200 m
Euphotic zone
Benthic environment
Abyssal zone
of benthic
environment
Bathyal zone
of benthic
environment
Depth
High tide
Intertidal zone
Low tide
Neritic
province
Oceanic
province
Pelagic environment
4000 m
6000 m
Hadal zone
of benthic
environment
Mary Beth Angelo/Science Source
Bill Curtsinger/NG ImageCollection
Dr Paul A Zahl/PhotoResearchers/Getty Images
Tom Brakefield/Stockbyte/Getty Images
Intertidal zone:
Rockweed (brown algae)
Shallow benthic environment:
Rough file clam
Saber-toothed viperfish
Oceanic province:
Bottlenose dolphins
Neritic province:
Tide zonesTide zones
Supratidal
(splash) zone
IntIntntereretidtidalall
zone
SubSubtidtidalal
zzoneone
LeLevvvel el eofofof
loloweswesttt tideideid
Level of
highest tide
Cyanonbacatereia,
seasea ha hairir (((UlUloUlothrthrrrrrixixxx),),
rough perriwinkles
AcoAcorn bn baranacnacleles,s,
rockk barnacales,
mussels, limpetsssssssssssssssssss,,,,,,,
perpereiwiiwiwnklnklkeses,
oystersr,
brobrobrown wn wnalgalgalgaeaeae
BroBrown wnalgalggggggaeaeaeaeaeaeaeae,,,,,
musmusselselss,,
seasea st starsars,,
brbrittittle le stastarsrs,,
seasea ur urchichinsns,,
spispiderder cr crababss
TidTidTidTidTTiTidTidTidTide pe pe pe e pe e pe pe ppppppppppppppppppppooloooloolooooloooolooooooooloo
Anemones,
tube worms,
hermit crabs
CommCommunity zonation pattern ofunity zonation pattern ofrorockcky shoresy shores
Ada
pted
from
Fig
ure
14.1 in Karleskint
,^ G
.Intr
oduction to Marine Biologyrr
yy
Philadelphi
aii:^
Har
co
urt
C
ollege Publishers
(^1998
).
<>ÌÊÊÌ
iÊVi>ÊUÊ}ÕÀiÊ££°{Ê
Zonation along a rocky
Ã
ÀiÊUÊ}ÕÀiÊ££°xÊ
Three zones are shown: the
supratidal, or “splash” zone,
which is never fully submerged;
the intertidal zone, which is fully
submerged at high tide; and the
subtidal zone (part of the benthic
environment), which is always
submerged. Representative
organisms are listed for each of
these zones.
The intertidal zone, the benthic
environment, and the pelagic environment
make up the ocean. The pelagic
environment consists of the neritic and
oceanic provinces. (The slopes of the
ocean floor aren’t as steep as shown; they
are exaggerated here to save space.)
279