20 January 2020 | Category: Resilience of the richest reefs

First dive Raja Ampat, Sorido

By Erik Meesters

I have been working on coral reefs since 1987, which means I...

So finally, after three hot days in Waisai where we had discussions with local authorities, we got on the Temukira, a nice little wooden ship that we rented for our expedition. It felt good to be on the water, much cooler and after days of rain it was finally sunny. We sailed to Cape Kri, where we anchored in the sand. The owner of Papua Diving, a diving resort, had invited us to have a look close to his property where apparently big changes were taking place.

Blog authors: Erik Meesters and Ricardo Tapilatu (Director of the research Center for Pacific Marine Resources, and Professor Faculty Fisheries and Marine Sciences)

Diving in a sinkhole

Our team consisted of five divers to photograph the bottom community and fishes along a number of transect lines. It turned out that we were diving in a sinkhole. While outside of the sinkhole the current was very fast, inside the hole it was very peaceful.

First dive in Raja Ampat

The sinkhole in front of Sorido dive resort (picture by Iqbal Alaik).

First dive in Raja Ampat

Popular dive spotSorido is close to one of the most visited dive spots in Raja Ampat, Cape Kri. And that became soon visible. Within half an hour we were surrounded by six big dive ships, so called liveaboards. The number of divers per boat can easily be between 15-25. One can easily imagine that 150 divers at once on one spot is too much.

First dive in Raja Ampat

Our liveaboard surrouned by four other boats.

Algae mats

We found that the sinkhole is dominated by Padina algae. Thick mats cover the slope of the sinkhole. A couple of years ago we hardly saw any algae, while now they seemed to be everywhere. What could have caused this change? At night, back on the boat, we discussed this with the team.

Algae thrive on nutrients, for instance from human waste. We found out that many live-aboard boats don’t have holding tanks for the waste water. Given that they anchor just next to the sinkhole, their sewage may end up in there. Because the sinkhole is so sheltered, everything that ends up in it is not flushed away like in many other places in Raja Ampat. As the dive resort owner summarized it: “At some of the dive sites, our guests literally got sh*t dumped on their head.”

The algae may however also result from the overflow of septic tanks on land, especially when the bottom consists of carbonate rock which is very porous. Ultimately, the contents of these septic tanks will end up on the reef. Another possible cause could be run-off from land, which often follows land clearing. The input from organic material from the land can lead to bloom of algae and cyanobacteria.

In the future we hope to find out what caused the algae mats, so the coral will recover and divers will have all the more reason to come back.

By Erik Meesters

I have been working on coral reefs since 1987, which means I’ve seen the reefs change tremendously. Where the water was once so clear you couldn’t see it, it is now always filled with floating particles limiting the amount of light that reaches the corals on the bottom. I started my professional career on Curacao and Bonaire, but have also worked in Indonesia, Hawaii, Tahiti, and the Maldives. My main interest is in the health and recovery of coral reefs and nowadays I work mainly on the reefs of the islands of the Caribbean Netherlands and on the Saba Bank, the largest protected nature area of the Netherlands. Currently I work on coral restoration (www.rescq.eu), cyanobacteria on coral reefs, and large scale assessments. The threats that reefs face are everywhere similar though local pressures may differ from place to place. Where chronic pressures such as pollution, eutrophication, and overfishing often lead to a gradual decrease in coral health, we are now faced with unprecedented decreases in coral reef quality and health by the impacts of climate change. The return rate of hurricanes and storms appears to be on the rise and episodes of extremely warm sea water cause massive bleaching, wreaking havoc and turning flourishing reefs into graveyards overnight. My research group at Wageningen Marine Research (WMR) studies in collaboration with the Netherlands Institute for Sea Research (NIOZ) the long-term development of the reefs of Bonaire and Curacao since 1973 and currently has the longest time series of data of a modern reef in the world. The work of our research group has recently received internationally recognition by awarding one of our publications with the ‘Best 2017 Paper Award’ from the editorial board of the journal Coral Reefs. The question which is often asked, is not whether coral reefs will survive, but should be whether humanity will survive. Healthy coral reefs are among the most amazing places in the world. They will survive with or without humanity (corals are on earth already 240 million years, while we are here only a meager 200 thousand years), but it is on us to decide whether we will be there to see it. If we don’t decrease our impacts on our environment we are unlikely to become as old as corals (another 239.8 million years!).

There are 3 comments.

  1. By: Erik Meesters · 06-02-2020 at 11:15 am

    Sorry Ricardo that it looks like I’m the only author. The text states that we are both author though. I guess it’s due to software restrictions.
    The Padina algae appear to be a general indication of more eutrophic conditions.
    thanks for your message,
    Erik

    1. By: Ricardo Tapilatu · 07-02-2020 at 11:11 am

      Thanks Erik. I just remembered the case once Im back on campus and checked my notes and images. My note is intended for our information. Anyway, both of us played roles as authors and also commentators.

  2. By: Ricardo Tapilatu · 06-02-2020 at 10:27 am

    Yes, there are nutrients impacts visible. I saw that one on the Waisai coast as well. The growing city has no a proper waste management in place . . . . does not seem to need much nutrient for algae to appear . . .

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