Previous Page  20 / 116 Next Page
Information
Show Menu
Previous Page 20 / 116 Next Page
Page Background

D I VE SLATE

18

|

FALL 2016

I

was in a small boat about 30 miles offshore

of San Diego, Calif., looking for life. We

were running hard at 20 knots when out of

the corner of my eye I caught a glimpse of

a tiny patch of brown against the vast blue

background. It was a bit of kelp about the size

of a trashcan lid. I turned toward it and immediately

saw a huge splash and a distressed yellowfin tuna doing

tight circles around the kelp. Here was a picture I had

wanted for years: a tuna on a kelp paddy.

When I got into the water I saw what had made that

big splash as the form of a massive 400- to 500-pound

blue marlin materialized out of the blue. The lightbulb

went off immediately, and I knew why the big marlin

was there — the more commonly seen striped marlin

does not prey on 20- to 30-pound tuna.

That day I got images of the blue marlin and the

tuna (see Parting Shot,

Alert Diver

, Winter 2015).

These were likely the first-ever underwater photos of

a blue marlin taken in California waters. It was among

the two or three best days I have ever had in 35 years

of diving kelp paddies.

That happened in the fall of 2014, which was the

beginning of a series of warming years that included

the very powerful 2015 El Niño. The warming events

of 2014, 2015 and 2016 have brought to the California

coast warm-water species from the south that had

rarely been seen over the years, and all of them were

observed around kelp paddies.

WHAT IS A KELP PADDY?

Searching for photographic subjects in the big blue

void of the open sea can be frustrating. Signs of life

are fleeting. The subtle splash of a marine mammal or

working birds are among the few signs that indicate

the possibility of life.

Much like the Atlantic coast, which has its own

drifting algae habitat (

Sargassum

), the Pacific coast

of North America has drifting kelp. Giant kelp

(

Macrocystis

) grows from Alaska to central Baja

California. Kelp paddies form when the anchoring

kelp holdfast weakens and breaks free after storms,

warming events or grazing by sea urchins. As the

80-foot-tall plants drift away, they become entangled

with other kelp plants. Buoyed to the surface by gas-

filled bladders, these floating masses are then swept

out to sea by wind and currents. An average-sized kelp

paddy might be the size of a bathtub, but they can

be more than 50 feet across with holdfasts dangling

down 40 feet. Kelp paddies can be found any time of

the year with locations varying from just a mile or so

off the coast to hundreds of miles out to sea. Most

kelp paddies drifting off the California coast originate

from the beds of giant kelp in the Channel Islands or

elsewhere along the West Coast.

Best described as “drifting islands of life,” kelp

paddies provide a refuge for planktonic fishes and

invertebrates that initially settle in the ready-made

habitat. Small fishes and invertebrates attract

schooling baitfish such as sardines and mackerel.

Larger predators such as tuna, marlin, sharks and

marine mammals complete the food chain as they

come to feed on the baitfish. The entire range of

large pelagic predators found on the Pacific coast

can be seen near kelp paddies. When the larger

predators appear, juvenile fishes can retreat within the

protection of the tangled plant mass.

The assemblage of animals found in association

with kelp drifting off the Pacific coast cannot be

found anywhere else in the world. For example, the

juvenile stage of the splitnose rockfish (

Sebastes

diploproa

) has only been observed under drifting

18

KELP PADDIES

|

22

DAN BOARD OF DIRECTORS

|

25

PATENT FORAMEN OVALE

AND FITNESS TO DIVE

|

28

DAN MEMBER PROFILE

|

30

PUBLIC SAFETY

ANNOUNCEMENT, EDUCATION SPOTLIGHT

|

31

TRAVEL SMARTER

KELP PADDIES

ISLANDS OF LIFE ADRIFT IN THE OPEN SEA

Text and photos by Richard Herrmann