemble terrestrial grasses of the family Poaceae.

Like all autotrophic plants, seagrasses photosynthesize, in the submerged photic zone, and most occur in shallow and sheltered coastal waters anchored in sand or mud bottoms. Most species undergo submarine pollination and complete their life cycle underwater.

Seagrasses form dense underwater seagrass meadows which are among the most productive ecosystems in the world. They function as important carbon sinks and provide habitats and food for a diversity of marine life comparable to that of coral reefs.

Evolution

Evolution of seagrass
Showing the progression onto land from marine origins, the diversification of land plants and the subsequent return to the sea by the seagrasses.

Terrestrial plants evolved perhaps as early as 450 million years ago from a group of green algae.[2] Seagrasses then evolved from terrestrial plants which migrated back into the ocean.[3][4] Between about 70 million and 100 million years ago, the three independent seagrass lineages (Hydrocharitaceae, Cymodoceaceae complex, and Zosteraceae) evolved from a single lineage of monocotyledonous flowering plants.[5]

Other plants that colonised the sea, such as salt marsh plants, mangroves, and marine algae, have more diverse evolutionary lineages. In spite of their low species diversity, seagrasses have succeeded in colonising the continental shelves of all continents except Antarctica.[6]

Around 140 million years ago, seagrasses evolved from early monocotyledonous land plants, which succeeded in conquering the marine environment. Today, they are a polyphyletic group of marine angiosperms with around 60 species in five families (Zosteraceae, Hydrocharitaceae, Posidoniaceae, Cymodoceaceae, and Ruppiaceae), which belong to the order Alismatales according to the Angiosperm Phylogeny Group IV System.[7] The genus Ruppia, which occurs in brackish water, is not regarded as a “real” seagrass by all authors and has been shifted to the Cymodoceaceae by some authors.[8] The APG IV System and The Plant List Webpage[9] do not share this family assignment.[10]

Seagrasses form important coastal ecosystems.[11] The worldwide endangering of these sea meadows, which provide food and habitat for many marine species, prompts the need for protection and understanding of these valuable resources. Recently, sequencing of the genomes of Zostera marina and Zostera muelleri allowed better understanding angiosperm adaption to the sea.[12][13] During the evolutionary step back to the ocean, different genes have been lost (e.g., stomatal genes) or have been reduced (e.g., genes involved in the synthesis of terpenoids) and others have been regained, such as in genes involved in sulfation.[13][10]

Genome information further revealed that adaption to the marine habitat was accomplished by severe changes of cell wall composition.[12][13] On the other hand, the cell walls of seagrasses are poorly understood. Beside ancestral traits of land plants, one would anticipate a habitat-driven adaption process to the new environment, which is characterized by multiple abiotic (high amounts of salt) and biotic (different seagrass grazers and bacterial colonization) stressors.[10] The cell walls of seagrasses seem to be fascinating combinations of features known from both angiosperm land plants and marine macroalgae with new structural elements.[10]

Taxonomy

Family Image Genera Description
Zosteraceae The family Zosteraceae, also known as the seagrass family, includes two genera containing 14 marine species. It is found in temperate and subtropical coastal waters, with the highest diversity located around Korea and Japan.
Species subtotal:  
Phyllospadix
Zostera
Hydrocharitaceae The family Hydrocharitaceae, also known as tape-grasses, include Canadian waterweed and frogbit. The family includes both fresh and marine aquatics, although of the sixteen genera currently recognised, only three are marine.[14] They are found throughout the world in a wide variety of habitats, but are primarily tropical.
Species subtotal:  
Enhalus
Halophila
Thalassia
Posidoniaceae The family Posidoniaceae contains a single genus with two to nine marine species found in the seas of the Mediterranean and around the south coast of Australia.
Species subtotal: 2 to 9  
Posidonia
Cymodoceaceae The family Cymodoceaceae, also known as manatee-grass, includes only marine species.[15] Some taxonomists do not recognized this family.
Species subtotal:  
Amphibolis
Cymodocea
Halodule
Syringodium
Thalassodendron
Total species:   

Intertidal and subtidal seagrasses

Morphological and photoacclimatory responses
of intertidal and subtidal Zostera marina eelgrass [16]

Seagrasses occurring in the intertidal and subtidal zones are exposed to highly variable environmental conditions due to tidal changes.[17][18] Seagrasses in the intertidal zone are regularly exposed to air and consequently experience extreme high and low temperatures, high photoinhibitory irradiance, and desiccation stress relative to subtidal seagrass.[18][19][20] Such extreme temperatures can lead to significant seagrass dieback when seagrasses are exposed to air during low tide.[21][22][23] Desiccation stress during low tide has been considered the primary factor limiting seagrass distribution at the upper intertidal zone.[24] Seagrasses residing the intertidal zone are usually smaller than those in the subtidal zone to minimize the effects of emergence stress.[25][22] Intertidal seagrasses also show light-dependent responses, such as decreased photosynthetic efficiency and increased photoprotection during periods of high irradiance and air exposure.[26][27]

Zostera marina seedling [28]

In contrast, seagrasses in the subtidal zone adapt to reduced light conditions caused by light attenuation and scattering due to the overlaying water column and suspended particles.[29][30] Seagrasses in the deep subtidal zone generally have longer leaves and wider leaf blades than those in the shallow subtidal or intertidal zone, which allows more photosynthesis, in turn resulting in greater growth.[20] Seagrasses also respond to reduced light conditions by increasing chlorophyll content and decreasing the chlorophyll a/b ratio to enhance light absorption efficiency by using the abundant wavelengths efficiently.[31][32][33] As seagrasses in the intertidal and subtidal zones are under highly different light conditions, they exhibit distinctly different photoacclimatory responses to maximize photosynthetic activity and photoprotection from excess irradiance.

Seagrasses assimilate large amounts of inorganic carbon to achieve high level production.[34][35] Marine macrophytes, including seagrass, use both CO2 and HCO
3
(bicarbonate) for photosynthetic carbon reduction.[36][37][38] Despite air exposure during low tide, seagrasses in the intertidal zone can continue to photosynthesize utilizing CO2 in the air.[39] Thus, the composition of inorganic carbon sources for seagrass photosynthesis probably varies between intertidal and subtidal plants. Because stable carbon isotope ratios of plant tissues change based on the inorganic carbon sources for photosynthesis,[40][41] seagrasses in the intertidal and subtidal zones may have different stable carbon isotope ratio ranges.

Movement ecology

Five types of seagrass motion capacity
Three influenced by abiotic vectors, one by biotic vectors
and the final via clonal growth [42]

Understanding the movement ecology of seagrasses provides a way to assess the capacity of populations to recover from impacts associated with existing and future pressures. These include the (re)-colonization of altered or fragmented landscapes, and movement associated with climate change.[42]

The marine environment acts as an abiotic dispersal vector and its physical properties significantly influence movement, presenting both challenges and opportunities that differ from terrestrial environments. Typical flow speeds in the ocean are around 0.1 m s−1, generally one to two orders of magnitude weaker than typical atmospheric flows (1–10 m s−1), that can limit dispersal.[43] However, as seawater density is approximately 1000 times greater than air, momentum of a moving mass of water at the same speed is three orders of magnitude greater than in air. Therefore, drag forces acting on individuals (proportional to density) are also three orders of magnitude higher, enabling relatively larger-sized propagules to be mobilized. But most importantly, buoyancy forces (proportional to the density difference between seawater and the propagule) significantly reduce the effective weight of submerged propagules.[44] Within seagrasses, propagules can weakly settle (negatively buoyant), remain effectively suspended in the interior of the water column (neutrally buoyant), or float at the surface (positively buoyant).[45][42]

With positive buoyancy (e.g. floating fruit), ocean surface currents freely move propagules, and dispersal distances are only limited by the viability time of the fruit,[46][47] leading to exceptionally long single dispersal events (more than 100 km),[48] which is rare for passive abiotic movement of terrestrial fruit and seeds.[49][42]

There are a variety of biotic dispersal vectors for seagrasses, as they feed on or live in seagrass habitat. These include dugongs, manatees, turtles, waterfowl, fish and invertebrates.[50][51][52][53] Each biotic vector has its own internal state, motion capacity, navigation capacity and external factors influencing its movement. These interact with plant movement ecology to determine the ultimate movement path of the plant.[54][55][42]

For example, if a waterbird feeds on a seagrass containing fruit with seeds that are viable after defecation, then the bird has the potential to transport the seeds from one feeding ground to another. Therefore, the movement path of the bird determines the potential movement path of the seed. Particular traits of the animal, such as its digestive passage time, directly influence the plant's movement path.[42]

Seagrass microbiome

Processes within the seagrass holobiont
The most important interconnected processes within the seagrass holobiont are related to processes in the carbon-, nitrogen- and sulfur cycles. Photosynthetically active radiation (PAR) determines the photosynthetic activity of the seagrass plant that determines how much carbon dioxide is fixed, how much dissolved organic carbon (DOC) is exuded from the leaves and root system, and how much oxygen is transported into the rhizosphere. Oxygen transportation into the rhizosphere alters the redox conditions in the rhizosphere, differentiating it from the surrounding sediments that are usually anoxic and sulfidic.[56][57]

Seagrass holobiont

The concept of the holobiont, which emphasizes the importance and interactions of a microbial host with associated microorganisms and viruses and describes their functioning as a single biological unit,[58] has been investigated and discussed for many model systems, although there is substantial criticism of a concept that defines diverse host-microbe symbioses as a single biological unit.[59] The holobiont and hologenome concepts have evolved since the original definition,[60] and there is no doubt that symbiotic microorganisms are pivotal for the biology and ecology of the host by providing vitamins, energy and inorganic or organic nutrients, participating in defense mechanisms, or by driving the evolution of the host.[61] Although most work on host-microbe interactions has been focused on animal systems such as corals, sponges, or humans, there is a substantial body of literature on plant holobionts.[62] Plant-associated microbial communities impact both key components of the fitness of plants, growth and survival,[63] and are shaped by nutrient availability and plant defense mechanisms.[64] Several habitats have been described to harbor plant-associated microbes, including the rhizoplane (surface of root tissue), the rhizosphere (periphery of the roots), the endosphere (inside plant tissue), and the phyllosphere (total above-ground surface area).[56]

Seagrass meadows

Seagrass beds/meadows can be either monospecific (made up of a single species) or in mixed beds. In temperate areas, usually one or a few species dominate (like the eelgrass Zostera marina in the North Atlantic), whereas tropical beds usually are more diverse, with up to thirteen species recorded in the Philippines.

Seagrass beds are diverse and productive ecosystems, and can harbor hundreds of associated species from all phyla, for example juvenile and adult fish, epiphytic and free-living macroalgae and microalgae, mollusks, bristle worms, and nematodes. Few species were originally considered to feed directly on seagrass leaves (partly because of their low nutritional content), but scientific reviews and improved working methods have shown that seagrass herbivory is an important link in the food chain, feeding hundreds of species, including green turtles, dugongs, manatees, fish, geese, swans, sea urchins and crabs. Some fish species that visit/feed on seagrasses raise their young in adjacent mangroves or coral reefs.

Seagrasses trap sediment and slow down water movement, causing suspended sediment to settle out. Trapping sediment benefits coral by reducing sediment loads, improving photosynthesis for both coral and seagrass.[65]

Seagrass bed with several echinoids
Seagrass bed with dense turtle grass (Thalassia testudinum) and an immature queen conch (Eustrombus gigas)

Although often overlooked, seagrasses provide a number of ecosystem services.[66][67] Seagrasses are considered ecosystem engineers.[68][4][3] This means that the plants alter the ecosystem around them. This adjusting occurs in both physical and chemical forms. Many seagrass species produce an extensive underground network of roots and rhizome which stabilizes sediment and reduces coastal erosion.[69] This system also assists in oxygenating the sediment, providing a hospitable environment for sediment-dwelling organisms.[68] Seagrasses also enhance water quality by stabilizing heavy metals, pollutants, and excess nutrients.[70][4][3] The long blades of seagrasses slow the movement of water which reduces wave energy and offers further protection against coastal erosion and storm surge. Furthermore, because seagrasses are underwater plants, they produce significant amounts of oxygen which oxygenate the water column. These meadows account for more than 10% of the ocean's total carbon storage. Per hectare, it holds twice as much carbon dioxide as rain forests and can sequester about 27.4 million tons of CO2 annually.[71] The storage of carbon is an essential ecosystem service as we move into a period of elevated atmospheric carbon levels. However, some climate change models suggest that some seagrasses will go extinct – Posidonia oceanica is expected to go extinct, or nearly so, by 2050.

Seagrass meadows provide food for many marine herbivores. Sea turtles, manatees, parrotfish, surgeonfish, sea urchins and pinfish feed on seagrasses. Many other smaller animals feed on the epiphytes and invertebrates that live on and among seagrass blades.[72] Seagrass meadows also provide physical habitat in areas that would otherwise be bare of any vegetation. Due to this three dimensional structure in the water column, many species occupy seagrass habitats for shelter and foraging. It is estimated that 17 species of coral reef fish spend their entire juvenile life stage solely on seagrass flats.[73] These habitats also act as a nursery grounds for commercially and recreationally valued fishery species, including the gag grouper (Mycteroperca microlepis), red drum, common snook, and many others.[74][75] Some fish species utilize seagrass meadows and various stages of the life cycle. In a recent publication, Dr. Ross Boucek and colleagues discovered that two highly sought after flats fish, the common snook and spotted sea trout provide essential foraging habitat during reproduction.[76] Sexual reproduction is extremely energetically expensive to be completed with stored energy; therefore, they require seagrass meadows in close proximity to complete reproduction.[76] Furthermore, many commercially important invertebrates also reside in seagrass habitats including bay scallops (Argopecten irradians), horseshoe crabs, and shrimp. Charismatic fauna can also be seen visiting the seagrass habitats. These species include West Indian manatee, green sea turtles, and various species of sharks. The high diversity of marine organisms that can be found on seagrass habitats promotes them as a tourist attraction and a significant source of income for many coastal economies along the Gulf of Mexico and in the Caribbean.

See also

References

  1. ^ Tomlinson and Vargo (1966). "On the morphology and anatomy of turtle grass, Thalassia testudinum (Hydrocharitaceae). I. Vegetative Morphology". Bulletin of Marine Science. 16: 748–761.
  2. ^ Knauth, L. Paul; Kennedy, Martin J. (2009). "The late Precambrian greening of the Earth". Nature. 460 (7256): 728–732. Bibcode:2009Natur.460..728K. doi:10.1038/nature08213. PMID 19587681. S2CID 4398942.
  3. ^ a b c Orth; et al. (2006). "A global crisis for seagrass ecosystems". BioScience. 56 (12): 987–996. doi:10.1641/0006-3568(2006)56[987:AGCFSE]2.0.CO;2. hdl:10261/88476.
  4. ^ a b c Papenbrock, J (2012). "Highlights in seagrass' phylogeny, physiology, and metabolism: what makes them so species?". International Scholarly Research Network: 1–15.
  5. ^ Les, D.H., Cleland, M.A. and Waycott, M. (1997) "Phylogenetic studies in Alismatidae, II: evolution of marine angiosperms (seagrasses) and hydrophily". Systematic Botany 22(3): 443–463.
  6. ^ Orth, Robert J.; Carruthers, TIM J. B.; Dennison, William C.; Duarte, Carlos M.; Fourqurean, James W.; Heck, Kenneth L.; Hughes, A. Randall; Kendrick, Gary A.; Kenworthy, W. Judson; Olyarnik, Suzanne; Short, Frederick T.; Waycott, Michelle; Williams, Susan L. (2006). "A Global Crisis for Seagrass Ecosystems". BioScience. 56 (12): 987. doi:10.1641/0006-3568(2006)56[987:AGCFSE]2.0.CO;2. ISSN 0006-3568.
  7. ^ "An update of the Angiosperm Phylogeny Group classification for the orders and families of flowering plants: APG IV". Botanical Journal of the Linnean Society. 181: 1–20. 2016. doi:10.1111/boj.12385.
  8. ^ Wilkin, Paul; Mayo, Simon J. (30 May 2013). Early Events in Monocot Evolution. ISBN 9781107244603.
  9. ^ The Plant List (2020). Ruppia. Available online at: http://www.theplantlist.org/1.1/browse/A/Ruppiaceae/Ruppia/ (accessed September 22, 2020).
  10. ^ a b c d Pfeifer, Lukas; Classen, Birgit (2020). "The Cell Wall of Seagrasses: Fascinating, Peculiar and a Blank Canvas for Future Research". Frontiers in Plant Science. 11: 588754. doi:10.3389/fpls.2020.588754. PMC 7644952. PMID 33193541.{{cite journal}}: CS1 maint: unflagged free DOI (link)
  11. ^ Hemminga, M. A., and Duarte, C. M. eds (2000). “Seagrasses in the human environment,” in Seagrass Ecology (Cambridge: Cambridge University Press), 248–291.
  12. ^ a b Lee, Hueytyng; Golicz, Agnieszka A.; Bayer, Philipp E.; Jiao, Yuannian; Tang, Haibao; Paterson, Andrew H.; Sablok, Gaurav; Krishnaraj, Rahul R.; Chan, Chon-Kit Kenneth; Batley, Jacqueline; Kendrick, Gary A.; Larkum, Anthony W.D.; Ralph, Peter J.; Edwards, David (2016). "The Genome of a Southern Hemisphere Seagrass Species (Zostera muelleri)". Plant Physiology. 172 (1): 272–283. doi:10.1104/pp.16.00868. PMC 5074622. PMID 27373688.
  13. ^ a b c Olsen, Jeanine L.; et al. (2016). "The genome of the seagrass Zostera marina reveals angiosperm adaptation to the sea". Nature. 530 (7590): 331–335. Bibcode:2016Natur.530..331O. doi:10.1038/nature16548. PMID 26814964. S2CID 3713147.
  14. ^ Christenhusz, Maarten J.M.; Byng, James W. (2016-05-20). "The number of known plants species in the world and its annual increase". Phytotaxa. 261 (3): 201. doi:10.11646/phytotaxa.261.3.1. ISSN 1179-3163.
  15. ^ Waycott, Michelle; McMahon, Kathryn; Lavery, Paul (2014). A Guide to Southern Temperate Seagrasses. CSIRO Publishing. ISBN 9781486300150.
  16. ^ Park, Sang Rul; Kim, Sangil; Kim, Young Kyun; Kang, Chang-Keun; Lee, Kun-Seop (2016). "Photoacclimatory Responses of Zostera marina in the Intertidal and Subtidal Zones". PLOS ONE. 11 (5): e0156214. Bibcode:2016PLoSO..1156214P. doi:10.1371/journal.pone.0156214. PMC 4881947. PMID 27227327.{{cite journal}}: CS1 maint: unflagged free DOI (link) Material was copied from this source, which is available under a Creative Commons Attribution 4.0 International License.
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Further references

  • den Hartog, C. 1970. The Sea-grasses of the World. Verhandl. der Koninklijke Nederlandse Akademie van Wetenschappen, Afd. Natuurkunde, No. 59(1).
  • Duarte, Carlos M. and Carina L. Chiscano “Seagrass biomass and production: a reassessment” Aquatic Botany Volume 65, Issues 1–4, November 1999, Pages 159–174.
  • Green, E.P. & Short, F.T.(eds). 2003. World Atlas of Seagrasses. University of California Press, Berkeley, CA. 298 pp.
  • Hemminga, M.A. & Duarte, C. 2000. Seagrass Ecology. Cambridge University Press, Cambridge. 298 pp.
  • Hogarth, Peter The Biology of Mangroves and Seagrasses (Oxford University Press, 2007)
  • Larkum, Anthony W.D., Robert J. Orth, and Carlos M. Duarte (Editors) Seagrasses: Biology, Ecology and Conservation (Springer, 2006)
  • Orth, Robert J. et al. "A Global Crisis for Seagrass Ecosystems" BioScience December 2006 / Vol. 56 No. 12, Pages 987–996.
  • Short, F.T. & Coles, R.G.(eds). 2001. Global Seagrass Research Methods. Elsevier Science, Amsterdam. 473 pp.
  • A.W.D. Larkum, R.J. Orth, and C.M. Duarte (eds). Seagrass Biology: A Treatise. CRC Press, Boca Raton, FL, in press.
  • A. Schwartz; M. Morrison; I. Hawes; J. Halliday. 2006. Physical and biological characteristics of a rare marine habitat: sub-tidal seagrass beds of offshore islands. Science for Conservation 269. 39 pp. [1]
  • Waycott, M, McMahon, K, & Lavery, P 2014, A guide to southern temperate seagrasses, CSIRO Publishing, Melbourne