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{{Use dmy dates|date=May 2022}}
{{Use dmy dates|date=May 2022}}
{{About|a classification of rivers|rivers named "Blackwater"|Blackwater River (disambiguation)||Blackwater (disambiguation)}}
{{About|a classification of rivers|rivers named "Blackwater"|Blackwater River (disambiguation)||Blackwater (disambiguation)}}
{{short description|Slow-moving, dark-colored river flowing through forested swamps or wetlands}}
{{Short description|Slow, dark river in forested swamps or wetlands}}
[[File:LeonSinksBlackWtrMay05.jpg|thumb|A swamp-fed stream in northern [[Florida]], showing tannin-stained undisturbed blackwater]]
[[File:LeonSinksBlackWtrMay05.jpg|thumb|A swamp-fed stream in northern [[Florida]], showing tannin-stained undisturbed blackwater]]


A '''blackwater river''' is a type of [[River#Classification|river]] with a slow-moving channel flowing through forested [[swamp]]s or [[wetland]]s. As vegetation decays, [[tannin]]s leach into the water, making a transparent, acidic water that is darkly stained, resembling [[black tea]]. Most major blackwater rivers are in the [[Amazon Basin]] and the [[Southern United States]]. The term is used in [[fluvial]] studies, [[geology]], [[geography]], [[ecology]], and [[biology]]. Not all dark rivers are blackwater in that technical sense. Some rivers in temperate regions, which drain or flow through areas of dark black [[loam]], are simply black due to the color of the soil; these rivers are ''black mud rivers''. There are also black mud [[Estuary|estuaries]].
A '''blackwater river''' is a type of [[River#Classification|river]] with a slow-moving channel flowing through forested [[swamp]]s or [[wetland]]s. Most major blackwater rivers are in the [[Amazon Basin]] and the [[Southern United States]]. The term is used in [[fluvial]] studies, [[geology]], [[geography]], [[ecology]], and [[biology]]. Not all dark rivers are blackwater in that technical sense. Some rivers in temperate regions, which drain or flow through areas of dark black [[loam]], are simply black due to the color of the soil; these rivers are ''black mud rivers''. There are also black mud [[Estuary|estuaries]].


Blackwater rivers are lower in nutrients than [[Whitewater river (river type)|whitewater rivers]] and have [[Ionic strength|ionic concentrations]] higher than rainwater.<ref>{{cite journal |doi=10.2307/2989823 |last=Janzen |first=D. H. |title=Tropical Blackwater Rivers, Animals, and Mast Fruiting by the [[Dipterocarpaceae]] |journal=Biotropica |volume=6 |issue=2 |date=July 1974 |pages=69–103 |jstor=2989823}}</ref><ref>{{cite journal |last=Sioli |first=Harald |year=1975 |title=Tropical rivers as expressions of their terrestrial environments |journal=Tropical Ecological Systems/Trends in Terrestrial and Aquatic Research |pages=275–288 |publisher=[[Springer Science+Business Media|Springer-Verlag]] |location=[[New York City]]}}</ref> The unique conditions lead to flora and fauna that differ from both whitewater and [[Clearwater river (river type)|clearwater rivers]].<ref name="Duncan">{{cite journal |last1=Duncan |first1=W. P. |last2=Fernandes |first2=M. N. |date=2010 |url=https://www.researchgate.net/profile/Wallice-Duncan/publication/230692696_Physicochemical_characterization_of_the_white_black_and_clearwater_rivers_of_the_Amazon_Basin_and_its_implications_on_the_distribution_of_freshwater_stingrays_Chondrichthyes_Potamotrygonidae/links/0fcfd5032ba0ebcae3000000/Physicochemical-characterization-of-the-white-black-and-clearwater-rivers-of-the-Amazon-Basin-and-its-implications-on-the-distribution-of-freshwater-stingrays-Chondrichthyes-Potamotrygonidae.pdf |title=Physicochemical characterization of the white, black, and clearwater rivers of the Amazon Basin and its implications on the distribution of freshwater stingrays (Chondrichthyes, Potamotrygonidae) |journal=PanamJAS |volume=5 |issue=3 |pages=454–464 |archive-url=https://web.archive.org/web/20211113075416/https://www.researchgate.net/profile/Wallice-Duncan/publication/230692696_Physicochemical_characterization_of_the_white_black_and_clearwater_rivers_of_the_Amazon_Basin_and_its_implications_on_the_distribution_of_freshwater_stingrays_Chondrichthyes_Potamotrygonidae/links/0fcfd5032ba0ebcae3000000/Physicochemical-characterization-of-the-white-black-and-clearwater-rivers-of-the-Amazon-Basin-and-its-implications-on-the-distribution-of-freshwater-stingrays-Chondrichthyes-Potamotrygonidae.pdf |archive-date=13 November 2021}}</ref> The classification of Amazonian rivers into black, clear, and whitewater was first proposed by [[Alfred Russel Wallace]] in 1853 based on water colour, but the types were more clearly defined by chemistry and physics by {{ill|Harald Sioli|de}} from the 1950s to the 1980s.<ref name="Duncan" /><ref name="Sioli1984">{{cite book| editor-last=Sioli |editor-first=H. | year=1984 | title=The Amazon: Limnology and landscape ecology of a mighty tropical river and its basin | isbn=978-94-009-6544-7}}</ref> Although many Amazonian rivers fall clearly into one of these categories, others show a mix of characteristics and may vary depending on season and flood levels.<ref name="Goulding1982">{{cite journal | last1=Goulding |first1=M. | first2=M. L. |last2=Carvalho | year=1982 | title=Life history and management of the tambaqui (Colossoma macropomum, Characidae): an important Amazonian food fish | journal=Revista Brasileira de Zoologia | volume=1 | issue=2 | pages=107–133 | doi=10.1590/S0101-81751982000200001 | doi-access=free }}</ref>
Blackwater rivers are lower in nutrients than [[Whitewater river (river type)|whitewater rivers]] and have [[Ionic strength|ionic concentrations]] higher than rainwater.<ref>{{cite journal |doi=10.2307/2989823 |last=Janzen |first=D. H. |title=Tropical Blackwater Rivers, Animals, and Mast Fruiting by the [[Dipterocarpaceae]] |journal=Biotropica |volume=6 |issue=2 |date=July 1974 |pages=69–103 |jstor=2989823}}</ref><ref>{{cite journal |last=Sioli |first=Harald |year=1975 |title=Tropical rivers as expressions of their terrestrial environments |journal=Tropical Ecological Systems/Trends in Terrestrial and Aquatic Research |pages=275–288 |publisher=[[Springer Science+Business Media|Springer-Verlag]] |location=[[New York City]]}}</ref> The unique conditions lead to flora and fauna that differ from both whitewater and [[Clearwater river (river type)|clearwater rivers]].<ref name="Duncan">{{cite journal |last1=Duncan |first1=W. P. |last2=Fernandes |first2=M. N. |date=2010 |url=https://www.researchgate.net/publication/230692696 |title=Physicochemical characterization of the white, black, and clearwater rivers of the Amazon Basin and its implications on the distribution of freshwater stingrays (Chondrichthyes, Potamotrygonidae) |journal=PanamJAS |volume=5 |issue=3 |pages=454–464 |archive-url=https://web.archive.org/web/20211113075416/https://www.researchgate.net/profile/Wallice-Duncan/publication/230692696_Physicochemical_characterization_of_the_white_black_and_clearwater_rivers_of_the_Amazon_Basin_and_its_implications_on_the_distribution_of_freshwater_stingrays_Chondrichthyes_Potamotrygonidae/links/0fcfd5032ba0ebcae3000000/Physicochemical-characterization-of-the-white-black-and-clearwater-rivers-of-the-Amazon-Basin-and-its-implications-on-the-distribution-of-freshwater-stingrays-Chondrichthyes-Potamotrygonidae.pdf |archive-date=13 November 2021}}</ref> The classification of Amazonian rivers into black, clear, and whitewater was first proposed by [[Alfred Russel Wallace]] in 1853 based on water colour, but the types were more clearly defined by chemistry and physics by {{ill|Harald Sioli|de}} from the 1950s to the 1980s.<ref name="Duncan" /><ref name="Sioli1984">{{cite book| editor-last=Sioli |editor-first=H. | year=1984 | title=The Amazon: Limnology and landscape ecology of a mighty tropical river and its basin |publisher=Springer | isbn=978-94-009-6544-7}}</ref> Although many Amazonian rivers fall clearly into one of these categories, others show a mix of characteristics and may vary depending on season and flood levels.<ref name="Goulding1982">{{cite journal | last1=Goulding |first1=M. | first2=M. L. |last2=Carvalho | year=1982 | title=Life history and management of the tambaqui (Colossoma macropomum, Characidae): an important Amazonian food fish | journal=Revista Brasileira de Zoologia | volume=1 | issue=2 | pages=107–133 | doi=10.1590/S0101-81751982000200001 | doi-access=free }}</ref>


==Comparison between white and black waters==
==Comparison between white and black waters==
Line 90: Line 90:
Black and [[Whitewater river (river type)|white waters]] differ significantly in their ionic composition, as shown in [[#table1|Table 1]]. Black waters are more [[acid]]ic, resulting in an [[aluminum]] concentration greater than that of the more neutral white waters. The major difference is the concentrations of [[sodium]], [[magnesium]], [[calcium]], and [[potassium]]; these are very low in black waters. This has ecological implications. Some animals need more calcium than is available in blackwaters, so for example, [[snail]]s, which need much calcium to build shells, are not abundant in blackwaters. The lack of dissolved ions in black waters results in a low [[electrical conductivity|conductivity]], similar to that of rainwater.{{Cn|date=February 2021}}
Black and [[Whitewater river (river type)|white waters]] differ significantly in their ionic composition, as shown in [[#table1|Table 1]]. Black waters are more [[acid]]ic, resulting in an [[aluminum]] concentration greater than that of the more neutral white waters. The major difference is the concentrations of [[sodium]], [[magnesium]], [[calcium]], and [[potassium]]; these are very low in black waters. This has ecological implications. Some animals need more calcium than is available in blackwaters, so for example, [[snail]]s, which need much calcium to build shells, are not abundant in blackwaters. The lack of dissolved ions in black waters results in a low [[electrical conductivity|conductivity]], similar to that of rainwater.{{Cn|date=February 2021}}


Black and white waters differ in their [[plankton]]ic fauna and flora. [[#table2|Tables 2]] and [[#table3|3]] compare the number of planktonic animals caught in black and white water localities only a few meters apart. The black water was not as extreme an example as the [[Rio Negro (Amazon)|Rio Negro]] system. However, it can be seen that the black water held greater numbers of [[rotifer]]s but fewer [[crustacean]]s and [[mite]]s. These crustaceans are important foods for [[larval fish]]. The zones where the two waters mix are attractive to [[ostracod]]s and young fish. These mixing zones tend to have many animals. The abundance is shown in Table{{nbsp}}3, which compares animals in {{convert|10|l}} of water.<ref>{{cite web |title=Comparison between white and black waters |access-date=21 May 2006 |url=http://www.amazonian-fish.co.uk/indexc30.html |work=Amazonian Fishes and their Habitats |publisher=Pisces Conservation Ltd |archive-url=https://web.archive.org/web/20110716122850/http://www.amazonian-fish.co.uk/indexc30.html |archive-date=16 July 2011 |url-status=dead }}</ref>
Black and white waters differ in their [[plankton]]ic fauna and flora. [[#table2|Tables 2]] and [[#table3|3]] compare the number of planktonic animals caught in black and white water localities only a few meters apart. The black water was not as extreme an example as the [[Rio Negro (Amazon)|Rio Negro]] system. However, it can be seen that the black water held greater numbers of [[rotifer]]s but fewer [[crustacean]]s and [[mite]]s. These crustaceans are important foods for [[larval fish]]. The zones where the two waters mix are attractive to [[ostracod]]s and young fish. These mixing zones tend to have many animals. The abundance is shown in Table{{nbsp}}3, which compares animals in {{convert|10|L}} of water.<ref>{{cite web |title=Comparison between white and black waters |access-date=21 May 2006 |url=http://www.amazonian-fish.co.uk/indexc30.html |work=Amazonian Fishes and their Habitats |publisher=Pisces Conservation Ltd |archive-url=https://web.archive.org/web/20110716122850/http://www.amazonian-fish.co.uk/indexc30.html |archive-date=16 July 2011 |url-status=dead }}</ref>


{| id="table2" class="wikitable" style="float:right; clear:right; margin:0 0 0.5em 1em;"
{| id="table2" class="wikitable" style="float:right; clear:right; margin:0 0 0.5em 1em;"
Line 233: Line 233:


==Comparison between clear and black waters==
==Comparison between clear and black waters==
Blackwater rivers resemble [[Clearwater river (river type)|clearwater rivers]] in having a low conductivity and relatively low levels of [[Total dissolved solids|dissolved solids]], but clearwater rivers have water that often only is somewhat acidic (typical pH ~6.5)<ref name="Duncan" /> and very clear with a greenish color.<ref name="Giovanetti">{{cite book | first1= Thomas A. |last1=Giovannetti | first2= Matthew M. |last2=Vriends | title = Discus Fish | url = https://archive.org/details/discusfishacompl00giov | url-access = limited | publisher = Barron's | location = Hauppauge, NY | year = 1991 | isbn = 0-8120-4669-2 | page = [https://archive.org/details/discusfishacompl00giov/page/n16 15]}}</ref> The main Amazonian clearwater rivers have their source in the [[Brazilian Plateau]] (such as [[Tapajós River|Tapajós]], [[Tocantins River|Tocantins]], [[Xingu River|Xingu]] and some right tributaries of the [[Madeira River|Madeira]]), but some originate in the [[Guiana Shield]] (such as [[Nhamundá River|Nhamundá]], [[Paru River|Paru]], and [[Araguari River (Amapá)|Araguari]]).<ref>{{cite journal |last1=Junk |first1=W. J. |last2=Piedade |first2=M. T. F. |last3=Schöngart |first3=J. |last4=Cohn-Haft |first4=M. |last5=Adeney |first5=J. M. |last6=Wittmann |first6=F. A. |date=2011 |title=Classification of Major Naturally-Occurring Amazonian Lowland Wetlands |journal=Wetlands |volume=31 |pages=623–640}}</ref>
Blackwater rivers resemble [[Clearwater river (river type)|clearwater rivers]] in having a low conductivity and relatively low levels of [[Total dissolved solids|dissolved solids]], but clearwater rivers have water that often only is somewhat acidic (typical pH ~6.5)<ref name="Duncan" /> and very clear with a greenish color.<ref name="Giovanetti">{{cite book | first1= Thomas A. |last1=Giovannetti | first2= Matthew M. |last2=Vriends | title = Discus Fish | url = https://archive.org/details/discusfishacompl00giov | url-access = limited | publisher = Barron's | location = Hauppauge, NY | year = 1991 | isbn = 0-8120-4669-2 | page = [https://archive.org/details/discusfishacompl00giov/page/n16 15]}}</ref> The main Amazonian clearwater rivers have their source in the [[Brazilian Plateau]] (such as [[Tapajós River|Tapajós]], [[Tocantins River|Tocantins]], [[Xingu River|Xingu]] and some right tributaries of the [[Madeira River|Madeira]]), but some originate in the [[Guiana Shield]] (such as [[Nhamundá River|Nhamundá]], [[Paru River|Paru]], and [[Araguari River (Amapá)|Araguari]]).<ref>{{cite journal |last1=Junk |first1=W. J. |last2=Piedade |first2=M. T. F. |last3=Schöngart |first3=J. |last4=Cohn-Haft |first4=M. |last5=Adeney |first5=J. M. |last6=Wittmann |first6=F. A. |date=2011 |title=Classification of Major Naturally-Occurring Amazonian Lowland Wetlands |journal=Wetlands |volume=31 |issue=4 |pages=623–640|doi=10.1007/s13157-011-0190-7 |s2cid=36001397 }}</ref>


== Blackwater rivers of the world ==
== Blackwater rivers of the world ==
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*[[Upper Little River]], North Carolina: flows into the [[Cape Fear River]].
*[[Upper Little River]], North Carolina: flows into the [[Cape Fear River]].
*[[Nanticoke River|Upper Nanticoke River]], Delaware and Maryland: flows into the Chesapeake Bay.
*[[Nanticoke River|Upper Nanticoke River]], Delaware and Maryland: flows into the Chesapeake Bay.
*[[Village Creek (Texas)|Village Creek]], a 63 Mile long stream in the [[Big Thicket]] region of southeast Texas: flows into the [[Neches River]].
*[[Waccamaw River]], North and South Carolina: flows into the Atlantic Ocean.
*[[Waccamaw River]], North and South Carolina: flows into the Atlantic Ocean.
*[[White Oak River]], North Carolina: flows into the Atlantic Ocean.
*[[White Oak River]], North Carolina: flows into the Atlantic Ocean.
*[[Wolf River (Mississippi)|Wolf River]]: arises in Northern Mississippi and runs through southwest Tennessee/Memphis into Mississippi River
*[[Wolf River (Tennessee)|Wolf River]]: arises in Northern Mississippi and runs through southwest Tennessee/Memphis into Mississippi River


===Northern United States===
===Northern United States===
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*[[Davey River]], Tasmania: a relatively small river in the southwest corner of the island which runs through extensive heathlands, peat bogs and [[Gymnoschoenus sphaerocephalus|button grass]] plains
*[[Davey River]], Tasmania: a relatively small river in the southwest corner of the island which runs through extensive heathlands, peat bogs and [[Gymnoschoenus sphaerocephalus|button grass]] plains
*[[Noosa River]], [[Queensland]]: a small section of the Noosa River running between Lake Cootharaba and Lake Cooroibah<ref>{{cite web|url=http://www.upstreampaddle.com/noosa.html|title=Noosa River Elanda Point to Campsite Fifteen Canoe Guidebook|website=www.upstreampaddle.com|access-date=19 November 2014|archive-date=8 July 2020|archive-url=https://web.archive.org/web/20200708025442/http://www.upstreampaddle.com/noosa.html|url-status=dead}}</ref>
*[[Noosa River]], [[Queensland]]: a small section of the Noosa River running between Lake Cootharaba and Lake Cooroibah<ref>{{cite web|url=http://www.upstreampaddle.com/noosa.html|title=Noosa River Elanda Point to Campsite Fifteen Canoe Guidebook|website=www.upstreampaddle.com|access-date=19 November 2014|archive-date=8 July 2020|archive-url=https://web.archive.org/web/20200708025442/http://www.upstreampaddle.com/noosa.html|url-status=dead}}</ref>
*[[Searys Creek]], Queensland: a small river running from the [[Great Sandy National Park]] to Tin Can Bay stained with [[Melaleuca alternifolia|tea-tree]] tannin.


====Intermittent blackwater events====
Other rivers in Australia may experience infrequent 'blackwater events' associated with flood waters connecting to forested floodplains and these events may be associated with hypoxic waters [low oxygen]. Examples include the [[Murray River]], [[Edward River]], [[Wakool River]] and [[Murrumbidgee River]].<ref>{{cite web |url=http://www.dpi.nsw.gov.au/fisheries/habitat/threats/fish-kills/black-water-events-causing-fish-kills-in-the-murray,-murrumbidgee-and-lower-darling-river-catchments-march-2012 |title=Black water event in the Murray, Murrumbidgee and Lower Darling River catchments: March 2012 |access-date=8 August 2014 |url-status=dead |archive-url=https://web.archive.org/web/20140808062137/http://www.dpi.nsw.gov.au/fisheries/habitat/threats/fish-kills/black-water-events-causing-fish-kills-in-the-murray%2C-murrumbidgee-and-lower-darling-river-catchments-march-2012 |archive-date=8 August 2014 }}</ref>
Other rivers in Australia may experience infrequent 'blackwater events' associated with flood waters connecting to forested floodplains and these events may be associated with hypoxic waters [low oxygen]. Examples include the [[Murray River]], [[Edward River]], [[Wakool River]] and [[Murrumbidgee River]].<ref>{{cite web |url=http://www.dpi.nsw.gov.au/fisheries/habitat/threats/fish-kills/black-water-events-causing-fish-kills-in-the-murray,-murrumbidgee-and-lower-darling-river-catchments-march-2012 |title=Black water event in the Murray, Murrumbidgee and Lower Darling River catchments: March 2012 |work=www.dpi.nsw.gov.au |access-date=8 August 2014 |url-status=dead |archive-url=https://web.archive.org/web/20140808062137/http://www.dpi.nsw.gov.au/fisheries/habitat/threats/fish-kills/black-water-events-causing-fish-kills-in-the-murray%2C-murrumbidgee-and-lower-darling-river-catchments-march-2012 |archive-date=8 August 2014 }}</ref>


===Indonesia===
===Indonesia===
* [[Sabangau River]]
* [[Sabangau River]]
* [[Kapuas River]]


==Gallery==
==Images of blackwater rivers==
<gallery widths="210px" heights="170px">
<gallery widths="210px" heights="170px">
Amazon blackwater.JPG|Amazon tributary classified as blackwater
Amazon blackwater.JPG|Amazon tributary classified as blackwater

Latest revision as of 01:41, 27 November 2024

A swamp-fed stream in northern Florida, showing tannin-stained undisturbed blackwater

A blackwater river is a type of river with a slow-moving channel flowing through forested swamps or wetlands. Most major blackwater rivers are in the Amazon Basin and the Southern United States. The term is used in fluvial studies, geology, geography, ecology, and biology. Not all dark rivers are blackwater in that technical sense. Some rivers in temperate regions, which drain or flow through areas of dark black loam, are simply black due to the color of the soil; these rivers are black mud rivers. There are also black mud estuaries.

Blackwater rivers are lower in nutrients than whitewater rivers and have ionic concentrations higher than rainwater.[1][2] The unique conditions lead to flora and fauna that differ from both whitewater and clearwater rivers.[3] The classification of Amazonian rivers into black, clear, and whitewater was first proposed by Alfred Russel Wallace in 1853 based on water colour, but the types were more clearly defined by chemistry and physics by Harald Sioli [de] from the 1950s to the 1980s.[3][4] Although many Amazonian rivers fall clearly into one of these categories, others show a mix of characteristics and may vary depending on season and flood levels.[5]

Comparison between white and black waters

[edit]
Table 1: Mean ionic composition, specific conductivity (μS/cm), and pH in Amazon waters.[6]
Solimões or
Amazon River
– whitewater
Rio Negro
– blackwater
Na (mg/L) 2.3 ± 0.8 0.380 ± 0.124
K (mg/L) 0.9 ± 0.2 0.327 ± 0.107
Mg (mg/L) 1.1 ± 0.2 0.114 ± 0.035
Ca (mg/L) 7.2 ± 1.6 0.212 ± 0.066
Cl (mg/L) 3.1 ± 2.1 1.7 ± 0.7
Si (mg/L) 4.0 ± 0.9 2.0 ± 0.5
Sr (μg/L) 37.8 ± 8.8 3.6 ± 1.0
Ba (μg/L) 22.7 ± 5.9 8.1 ± 2.1
Al (μg/L) 44 ± 37 112 ± 29
Fe (μg/L) 109 ± 76 178 ± 58
Mn (μg/L) 5.9 ± 5.1 9.0 ± 2.4
Cu (μg/L) 2.4 ± 0.6 1.8 ± 0.5
Zn (μg/L) 3.2 ± 1.5 4.1 ± 1.8
Conductivity 57 ± 8 9 ± 2
pH 6.9 ± 0.4 5.1±0.6
Total P (μg/L) 105 ± 58 25 ± 17
Total C (mg/L) 13.5 ± 3.1 10.5 ± 1.3
HCO3-C (mg/L) 6.7 ± 0.8 1.7 ± 0.5

Black and white waters differ significantly in their ionic composition, as shown in Table 1. Black waters are more acidic, resulting in an aluminum concentration greater than that of the more neutral white waters. The major difference is the concentrations of sodium, magnesium, calcium, and potassium; these are very low in black waters. This has ecological implications. Some animals need more calcium than is available in blackwaters, so for example, snails, which need much calcium to build shells, are not abundant in blackwaters. The lack of dissolved ions in black waters results in a low conductivity, similar to that of rainwater.[citation needed]

Black and white waters differ in their planktonic fauna and flora. Tables 2 and 3 compare the number of planktonic animals caught in black and white water localities only a few meters apart. The black water was not as extreme an example as the Rio Negro system. However, it can be seen that the black water held greater numbers of rotifers but fewer crustaceans and mites. These crustaceans are important foods for larval fish. The zones where the two waters mix are attractive to ostracods and young fish. These mixing zones tend to have many animals. The abundance is shown in Table 3, which compares animals in 10 litres (2.2 imp gal; 2.6 US gal) of water.[7]

Table 2: Planktonic organisms collected in black (Japura) and white (Solimões) waters.[6]
Animal groups
present
Black
water
Mixed
water
White
water
Rotifera 284 23 0
Cladocera 5 29 43
Ostracoda 39 97 29
Calanoida 11 51 66
Cyclopoida 22 49 61
Chironomidae 0 3 3
Acari (mites) 0 0 2
Table 3: Number of planktonic organisms collected in 10 L of black, white, and mixed waters.[6]
Black water Mixed water White water
Animal groups
present
Open
water
Forest Open
water
Forest Open
water
Forest
Volvocaceae 42   38      
Rotifera 87 5 34      
Cladocera 6   5   8 1
Ostracoda 2 11 3   7  
Calanoida 23 3 10      
Cyclopoida 5 27 19 1 13 1
Mysidacea   1        
Diptera         1  
Acari (mites)     1   1  
Larval fish     1   1  

Comparison between clear and black waters

[edit]

Blackwater rivers resemble clearwater rivers in having a low conductivity and relatively low levels of dissolved solids, but clearwater rivers have water that often only is somewhat acidic (typical pH ~6.5)[3] and very clear with a greenish color.[8] The main Amazonian clearwater rivers have their source in the Brazilian Plateau (such as Tapajós, Tocantins, Xingu and some right tributaries of the Madeira), but some originate in the Guiana Shield (such as Nhamundá, Paru, and Araguari).[9]

Blackwater rivers of the world

[edit]

Amazonia

[edit]

Orinoco basin

[edit]

Southern United States

[edit]
The Lumber River as seen from the boat launch at Princess Ann near Orrum, North Carolina

Northern United States

[edit]
Chocolate-colored Tahquamenon Falls

Africa

[edit]

Australia

[edit]

Intermittent blackwater events

[edit]

Other rivers in Australia may experience infrequent 'blackwater events' associated with flood waters connecting to forested floodplains and these events may be associated with hypoxic waters [low oxygen]. Examples include the Murray River, Edward River, Wakool River and Murrumbidgee River.[14]

Indonesia

[edit]
[edit]

See also

[edit]

References

[edit]
  1. ^ Janzen, D. H. (July 1974). "Tropical Blackwater Rivers, Animals, and Mast Fruiting by the Dipterocarpaceae". Biotropica. 6 (2): 69–103. doi:10.2307/2989823. JSTOR 2989823.
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