By Michael Moore
The time has arrived when the age of a fish is an
important factor in its management and catch status. The accuracy of
determining the age of a given species has made a quantum leap in the last
decade due to the application of nuclear technology with roots in dating tree
rings and rocks to ichthyology – and leaving previous methods of estimating
species longevity far behind.
Scientists at NOAA’s Pacific Islands Fisheries Science
Center in Honolulu have been working on how to accurately determine the age of
a given species of fish by using two measures of radiation decay over time.
Center in Honolulu have been working on how to accurately determine the age of
a given species of fish by using two measures of radiation decay over time.
The first method, bomb radiocarbon dating, is based on a
time-specific event – in this case the atmospheric atomic bomb tests in the
Pacific. Bomb radiocarbon dating is a technique that has evolved as a unique
application in the age validation of marine fishes and invertebrates.
time-specific event – in this case the atmospheric atomic bomb tests in the
Pacific. Bomb radiocarbon dating is a technique that has evolved as a unique
application in the age validation of marine fishes and invertebrates.
The second method, lead-radium dating, has been used
successfully for nearly 30 species of fish by other investigators and is based
on a known radioisotope decay series. It can be used to determine ages for fish
ranging from a few years to about 100 years.
successfully for nearly 30 species of fish by other investigators and is based
on a known radioisotope decay series. It can be used to determine ages for fish
ranging from a few years to about 100 years.
The approach relies on a conserved record of the rapid
increase in radiocarbon (14C) that occurred in the oceans of the world as a
result of atmospheric testing of thermonuclear devices in the 1950’s and
1960’s. It can be used to age fish born during this period, and is currently
effective only for fish up to about 53 years old.
increase in radiocarbon (14C) that occurred in the oceans of the world as a
result of atmospheric testing of thermonuclear devices in the 1950’s and
1960’s. It can be used to age fish born during this period, and is currently
effective only for fish up to about 53 years old.
Both methods measure the amount of radioisotopes present in
the tiny ear bones – otoliths – of the fish. The radioisotopes are stored in
the calcium carbonate of the otoliths. The otoliths are micro-milled to expose
their core. The lead-radium measurements are performed in Hawaii and the
carbon-14 readings are done at the National Ocean Sciences Accelerator Mass
Spectrometry Facility (NOSAM) at Woods Hole Oceanographic Institution.
the tiny ear bones – otoliths – of the fish. The radioisotopes are stored in
the calcium carbonate of the otoliths. The otoliths are micro-milled to expose
their core. The lead-radium measurements are performed in Hawaii and the
carbon-14 readings are done at the National Ocean Sciences Accelerator Mass
Spectrometry Facility (NOSAM) at Woods Hole Oceanographic Institution.
Bomb radiocarbon dating can determine the age of individual
fish with high precision (± 1 to 2 years). Lead-radium dating, on the other
hand, can be used for fish of any age but detection limits require the pooling
of otoliths from many fish to attain measureable lead-radium levels. A group of
fish of similar size is used, and the result is an estimate of average age for
the group. Where both methods are feasible, using both can provide the most
information in an exploratory study.
fish with high precision (± 1 to 2 years). Lead-radium dating, on the other
hand, can be used for fish of any age but detection limits require the pooling
of otoliths from many fish to attain measureable lead-radium levels. A group of
fish of similar size is used, and the result is an estimate of average age for
the group. Where both methods are feasible, using both can provide the most
information in an exploratory study.
What allows for the precision of bomb radiocarbon dating is
the fact that the radiocarbon signal can be measured over time in reef-building
corals because coral stores the ocean signal in annual growth bands of the
skeleton. The same is true for fish otoliths, the tiny bones in the ear of the
fish. The radiocarbon signal is stored in the otolith calcium carbonate.
the fact that the radiocarbon signal can be measured over time in reef-building
corals because coral stores the ocean signal in annual growth bands of the
skeleton. The same is true for fish otoliths, the tiny bones in the ear of the
fish. The radiocarbon signal is stored in the otolith calcium carbonate.
This means the measured radiocarbon in the otolith core
(birth year) can be correlated to the coral radiocarbon record. The timing must
be right because the birth year must be during the rise of radiocarbon from the
bomb test period –from1955 to 1970. An example of how this works is if a fish
was captured in 1995 and its otolith core radiocarbon matched the coral record
from 1965. This fish was 30 years old.
(birth year) can be correlated to the coral radiocarbon record. The timing must
be right because the birth year must be during the rise of radiocarbon from the
bomb test period –from1955 to 1970. An example of how this works is if a fish
was captured in 1995 and its otolith core radiocarbon matched the coral record
from 1965. This fish was 30 years old.
“The coral records are a nice time-specific record of
marine chemistry including the radiocarbon signal created by the bomb tests in
the 50’s and 60’s,” said Allen H. Andrews, a PhD ichthyologist who works
as a Research Fisheries Biologist at the Pacific Islands Fisheries Center of
NOAA Fisheries. Andrews is currently working on determining the age, growth,
and longevity of marine organisms using naturally occurring and man-made
radioactivity. His work crosses numerous disciplines within marine science and
directly involves research in ichthyology, radiochemistry, marine ecology, and
chemical-physical oceanography.
marine chemistry including the radiocarbon signal created by the bomb tests in
the 50’s and 60’s,” said Allen H. Andrews, a PhD ichthyologist who works
as a Research Fisheries Biologist at the Pacific Islands Fisheries Center of
NOAA Fisheries. Andrews is currently working on determining the age, growth,
and longevity of marine organisms using naturally occurring and man-made
radioactivity. His work crosses numerous disciplines within marine science and
directly involves research in ichthyology, radiochemistry, marine ecology, and
chemical-physical oceanography.
One of the fish species that Andrews and his colleagues have
worked with is the Hawaiian pink snapper, (Pristipomoides filamentosus) known
as opakapaka.
worked with is the Hawaiian pink snapper, (Pristipomoides filamentosus) known
as opakapaka.
“Opakapaka were originally seen as a relatively fast
growing species with a maximum estimated age between 5 and 18 years,” said
Andrews. “The methods used to come up with these estimates are good for
validating the age of young fish, but not as appropriate for the largest fish.
growing species with a maximum estimated age between 5 and 18 years,” said
Andrews. “The methods used to come up with these estimates are good for
validating the age of young fish, but not as appropriate for the largest fish.
“Most fish can be aged by counting annual growth zones
in otoliths, similar to counting rings in a tree,” he said. “But
opakapaka otoliths have not revealed growth zones that can be counted for the
oldest fish. Therefore, the methods used for early fish growth were used to
extrapolate an age for the largest fish. For some fishes this practice may be
valid, but with opakapaka the results were unclear.”
in otoliths, similar to counting rings in a tree,” he said. “But
opakapaka otoliths have not revealed growth zones that can be counted for the
oldest fish. Therefore, the methods used for early fish growth were used to
extrapolate an age for the largest fish. For some fishes this practice may be
valid, but with opakapaka the results were unclear.”
Bomb radiocarbon dating of opakapaka revealed they could
live more than 40 years. In the study, otoliths from collections revealed ages
from 11 to 43 years for lengths of 20 inches to 29 inches. Overall, the age and
growth calculated for young fish by other methods remained valid up to about
5-10 years, but the extrapolated maximum ages underestimated true age. This
means opakapaka can grow fairly large in less than 10 years, but each fish can
reproduce for more than 30 years.
live more than 40 years. In the study, otoliths from collections revealed ages
from 11 to 43 years for lengths of 20 inches to 29 inches. Overall, the age and
growth calculated for young fish by other methods remained valid up to about
5-10 years, but the extrapolated maximum ages underestimated true age. This
means opakapaka can grow fairly large in less than 10 years, but each fish can
reproduce for more than 30 years.
Bomb Radiocarbon dating has been used to determine the
longevity other species, sometimes with dramatically unexpected results.
longevity other species, sometimes with dramatically unexpected results.
This recently turned out to be the case with the bluespine
unicornfish (Naso unicornis), a fish commonly seen by snorkelers in Hawaii and
known locally as Kala. This fish may seem like a small to medium-sized reef
fish to most people, but it can be a regular part of fish markets reaching a
maximum size of up to 27 inches. Its range is considerable as a tropical fish
ranging from Hawaii throughout the southern tropical Pacific and Indo-Pacific,
and into the Indian Ocean to the eastern coast of Africa.
unicornfish (Naso unicornis), a fish commonly seen by snorkelers in Hawaii and
known locally as Kala. This fish may seem like a small to medium-sized reef
fish to most people, but it can be a regular part of fish markets reaching a
maximum size of up to 27 inches. Its range is considerable as a tropical fish
ranging from Hawaii throughout the southern tropical Pacific and Indo-Pacific,
and into the Indian Ocean to the eastern coast of Africa.
“One of the challenges with the Kala is with the size
of the otoliths from this fish,” said Andrews, who is working with
collaborators Ed DeMartini and Jeff Eble on the project, an extension of work
started by Eble as a University of Hawaii graduate student.
of the otoliths from this fish,” said Andrews, who is working with
collaborators Ed DeMartini and Jeff Eble on the project, an extension of work
started by Eble as a University of Hawaii graduate student.
“They are small, and for me to validate the age I need
to extract the core – first year of growth or less – from the otolith and
analyze it for radiocarbon,” he said. “This was very difficult
and near the limits of what I can extract with the micromill with confidence
plus what NOSAMS can measure for radiocarbon with a reasonable level of
precision.
to extract the core – first year of growth or less – from the otolith and
analyze it for radiocarbon,” he said. “This was very difficult
and near the limits of what I can extract with the micromill with confidence
plus what NOSAMS can measure for radiocarbon with a reasonable level of
precision.
“The latest bomb radiocarbon dating confirmed the 50
year estimate of longevity for the species that Jeff Eble made from counting
growth zones in otolith sections.”
year estimate of longevity for the species that Jeff Eble made from counting
growth zones in otolith sections.”
This kind of information is important for fishery management
because proper stock assessments can be made to determine population
productivity, and ultimately an estimate of a sustainable yield.
because proper stock assessments can be made to determine population
productivity, and ultimately an estimate of a sustainable yield.
“All of this information on longevity is important in
determining fishable levels and the sustainability of a given species
fishery,” said Andrews. “It helps us understand the growth cycle of
the species, plus when it starts breeding combined with that species’
fecundity. It’s not as straightforward as people might think.”
determining fishable levels and the sustainability of a given species
fishery,” said Andrews. “It helps us understand the growth cycle of
the species, plus when it starts breeding combined with that species’
fecundity. It’s not as straightforward as people might think.”